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For the scientific journal, see Geology (journal).
Geologic provinces of the world (USGS)
     Shield      Platform      Orogen      Basin      Large igneous province      Extended crust Oceanic crust:      0–20 Ma      20–65 Ma      >65 Ma
Geology (from the Greek γῆ, gê, "earth" and λόγος, logos, "speech") is the science and study of the solid and liquid matter that constitutes the Earth. The field of geology encompasses the study of the composition, structure, physical properties, dynamics, and history of Earth materials, and the processes by which they are formed, moved, and changed. The field is a major academic discipline, and is also important for mineral and hydrocarbon extraction, knowledge about and mitigation of natural hazards, some engineering fields, and understanding past climates and environments.

Contents

History and etymology

History

Main article: History of geology
A mosquito and a fly in this Baltic amber necklace are between 40 and 60 million years old
The work Peri Lithon (On Stones) by the ancient Greek scholar Theophrastus (372–287 BC), a student of ancient Greek philosopher Aristotle, remained authoritative for a millennium. Peri Lithon was translated into Latin and some other foreign languages. Its interpretation of fossils was the most dominant theory in classical Antiquity and the early Middle Ages, until it was replaced by Avicenna's theory of petrifying fluids (succus lapidificatus) in the late Middle Ages.[1][2] In the Roman period, Pliny the Elder produced a very extensive discussion of many more minerals and metals then widely used for practical ends. He is among the first to correctly identify the origin of amber as a fossilized resin from pine trees by the observation of insects trapped within some pieces. He also laid the basis of crystallography by recognising the octahedral habit of diamond.
Some modern scholars, such as Fielding H. Garrison, are of the opinion that modern geology began in the medieval Islamic world.[3] Abu al-Rayhan al-Biruni (973–1048 AD) was one of the earliest Muslim geologists, whose works included the earliest writings on the geology of India, hypothesizing that the Indian subcontinent was once a sea.[4] Ibn Sina (Avicenna, 981–1037), in particular, made significant contributions to geology and the natural sciences (which he called Attabieyat) along with other natural philosophers such as Ikhwan AI-Safa and many others. He wrote an encyclopaedic work entitled “Kitab al-Shifa” (the Book of Cure, Healing or Remedy from ignorance), in which Part 2, Section 5, contains his essay on Mineralogy and Meteorology, in six chapters: Formation of mountains, The advantages of mountains in the formation of clouds; Sources of water; Origin of earthquakes; Formation of minerals; The diversity of earth’s terrain. These principles were later known in the Renaissance of Europe as the law of superposition of strata, the concept of catastrophism, and the doctrine of uniformitarianism. These concepts were also embodied in the Theory of the Earth by James Hutton in the Eighteenth century C.E. Academics such as Toulmin and Goodfield (1965), commented on Avicenna's contribution: "Around A.D. 1000, Avicenna was already suggesting a hypothesis about the origin of mountain ranges, which in the Christian world, would still have been considered quite radical eight hundred years later".[5] Avicenna's scientific methodology of field observation was also original in the Earth sciences, and remains an essential part of modern geological investigations.[2]
In China, the polymath Shen Kua (1031–1095) formulated a hypothesis for the process of land formation: based on his observation of fossil animal shells in a geological stratum in a mountain hundreds of miles from the ocean, he inferred that the land was formed by erosion of the mountains and by deposition of silt.
William Smith's geologic map of England, Wales, and southern Scotland. Completed in 1815, it was the first national-scale geologic map, and by far the most accurate of its time.[6]
Georg Agricola (1494–1555), a physician, wrote the first systematic treatise about mining and smelting works, De re metallica libri XII, with an appendix Buch von den Lebewesen unter Tage (Book of the Creatures Beneath the Earth). He covered subjects like wind energy, hydrodynamic power, melting cookers, transport of ores, extraction of soda, sulfur and alum, and administrative issues. The book was published in 1556.
Nicolas Steno (1638–1686) is credited with the law of superposition, the principle of original horizontality, and the principle of lateral continuity: three defining principles of stratigraphy. By the 1700s Jean-Étienne Guettard and Nicolas Desmarest hiked central France and recorded their observations on geological maps; Guettard recorded the first observation of the volcanic origins of this part of France.
William Smith (1769–1839) drew some of the first geological maps and began the process of ordering rock strata (layers) by examining the fossils contained in them.[6]
James Hutton is often viewed as the first modern geologist.[7] In 1785 he presented a paper entitled Theory of the Earth to the Royal Society of Edinburgh. In his paper, he explained his theory that the Earth must be much older than had previously been supposed in order to allow enough time for mountains to be eroded and for sediments to form new rocks at the bottom of the sea, which in turn were raised up to become dry land. Hutton published a two-volume version of his ideas in 1795 (Vol. 1, Vol. 2).
The geologist, 19th century painting by Carl Spitzweg
Followers of Hutton were known as Plutonists because they believed that some rocks were formed by vulcanism which is the deposition of lava from volcanoes, as opposed to the Neptunists, who believed that all rocks had settled out of a large ocean whose level gradually dropped over time.
In 1811 Georges Cuvier and Alexandre Brongniart published their explanation of the antiquity of the Earth, inspired by Cuvier's discovery of fossil elephant bones in Paris. To prove this, they formulated the principle of stratigraphic succession of the layers of the earth. They were independently anticipated by William Smith's stratigraphic studies on England and Scotland.
Sir Charles Lyell first published his famous book, Principles of Geology[8], in 1830. Lyell continued to publish new revisions until he died in 1875. The book, which influenced the thought of Charles Darwin, successfully promoted the doctrine of uniformitarianism. This theory states that slow geological processes have occurred throughout the Earth's history and are still occurring today. In contrast, catastrophism is the theory that Earth's features formed in single, catastrophic events and remained unchanged thereafter. Though Hutton believed in uniformitarianism, the idea was not widely accepted at the time.
Plate tectonics – seafloor spreading and continental drift illustrated on relief globe of the Field Museum
Much of 19th-century geology revolved around the question of the Earth's exact age. Estimates varied from a few 100,000 to billions of years.[9] The most significant advance in 20th century geology has been the development of the theory of plate tectonics in the 1960s. Plate tectonic theory arose out of two separate geological observations: seafloor spreading and continental drift. The theory revolutionized the Earth sciences.
The theory of continental drift was proposed by Frank Bursley Taylor in 1908, expanded by Alfred Wegener in 1912 and by Arthur Holmes, but wasn't broadly accepted until the late 1960s when the theory of plate tectonics was developed.

Etymology

The word "geology" was first used by Jean-André Deluc in the year 1778 and introduced as a fixed term by Horace-Bénédict de Saussure in the year 1779. The science was not included in Encyclopædia Britannica's third edition completed in 1797, but had a lengthy entry in the fourth edition completed by 1809.[10] An older meaning of the word was first used by Richard de Bury to distinguish between earthly and theological jurisprudence.

Geologic time

Geological time put in a diagram called a geological clock, showing the relative lengths of the eons of the Earth's history.
Main articles: History of the Earth and Geologic time scale
The geologic time scale encompasses the history of the Earth.[11] It is bracketed at the young end by the dates of the earliest solar system material at 4.567 Ga[12] (gigaannum: billion years ago) and the age of the Earth at 4.54 Ga[13][14], at the beginning of the informally-recognized Hadean eon. At the young end of the scale, it is bracketed by the present day in the Holocene epoch.

Important milestones

Brief time scale

The second and third timelines are each subsections of their preceding timeline as indicated by asterisks. The Holocene (the latest epoch) is too small to be shown clearly on this timeline.
Millions of Years

Relative and Absolute Dating

Geological events can be given a precise date at a point in time, or they can be related to other events that came before and after them. Geologists use a variety of methods to give both relative and absolute dates to geological events. They then use these dates to find the rates at which processes occur.

Relative dating

Main article: Relative dating
Cross-cutting relations can be used to determine the relative ages of rock strata and other geological structures. Explanations: A - folded rock strata cut by a thrust fault; B - large intrusion (cutting through A); C - erosional angular unconformity (cutting off A & B) on which rock strata were deposited; D - volcanic dyke (cutting through A, B & C); E - even younger rock strata (overlying C & D); F - normal fault (cutting through A, B, C & E).
Methods for relative dating were developed when geology first emerged as a formal science. Geologists still use the following principles today as a means to provide information about geologic history and the timing of geologic events.
The principle of intrusive relationships concerns crosscutting intrusions. In geology, when an igneous intrusion cuts across a formation of sedimentary rock, it can be determined that the igneous intrusion is younger than the sedimentary rock. There are a number of different types of intrusions, including stocks, laccoliths, batholiths, sills and dikes.
The principle of cross-cutting relationships pertains to the formation of faults and the age of the sequences through which they cut. Faults are younger than the rocks they cut; accordingly, if a fault is found that penetrates some formations but not those on top of it, then the formations that were cut are older than the fault, and the ones that are not cut must be younger than the fault. Finding the key bed in these situations may help determine whether the fault is a normal fault or a thrust fault.[15]
The principle of inclusions and components states that, with sedimentary rocks, if inclusions (or clasts) are found in a formation, then the inclusions must be older than the formation that contains them. For example, in sedimentary rocks, it is common for gravel from an older formation to be ripped up and included in a newer layer. A similar situation with igneous rocks occurs when xenoliths are found. These foreign bodies are picked up as magma or lava flows, and are incorporated, later to cool in the matrix. As a result, xenoliths are older than the rock which contains them.
The principle of uniformitarianism states that the geologic processes observed in operation that modify the Earth's crust at present have worked in much the same way over geologic time.[16] A fundamental principle of geology advanced by the 18th century Scottish physician and geologist James Hutton, is that "the present is the key to the past." In Hutton's words: "the past history of our globe must be explained by what can be seen to be happening now."[citation needed]
The principle of original horizontality states that the deposition of sediments occurs as essentially horizontal beds. Observation of modern marine and non-marine sediments in a wide variety of environments supports this generalization (although cross-bedding is inclined, the overall orientation of cross-bedded units is horizontal).[15]
The principle of superposition states that a sedimentary rock layer in a tectonically undisturbed sequence is younger than the one beneath it and older than the one above it. Logically a younger layer cannot slip beneath a layer previously deposited. This principle allows sedimentary layers to be viewed as a form of vertical time line, a partial or complete record of the time elapsed from deposition of the lowest layer to deposition of the highest bed.[15]
The principle of faunal succession is based on the appearance of fossils in sedimentary rocks. As organisms exist at the same time period throughout the world, their presence or (sometimes) absence may be used to provide a relative age of the formations in which they are found. Based on principles laid out by William Smith almost a hundred years before the publication of Charles Darwin's theory of evolution, the principles of succession were developed independently of evolutionary thought. The principle becomes quite complex, however, given the uncertainties of fossilization, the localization of fossil types due to lateral changes in habitat (facies change in sedimentary strata), and that not all fossils may be found globally at the same time.[17]

Absolute dating

Main articles: Absolute dating, Radiometric dating, and Geochronology
Geologists can also give precise absolute dates to geologic events. These dates are useful on their own, and can also be used in conjunction with relative dating methods or to calibrate relative dating methods.[18]
A large advance in geology in the advent of the 20th century was the ability to give precise absolute dates to geologic events through radioactive isotopes and other methods. The advent of isotopic dating changed the understanding of geologic time. Before, geologists could only use fossils to date sections of rock relative to one another. With isotopic dates, absolute dating became possible, and these absolute dates could be applied fossil sequences in which there was datable material, converting the old relative ages into new absolute ages.
For many geologic applications, isotope ratios are measured in minerals that give the amount of time that has passed since a rock passed through its particular closure temperature, the point at which different radiometric isotopes stop diffusing into and out of the crystal lattice.[19][20] These are used in geochronologic and thermochronologic studies. Common methods include uranium-lead dating, potassium-argon dating and argon-argon dating, and uranium-thorium dating. These methods are used for a variety of applications. Dating of lavas and ash layers can help to date stratigraphy and calibrate relative dating techniques. These methods can also be used to determine ages of pluton emplacement. Thermochemical techniques can be used to determine temperature proiles within the crust, the uplift of mountain ranges, and paleotopography.
Fractionation of the lanthanide series elements is used to compute ages since rocks were removed from the mantle.
Other methods are used for more recent events. Optically stimulated luminescence and cosmogenic radionucleide dating are used to date surfaces and/or erosion rates. Dendrochronology can also be used for the dating of landscapes. Radiocarbon dating is used for young organic material.

Geologic Materials

The majority of geological data come from research on solid Earth materials. These typically fall into one of two categories: rock and unconsolidated material.

Rock

This schematic diagram of the rock cycle shows the relationship between magma and sedimentary, metamorphic, and igneous rock
Main articles: Rock (geology) and Rock cycle
There are three major types of rock: igneous, sedimentary, and metamorphic. The rock cycle is an important concept in geology which illustrates the relationships between these three types of rock, and magma. When a rock crystallizes from melt (magma and/or lava), it is an igneous rock. This rock can be weathered and eroded, and then redeposited and lithified into a sedimentary rock, or be turned into a metamorphic rock due to heat and pressure that change the mineral content of the rock and give it a characteristic fabric. The sedimentary rock can then be subsequently turned into a metamorphic rock due to heat and pressure, and the metamorphic rock can be weathered, eroded, deposited, and lithified, becoming a sedimentary rock. Sedimentary rock may also be re-eroded and redeposited, and metamorphic rock may also undergo additional metamorphism. All three types of rocks may be re-melted; when this happens, a new magma is formed, from which an igneous rock may once again crystallize.
The majority of research in geology is associated with the study of rock, as rock provides the primary record of the majority of the geologic history of the Earth.

Unconsolidated material

Geologists also study unlithified material, which typically comes from more recent deposits. Because of this, the study of such material is often known as Quaternary geology, after the recent Quaternary Period. This includes the study of sediment and soils, and is important to some (or many) studies in geomorphology, sedimentology, and paleoclimatology.

Whole-Earth structure

Oceanic-continental convergence resulting in subduction and volcanic arcs illustrates one effect of plate tectonics.

Plate tectonics

Main article: Plate tectonics
On this diagram, subducting slabs are in blue, and continental margins and a few plate boundaries are in red. The blue blob in the cutaway section is the seismically-imaged Farallon Plate, which is subducting beneath North America. The remnants of this plate on the Surface of the Earth are the Juan de Fuca Plate and Explorer plate in the Northwestern USA / Southwestern Canada, and the Cocos Plate on the west coast of Mexico.
In the 1960s, a series of discoveries, the most important of which was seafloor spreading[21][22], showed that the Earth's lithosphere, which includes the crust and rigid uppermost portion of the upper mantle, is separated into a number of tectonic plates that move across the plastically-deforming, solid, upper mantle, which is called the asthenosphere. There is an intimate coupling between the movement of the plates on the surface and the convection of the mantle: oceanic plate motions and mantle convection currents always move in the same direction, because the oceanic lithosphere is the rigid upper thermal boundary layer of the convecting mantle. This coupling between rigid plates moving on the surface of the Earth and the convecting mantle is called plate tectonics.
The development of plate tectonics provided a physical basis for many observations of the solid Earth. Long linear regions of geologic features could be explained as plate boundaries.[23] Mid-ocean ridges, high regions on the seafloor where hydrothermal vents and volcanoes exist, were explained as divergent boundaries, where two plates move apart. Arcs of volcanoes and earthquakes were explained as convergent boundaries, where one plate subducts under another. Transform boundaries, such as the San Andreas fault system, resulted in widespread powerful earthquakes. Plate tectonics also provided a mechanism for Alfred Wegener's theory of continental drift[24], in which the continents move across the surface of the Earth over geologic time. They also provided a driving force for crustal deformation, and a new setting for the observations of structural geology. The power of the theory of plate tectonics lies in its ability to combine all of these observations into a single theory of how the lithosphere moves over the convecting mantle.

Earth structure

Main article: Structure of the Earth
Earth layered structure. (1) inner core; (2) outer core; (3) lower mantle; (4) upper mantle; (5) lithosphere; (6) crust
Earth layered structure. Typical wave paths from earthquakes like these gave early seismologists insights into the layered structure of the Earth
Advances in seismology, computer modeling, and mineralogy and crystallography at high temperatures and pressures give insights into the internal composition and structure of the Earth.
Seismologists can use the arrival times of seismic waves in reverse to image the interior of the Earth. Early advances in this field showed the existence of a liquid outer core (where shear waves were not able to propagate) and a dense solid inner core. These advances led to the development of a layered model of the Earth, with a crust and lithosphere on top, the mantle below (separated within itself by seismic discontinuities at 410 and 660 kilometers), and the outer core and inner core below that. More recently, seismologists have been able to create detailed images of wave speeds inside the earth in the same way a doctor images a body in a CT scan. These images have led to a much more detailed view of the interior of the Earth, and have replaced the simplified layered model with a much more dynamic model.
Mineralogists have been able to use the pressure and temperature data from the seismic and modelling studies alongside knowledge of the elemental composition of the Earth at depth to reproduce these conditions in experimental settings and measure changes in crystal structure. These studies explain the chemical changes associated with the major seismic discontinuities in the mantle, and show the crystallographic structures expected in the inner core of the Earth.

Geological evolution of an area

An originally horizontal sequence of sedimentary rocks (in shades of tan) are affected by igneous activity. Deep below the surface are a magma chamber and large associated igneous bodies. The magma chamber feeds the volcano, and sends off shoots of magma that will later crystallize into dikes and sills. Magma also advances upwards to form intrusive igneous bodies. The diagram illustrates both a cinder cone volcano, which releases ash, and a composite volcano, which releases both lava and ash.
An illustration of the three types of faults. Strike-slip faults occur when rock units slide past one another, normal faults occur when rocks are undergoing horizontal extension, and thrust faults occur when rocks are undergoing horizontal shortening.
The geology of an area evolves through time as rock units are deposited and inserted and deformational processes change their shapes and locations.
Rock units are first emplaced either by deposition onto the surface or intrusion into the overlying rock. Deposition can occur when sediments settle onto the surface of the Earth and later lithify into sedimentary rock, or when as volcanic material such as volcanic ash or lava flows blanket the surface. Igneous intrusions such as batholiths, laccoliths, dikes, and sills, push upwards into the overlying rock, and crystallize as they intrude.
After the initial sequence of rocks has been deposited, the rock units can be deformed and/or metamorphosed. Deformation typically occurs as a result of horizontal shortening, horizontal extension, or side-to-side (strike-slip) motion. These structural regimes broadly relate to convergent boundaries, divergent boundaries, and transform boundaries, respectively, between tectonic plates.
When rock units are placed under horizontal compression, they shorten and become thicker. Because rock units, other than muds, do not significantly change in volume, this is accomplished in two primary ways: through faulting and folding. In the shallow crust, where brittle deformation can occur, thrust faults form, which cause deeper rock to move on top of shallower rock. Because deeper rock is often older, as noted by the principle of superposition, this can result in older rocks moving on top of younger ones. Movement along faults can result in folding, either because the faults are not planar, or because the rock layers are dragged along, forming drag folds, as slip occurs are along the fault. Deeper in the Earth, rocks behave plastically, and fold instead of faulting. These folds can either be those where the material in the center of the fold buckles upwards, creating "antiforms", or where it buckles downwards, creating "synforms". If the tops of the rock units within the folds remain pointing upwards, they are called anticlines and synclines, respectively. If some of the units in the fold are facing downward, the structure is called an overturned anticline or syncline, and if all of the rock units are overturned or the correct up-direction is unknown, they are simply called by the most general terms, antiforms and synforms.
A diagram of folds, indicating an anticline and a syncline.
Even higher pressures and temperatures during horizontal shortening can cause both folding and metamorphism of the rocks. This metamorphism causes changes in the mineral composition of the rocks; creates a foliation, or planar surface, that is related to mineral growth under stress; and can remove signs of the original textures of the rocks, such as bedding in sedimentary rocks, flow features of lavas, and crystal patterns in crystalline rocks.
Extension causes the rock units as a whole to become longer and thinner. This is primarily accomplished through normal faulting and through the ductile stretching and thinning. Normal faults drop rock units that are higher below those that are lower. This typically results in younger units being placed below older units. Stretching of units can result in their thinning; in fact, there is a location within the Maria Fold and Thrust Belt in which the entire sedimentary sequence of the Grand Canyon can be seen over a length of less than a meter. Rocks at the depth to be ductilely stretched are often also metamorphosed. These stretched rocks can also pinch into lenses, known as boudins, after the French word for "sausage", because of their visual similarity.
Where rock units slide past one another, strike-slip faults develop in shallow regions, and become shear zones at deeper depths where the rocks deform ductilely.
Geologic cross-section of Kittatinny Mountain. This cross-section shows metamorphic rocks, overlain by younger sediments deposited after the metamorphic event. These rock units were later folded and faulted during the uplift of the mountain.
The addition of new rock units, both depositionally and intrusively, often occurs during deformation. Faulting and other deformational processes result in the creation of topographic gradients, causing material on the rock unit that is increasing in elevation to be eroded by hillslopes and channels. These sediments are deposited on the rock unit that is going down. Continual motion along the fault maintains the topographic gradient in spite of the movement of sediment, and continues to create accommodation space for the material to deposit. Deformational events are often also associated with volcanism and igneous activity. Volcanic ashes and lavas accumulate on the surface, and igneous intrusions enter from below. Dikes, long, planar igneous intrusions, enter along cracks, and therefore often form in large numbers in areas that are being actively deformed. This can result in the emplacement of dike swarms, such as those that are observable across the Canadian shield, or rings of dikes around the lava tube of a volcano.
All of these processes do not necessarily occur in a single environment, and do not necessarily occur in a single order. The Hawaiian Islands, for example, consist almost entirely of layered basaltic lava flows. The sedimentary sequences of the mid-continental United States and the Grand Canyon in the southwestern United States contain almost-undeformed stacks of sedimentary rocks that have remained in place since Cambrian time. Other areas are much more geologically complex. In the southwestern United States, sedimentary, volcanic, and intrusive rocks have been metamorphosed, faulted, foliated, and folded. Even older rocks, such as the Acasta gneiss of the Slave craton in northwestern Canada, the oldest known rock in the world have been metamorphosed to the point where their origin is undiscernable without laboratory analysis. In addition, these processes can occur in stages. In many places, the Grand Canyon in the southwestern United States being a very visible example, the lower rock units were metamorphosed and deformed, and then deformation ended and the upper, undeformed units were deposited. Although any amount of rock emplacement and rock deformation can occur, and they can occur any number of times, these concepts provide a guide to understanding the geological history of an area.

Methods of geology

Geologists use a number of field, laboratory, and numerical modeling methods to decipher Earth history and understand the processes that occur on and in the Earth. In typical geological investigations, geologists use primary information related to petrology (the study of rocks), stratigraphy (the study of sedimentary layers), and structural geology (the study of positions of rock units and their deformation). In many cases, geologists also study modern soils, rivers, landscapes, and glaciers; investigate past and current life and biogeochemical pathways, and use geophysical methods to investigate the subsurface.

Field methods

A typical USGS field mapping camp in the 1950's
Today, handheld computers with GPS and geographic information systems software are often used in geological field work (digital geologic mapping).
Geological field work varies depending on the task at hand. Typical fieldwork could consist of:

Laboratory methods

A petrographic microscope, which is a optical microscope fitted with cross-polarizing lenses, a conoscopic lens, and compensators (plates of anisotropic materials; gypsum plates and quartz wedges are common), for crystallographic analysis.

Petrology

Main article: Petrology
In addition to the field identification of rocks, petrologists identify rock samples in the laboratory. Two of the primary methods for identifying rocks in the laboratory are through optical microscopy and by using an electron microprobe. In an optical mineralogy analysis, thin sections of rock samples are analyzed through a petrographic microscope, where the minerals can be identified through their different properties in plane-polarized and cross-polarized light, including their birefringence, pleochroism, twinning, and interference properties with a conoscopic lens.[31] In the electron microprobe, individual locations are analyzed for their exact chemical compositions and variation in composition within individual crystals.[32] Stable[33] and radioactive isotope[34] studies provide insight into the geochemical evolution of rock units.
Petrologists use fluid inclusion data[35] and perform high temperature and pressure physical experiments[36] to understand the temperatures and pressures at which different mineral phases appear, and how they change through igneous[37] and metamorphic processes. This research can be extrapolated to the field to understand metamorphic processes and the conditions of crystallization of igneous rocks.[38] This work can also help to explain processes that occur within the Earth, such as subduction and magma chamber evolution.

Structural geology

A diagram of an orogenic wedge. The wedge grows through faulting in the interior and along the main basal fault, called the décollement. It builds its shape into a critical taper, in which the angles within the wedge remain the same as failures inside the material balance failures along the décollement. It is analogous to a bulldozer pushing a pile of dirt, where the bulldozer is the overriding plate.
Main article: Structural geology
Structural geologists use microscopic analysis of oriented thin sections of geologic samples to observe the fabric within the rocks which gives information about strain within the crystal structure of the rocks. They also plot and combine measurements of geological structures in order to better understand the orientations of faults and folds in order to reconstruct the history of rock deformation in the area. In addition, they perform analog and numerical experiments of rock deformation in large and small settings.
The analysis of structures is often accomplished by plotting the orientations various features onto stereonets. A stereonet is a stereographic projection of a sphere onto a plane, in which planes are projected as lines and lines are projected as points. These can be used to find the locations of fold axes, relationships between several faults, and relationships between other geologic structures.
Among the most well-known experiments in structural geology are those involving orogenic wedges, which are zones in which mountains are built along convergent tectonic plate boundaries.[39] In the analog versions of these experiments, horizontal layers of sand are pulled along a lower surface into a back stop, which results in realistic-looking patterns of faulting and the growth of a critically-tapered (all angles remain the same) orogenic wedge.[40] Numerical models work in the same way as these analog models, though they are often more sophisticated and can include patterns of erosion and uplift in the mountain belt.[41] This helps to show the relationship between erosion and the shape of the mountain range. These studies can also give useful information about pathways for metamorphism through pressure, temperature, space, and time.[42]

Stratigraphy

Main article: Stratigraphy
Exploration geologists examining a freshly recovered drill core. Chile, 1994
In the laboratory, stratigraphers analyze samples of stratigraphic sections that can be returned from the field, such as those from drill cores.[43] Stratigraphers also analyze data from geophysical surveys that show the locations of stratigraphic units in the subsurface.[44] Geophysical data and well logs can be combined to produce a better view of the subsurface, and stratigraphers often use computer programs to do this in three dimensions.[45] Stratigraphers can then use these data to reconstruct ancient processes occurring on the surface of the Earth,[46] interpret past environments, and locate areas for water, coal, and hydrocarbon extraction.
In the laboratory, biostratigraphers analyze rock samples from outcrop and drill cores for the fossils found in them.[43] These fossils help scientists to date the core and to understand the depositional environment in which the rock units formed. Geochronologists precisely date rocks within the stratigraphic section in order to provide better absolute bounds on the timing and rates of deposition.[47] Magnetic stratigraphers look for signs of magnetic reversals in igneous rock units within the drill cores.[43] Other scientists perform stable isotope studies on the rocks to gain information about past climate.[43]

Planetary geology

Surface of Mars as photographed by the Viking 2 lander December 9, 1977.
Main articles: Planetary geology and Geology of solar terrestrial planets
With the advent of space exploration in the twentieth century, geologists have begun to look at other planetary bodies in the same way as the Earth. This led to the establishment of the field of planetary geology, sometimes known as Astrogeology, in which geologic principles are applied to other bodies of the solar system.
Although the Greek-language-origin prefix geo refers to Earth, "geology" is often used in conjunction with the names of other planetary bodies when describing their composition and internal processes: examples are "the geology of Mars" and "Lunar geology". Specialised terms such as selenology (studies of the Moon), areology (of Mars), etc., are also in use.
Although planetary geologists are interested in all aspects of the planets, a significant focus is in the search for past or present life on other worlds. This has led to many missions whose purpose (or one of their purposes) is to examine planetary bodies for evidence of life. One of these is the Phoenix lander, which analyzed Martian polar soil for water and chemical and mineralogical constituents related to biological processes.

Applied geology

Economic geology

Main article: Economic geology
Economic geologists help locate and manage the Earth's natural resources, such as petroleum and coal, as well as mineral resources, which include metals such as iron, copper, and uranium.

Mining geology

Main article: Mining
Mining geology consists of the extractions of mineral resources from the Earth. Some resources of economic interests include gemstones, metals, and many minerals such as asbestos, perlite, mica, phosphates, zeolites, clay, pumice, quartz, and silica, as well as elements such as sulfur, chlorine, and helium.

Petroleum geology

Main article: Petroleum geology
Petroleum geologists study locations of the subsurface of the Earth which can contain extractable hydrocarbons, especially petroleum and natural gas. Because many of these reservoirs are found in sedimentary basins[48], they study the formation of these basins, as well as their sedimentary and tectonic evolution and the present-day positions of the rock units.

Engineering geology

Main articles: Engineering geology, Soil mechanics, and Geotechnical engineering
Engineering geology is the application of the geologic principles to engineering practice for the purpose of assuring that the geologic factors affecting the location, design, construction, operation and maintenance of engineering works are properly addressed.
In the field of civil engineering, geological principles and analyses are used in order to ascertain the mechanical principles of the material on which structures are built. This allows tunnels to be built without collapsing, bridges and skyscrapers to be built with sturdy foundations, and buildings to be built that will not settle in clay and mud.[49]

Hydrology and environmental issues

Main article: Hydrogeology
Geology and geologic principles can be applied to various environmental problems, such as stream restoration, the restoration of brownfields, and the understanding of the interactions between natural habitat and the geologic environment. Groundwater hydrology, or hydrogeology, is used to locate groundwater,[50] which can often provide a ready supply of uncontaminated water and is especially important in arid regions,[51] and to monitor the spread of contaminants in groundwater wells.[50][52]
Geologists also obtain data through stratigraphy, boreholes, core samples, and ice cores. Ice cores[53] and sediment cores[54] are used to for paleoclimate reconstructions, which tell geologists about past and present temperature, precipitation, and sea level across the globe. These data are our primary source of information on global climate change outside of instrumental data.[55]

Natural hazards

Main article: Natural hazard
Geologists and geophysicists study natural hazards in order to enact safe building codes and warning systems that are used to prevent loss of property and life.[56] Examples of important natural hazards that are pertinent to geology (as opposed those that are mainly or only pertinent to meteorology) are:

Fields or related disciplines

Regional geology

By mountain range

By nations

By planet

See also

Environment portal
Ecology portal
Earth sciences portal
Energy portal
Main article: Outline of geology

Notes

  1. ^ Rudwick, M. J. S. (1985). The Meaning of Fossils: Episodes in the History of Palaeontology. University of Chicago Press. p. 24. ISBN 0226731030. 
  2. ^ a b Munim M. Al-Rawi and Salim Al-Hassani (November 2002). "The Contribution of Ibn Sina (Avicenna) to the development of Earth sciences". FSTC. http://www.muslimheritage.com/uploads/ibnsina.pdf. Retrieved 2008-07-01. 
  3. ^ Fielding H. Garrison wrote in the History of Medicine:
    "The Saracens themselves were the originators not only of algebra, chemistry, and geology, but of many of the so-called improvements or refinements of civilization, such as street lamps, window-panes, fireworks, stringed instruments, cultivated fruits, perfumes, spices, etc."
  4. ^ Abdus Salam (1984), "Islam and Science". In C. H. Lai (1987), Ideals and Realities: Selected Essays of Abdus Salam, 2nd ed., World Scientific, Singapore, pp. 179–213.
  5. ^ Toulmin, S. and Goodfield, J. (1965), ’The Ancestry of science: The Discovery of Time’, Hutchinson & Co., London, p. 64 (see also The Contribution of Ibn Sina to the development of Earth sciences)
  6. ^ a b Simon Winchester ; (2002). The map that changed the world: William Smith and the birth of modern geology. New York, NY: Perennial. ISBN 0060931809. 
  7. ^ James Hutton: The Founder of Modern Geology, American Museum of Natural History
  8. ^ Charles Lyell. (1991). Principles of geology. Chicago: University of Chicago Press. ISBN 9780226497976. 
  9. ^ England, Philip (2007). "John Perry's neglected critique of Kelvin's age for the Earth: A missed opportunity in geodynamics". GSA Today 17: 4. doi:10.1130/GSAT01701A.1. 
  10. ^ Winchester, Simon (2001). The Map that Changed the World. HarperCollins Publishers. pp. 25.  ISBN 0-06-093180-9
  11. ^ International Commission on Stratigraphy
  12. ^ a b Amelin, Y; Krot, An; Hutcheon, Id; Ulyanov, Aa (Sep 2002). "Lead isotopic ages of chondrules and calcium-aluminum-rich inclusions.". Science (New York, N.Y.) 297 (5587): 1678–83. doi:10.1126/science.1073950. ISSN 0036-8075. PMID 12215641. 
  13. ^ a b Patterson, C., 1956. “Age of Meteorites and the Earth.” Geochimica et Cosmochimica Acta 10: p. 230-237.
  14. ^ a b G. Brent Dalrymple (1994). The age of the earth. Stanford, Calif.: Stanford Univ. Press. ISBN 0804723311. 
  15. ^ a b c Olsen, Paul E. (2001). "Steno's Principles of Stratigraphy". Dinosaurs and the History of Life. Columbia University. http://rainbow.ldeo.columbia.edu/courses/v1001/steno.html. Retrieved 2009-03-14. 
  16. ^ Reijer Hooykaas, Natural Law and Divine Miracle: The Principle of Uniformity in Geology, Biology, and Theology, Leiden: EJ Brill, 1963.
  17. ^ As recounted in Simon Winchester, The Map that Changed the World (New York: HarperCollins, 2001), pp. 59-91.
  18. ^ Tucker, R. D.; Bradley, D. C.; Ver Straeten, C. A.; Harris, A. G.; Ebert, J. R.; McCutcheon, S. R. (1998). "New U–Pb zircon ages and the duration and division of Devonian time". Earth and Planetary Science Letters 158: 175. doi:10.1016/S0012-821X(98)00050-8.  edit
  19. ^ Hugh R. Rollinson (1996). Using geochemical data evaluation, presentation, interpretation. Harlow: Longman. ISBN 9780582067011. 
  20. ^ Gunter Faure. (1998). Principles and applications of geochemistry : a comprehensive textbook for geology students. Upper Saddle River, NJ: Prentice-Hall. ISBN 9780023364501. 
  21. ^ H. H. Hess, "History Of Ocean Basins" (November 1, 1962). IN: Petrologic studies: a volume in honor of A. F. Buddington. A. E. J. Engel, Harold L. James, and B. F. Leonard, editors. [New York?]: Geological Society of America, 1962. pp. 599–620.
  22. ^ Kious, Jacquelyne; Tilling, Robert I. (February 1996). "Developing the Theory". This Dynamic Earth: The Story of Plate Tectonics. Kiger, Martha, Russel, Jane (Online ed.). Reston, Virginia, USA: United States Geological Survey. ISBN 0-16-048220-8. http://pubs.usgs.gov/gip/dynamic/understanding.html. Retrieved 13 March 2009. 
  23. ^ Kious, Jacquelyne; Tilling, Robert I. (February 1996). "Understanding Plate Motions". This Dynamic Earth: The Story of Plate Tectonics. Kiger, Martha, Russel, Jane (Online ed.). Reston, Virginia, USA: United States Geological Survey. ISBN 0-16-048220-8. http://pubs.usgs.gov/gip/dynamic/understanding.html. Retrieved 13 March 2009. 
  24. ^ Origin of continents and oceans. S.l.: Dover Pub. 1999. ISBN 0486617084. 
  25. ^ Robert R. Compton. (1985). Geology in the field. New York: Wiley. ISBN 0471829021. 
  26. ^ "USGS Topographic Maps". United States Geological Survey. http://topomaps.usgs.gov/. Retrieved 2009-04-11. 
  27. ^ H. Robert Burger, Anne F. Sheehan, Craig H. Jones. (2006). Introduction to applied geophysics : exploring the shallow subsurface. New York: W.W. Norton. ISBN 0393926370. 
  28. ^ ed. by Wolfgang E. Krumbein (1978). Environmental biogeochemistry and geomicrobiology. Ann Arbor, Mich.: Ann Arbor Science Publ.. ISBN 0250402181. 
  29. ^ Ian McDougall, T. Mark Harrison. (1999). Geochronology and thermochronology by the ♯°Ar/©Ar method. New York: Oxford University Press. ISBN 0195109201. 
  30. ^ Bryn Hubbard, Neil Glasser. (2005). Field techniques in glaciology and glacial geomorphology. Chichester, England: J. Wiley. ISBN 0470844264. 
  31. ^ William D. Nesse. (1991). Introduction to optical mineralogy. New York: Oxford University Press. ISBN 0195060245. 
  32. ^ Morton, ANDREW C. (1985). "A new approach to provenance studies: electron microprobe analysis of detrital garnets from Middle Jurassic sandstones of the northern North Sea". Sedimentology 32: 553. doi:10.1111/j.1365-3091.1985.tb00470.x. 
  33. ^ Zheng, Y (2003). "Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China: implications for geodynamics and fluid regime". Earth-Science Reviews 62: 105. doi:10.1016/S0012-8252(02)00133-2. 
  34. ^ Condomines, M (1995). "Magma dynamics at Mt Etna: Constraints from U-Th-Ra-Pb radioactive disequilibria and Sr isotopes in historical lavas". Earth and Planetary Science Letters 132: 25. doi:10.1016/0012-821X(95)00052-E. 
  35. ^ T.J. Shepherd, A.H. Rankin, D.H.M. Alderton. (1985). A practical guide to fluid inclusion studies. Glasgow: Blackie. ISBN 0412006014. 
  36. ^ Sack, Richard O. (1987). "Experimental petrology of alkalic lavas: constraints on cotectics of multiple saturation in natural basic liquids". Contributions to Mineralogy and Petrology 96: 1. doi:10.1007/BF00375521. 
  37. ^ Alexander R. McBirney. (2007). Igneous petrology. Boston: Jones and Bartlett Publishers. ISBN 9780763734480. 
  38. ^ Frank S. Spear (1995). Metamorphic phase equilibria and pressure-temperature-time paths. Washington, DC: Mineralogical Soc. of America. ISBN 9780939950348. 
  39. ^ Dahlen, F A (1990). "Critical Taper Model of Fold-And-Thrust Belts and Accretionary Wedges". Annual Review of Earth and Planetary Sciences 18: 55. doi:10.1146/annurev.ea.18.050190.000415. 
  40. ^ Gutscher, M (1998). "Material transfer in accretionary wedges from analysis of a systematic series of analog experiments". Journal of Structural Geology 20: 407. doi:10.1016/S0191-8141(97)00096-5. 
  41. ^ Koons, P O (1995). "Modeling the Topographic Evolution of Collisional Belts". Annual Review of Earth and Planetary Sciences 23: 375. doi:10.1146/annurev.ea.23.050195.002111. 
  42. ^ Dahlen, F. A., Suppe, J. & Davis, D. J. geophys. Res. 89, 10087−10101 (1983).
  43. ^ a b c d Hodell, David A. (1994). "Magnetostratigraphic, Biostratigraphic, and Stable Isotope Stratigraphy of an Upper Miocene Drill Core from the Salé Briqueterie (Northwestern Morocco): A High-Resolution Chronology for the Messinian Stage". Paleoceanography 9: 835. doi:10.1029/94PA01838. 
  44. ^ edited by A.W. Bally. (1987). Atlas of seismic stratigraphy. Tulsa, Okla., U.S.A.: American Association of Petroleum Geologists. ISBN 0891810331. 
  45. ^ Fernández, O. (2004). "Three-dimensional reconstruction of geological surfaces: An example of growth strata and turbidite systems from the Ainsa basin (Pyrenees, Spain)". AAPG Bulletin 88: 1049. doi:10.1306/02260403062. 
  46. ^ Poulsen, Chris J. (1998). "Three-dimensional stratigraphic evolution of the Miocene Baltimore Canyon region: Implications for eustatic interpretations and the systems tract model". Geological Society of America Bulletin 110: 1105. doi:10.1130/0016-7606(1998)110<1105:TDSEOT>2.3.CO;2. 
  47. ^ Toscano, M (1999). "Submerged Late Pleistocene reefs on the tectonically-stable S.E. Florida margin: high-precision geochronology, stratigraphy, resolution of Substage 5a sea-level elevation, and orbital forcing.". Quaternary Science Reviews 18: 753. doi:10.1016/S0277-3791(98)00077-8. 
  48. ^ Richard C. Selley. (1998). Elements of petroleum geology. San Diego: Academic Press. ISBN 0-12-636370-6. 
  49. ^ Braja M. Das. (2006). Principles of geotechnical engineering. England: THOMSON LEARNING (KY). ISBN 0534551440. 
  50. ^ a b Hamilton, Pixie A. (1995). "Effects of Agriculture on Ground-Water Quality in Five Regions of the United States". Ground Water 33: 217. doi:10.1111/j.1745-6584.1995.tb00276.x. 
  51. ^ Seckler, David (1999). "Water Scarcity in the Twenty-first Century". International Journal of Water Resources Development 15: 29. doi:10.1080/07900629948916. 
  52. ^ Welch, Alan H. (1988). "Arsenic in Ground Water of the Western United States". Ground Water 26: 333. doi:10.1111/j.1745-6584.1988.tb00397.x. 
  53. ^ Barnola, J. M. (1987). "Vostok ice core provides 160,000-year record of atmospheric CO2". Nature 329: 408. doi:10.1038/329408a0. 
  54. ^ Colman, S.M. (1990). "Holocene paleoclimatic evidence and sedimentation rates from a core in southwestern Lake Michigan". Journal of Paleolimnology 4. doi:10.1007/BF00239699. 
  55. ^ Jones, P. D. (2004). "Climate over past millennia". Reviews of Geophysics 42: RG2002. doi:10.1029/2003RG000143. 
  56. ^ USGS Natural Hazards Gateway

External links

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Study guide

Up to date as of January 14, 2010
(Redirected to School:Geology article)

From Wikiversity

Welcome to the Geology School!
Jordens inre.svg
A school is a large organizational structure which can contain various departments and divisions. The departments and divisions should be listed in the departments and divisions section. The school should not contain any learning resources. The school can contain projects for developing learning resources.

Divisions and departments

Divisions and Departments of the School exist on pages in "topic" namespace. Start the name of departments with the "Topic:" prefix; departments reside in the Topic: namespace. .Departments and divisions link to learning materials and learning projects.^ The geology department has replaced traditional lectures with project-oriented lectures/labs so that students learn geology in authentic problem-oriented settings.
  • Dickinson College - Geology 16 January 2010 4:31 UTC www.dickinson.edu [Source type: Academic]

 Divisions can link subdivisions or to departments. .For more information on schools, divisions and departments look at the Naming Conventions.^ Can I add new entries to the Geographic Names Information System for manmade and administrative features, such as churches, cemeteries, schools, shopping centers, etc.?
  • Welcome to the USGS - U.S. Geological Survey 16 January 2010 4:31 UTC www.usgs.gov [Source type: General]

 ^ Nate wrote 1 day ago : Every Friday throughout the school year, the Kent State University Department of Geology welcomes gu … more → .
  • Geology — Blogs, Pictures, and more on WordPress 16 January 2010 4:31 UTC en.wordpress.com [Source type: General]

 ^ For more information on the geology of Ambergris Caye and Belize, click here for a study by Dr. Sal Mazzullo, Department of Geology, Wichita State University.
  • Geology of Belize, Geologic History of Ambergris Caye, Belize 16 January 2010 4:31 UTC ambergriscaye.com [Source type: FILTERED WITH BAYES]

Fields and related disciplines

An illustrated depiction of a syncline and anticline commonly studied in Structural geology and Geomorphology.

Learning projects

Active participants

.The histories of Wikiversity pages indicate who the active participants are.^ I hope my regular visitors will actively participate in the NY Geology Resource Page.
  • New York Geology Resource Forum-Earth Science information, links, and more. 16 January 2010 4:31 UTC newyork.geology-forum.com [Source type: General]

 .If you are an active participant in this school, you can list your name here (this can help small schools grow and the participants communicate better; for large schools it is not needed).^ After having gone to a small school where you know everyone and everyone knows you it was quite a change to be at a school where I did not even know all the geology professors let alone students.
  • Alumni (Bowdoin, Geology) 16 January 2010 4:31 UTC www.bowdoin.edu [Source type: FILTERED WITH BAYES]

 ^ There are a number of resources online and in the department to help you study for the GRE, pick a graduate program, get letters of recommendation, and strengthen your résumé.
  • Blogs | Geology and Astronomy 16 January 2010 4:31 UTC geology.wcupa.edu [Source type: FILTERED WITH BAYES]

 ^ Moshier are active in their church in Geneva IL, currently helping in the youth (middle school) ministry.
  • Wheaton College (Wheaton, IL) - Geology Faculty 16 January 2010 4:31 UTC www.wheaton.edu [Source type: Academic]

 Please remember: if you have an account here people can write you a message also in the future, because IP addresses change !
  • .chantelle
  • Ravi Arya
  • Chrissy
  • Rahul Sharma
  • James89
  • Extremekd
  • User:Goodguy007

School news

  • 26 August 2006 - School founded!

External links for learning


1911 encyclopedia

Up to date as of January 14, 2010
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Wikibooks

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(Redirected to General Geology article)

From Wikibooks, the open-content textbooks collection

Terra globe icon.png
.Geology (from Greek γη- (ge-, "the earth") and λογος ("logos", "word", "reason")) is the science and study of the solid matter of a celestial body, its composition, structure, physical properties, history and the processes that shape it.^ X6yos, science), the science which investigates the physical history of the earth.

 ^ Rocks and the Rock Cycle Earth's Layers and Moving Plates Fossils and Earth History Scientists Who Study Rocks Earth Science Literacy Framework .

 ^ Designed to introduce upper-undergraduate/first-year-graduate students in earth sciences and natural resources to the study of hydrologic science.
  • TCU Geology Graduate Programs 16 January 2010 4:31 UTC www.geo.tcu.edu [Source type: Academic]

 .In this book, the term Geology will apply to the Earth in particular.^ In this book, the term Geology will apply to the Earth in particular.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Welcome to the GEOLOGY Home Page Lower Columbia College Geology is the study of Earth, in particular it's rocks and minerals, and the processes that create and modify them.
  • LCC GEOLOGY Home Page 07/08/02 a.m. 16 January 2010 4:31 UTC lcc.ctc.edu [Source type: Academic]

 ^ Geology: History of the Earth: Environments of Our Past : Journey through the history of the Earth, with stops at particular points in time to examine the fossil record and stratigraphy .
  • Kidinfo.com - Your Guide to Information About Geology and Geological Topics 16 January 2010 4:31 UTC www.kidinfo.com [Source type: General]
.Geology can be split into two main branches: historical and physical.^ In 1943 the Chair of Geology split into two chairs: the Chair of Historical Geology and the Chair of Dynamic Geology.
  • Faculty of Geology >> Geology at Moscow State University 16 January 2010 4:31 UTC www.geol.msu.ru [Source type: Academic]

 ^ Geology can be split into two main branches: historical and physical.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Paleoclimatology and Paleoceanography are two of the most important branches of geology because they provide insight into how the Earth might respond to Global Warming.
  • Geology As a Career 16 January 2010 4:31 UTC www.ohio.edu [Source type: FILTERED WITH BAYES]

 .Historical geology attempts to understand the origins, composition, systems and changes of the Earth.^ Earth history - Historical geology and stratigraphy .
  • geology (science) -- Britannica Online Encyclopedia 16 January 2010 4:31 UTC www.britannica.com [Source type: Academic]

 ^ They provide an understanding of the origin, structure, composition and history of the earth.
  • About Geology 16 January 2010 4:31 UTC www.capilanou.ca [Source type: Academic]

 ^ Geology is the study of the origins of Earth, composition, processes and Earth history.
  • Geology and Geological Engineering Home 16 January 2010 4:31 UTC www.olemiss.edu [Source type: Academic]

Contents

History

.According to the widely accepted Big Bang theory, the Universe began at some point in space and time around 13,700,000,000 years ago, as evidenced by the doppler effect observed in all stars and a 3 degree Kelvin background radiation observed elsewhere.^ According to the widely accepted Big Bang theory, the Universe began at some point in space and time around 13,700,000,000 years ago, as evidenced by the doppler effect observed in all stars and a 3 degree Kelvin background radiation observed elsewhere.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ SCENE X: 12,000 Years Ago .
  • A Pictorial History of Albuquerque Area Geology - Albuquerque's Environmental Story 16 January 2010 4:31 UTC www.cabq.gov [Source type: FILTERED WITH BAYES]

 ^ The oldest particle on Earth, a zircon crystal from 4.4 billion years ago, was found in Western Australia* - closest to the time when Time on Earth began.
  • :: OZ Greetings :: - Geology Articles 16 January 2010 4:31 UTC oz-greetings.com.au [Source type: FILTERED WITH BAYES]
.
  • In about 10E-43 seconds, physics became defined and gravity separated from other forces.^ In about 10E-43 seconds, physics became defined and gravity separated from other forces.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ Other physical properties of minerals that aid in identification are crystal form , cleavage type, fracture, streak, lustre, colour, specific gravity , and density.
    • geology (science) -- Britannica Online Encyclopedia 16 January 2010 4:31 UTC www.britannica.com [Source type: Academic]

     ^ The temperature was 1027 K. At 10E-6 seconds, quarks began to bind into protons and neutrons; matter and antimatter destroyed each other and the balance turned out to be in favor of matter.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     .The Universe was 10E32 K in temperature.
  • At 10E-35 seconds, the Universe expanded to the size of a softball and the strong nuclear force separated.^ At 10E-35 seconds, the Universe expanded to the size of a softball and the strong nuclear force separated.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ The temperature was 1027 K. At 10E-6 seconds, quarks began to bind into protons and neutrons; matter and antimatter destroyed each other and the balance turned out to be in favor of matter.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ In about 10E-43 seconds, physics became defined and gravity separated from other forces.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     .Energy turned into quarks and electrons and their anti-matter counterparts.^ Energy turned into quarks and electrons and their anti-matter counterparts.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ Mixed with this sediment was organic matter, that under the heat and pressure of burial, turned into petroleum and natural gas.
    • Gulf Coast Geology | Educator and Student Resources | Gulf of Mexico Program | US EPA 16 January 2010 4:31 UTC www.epa.gov [Source type: News]

     ^ The temperature was 1027 K. At 10E-6 seconds, quarks began to bind into protons and neutrons; matter and antimatter destroyed each other and the balance turned out to be in favor of matter.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     .The temperature was 1027 K.
  • At 10E-6 seconds, quarks began to bind into protons and neutrons; matter and antimatter destroyed each other and the balance turned out to be in favor of matter.^ Energy turned into quarks and electrons and their anti-matter counterparts.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ The temperature was 1027 K. At 10E-6 seconds, quarks began to bind into protons and neutrons; matter and antimatter destroyed each other and the balance turned out to be in favor of matter.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ Rain falling on this material dissolved some of the calcite skeletal fragments and then precipitated this calcite in between other grains to cement all of the grains together and turn the material into a limestone.
    • Geology of Belize, Geologic History of Ambergris Caye, Belize 16 January 2010 4:31 UTC ambergriscaye.com [Source type: FILTERED WITH BAYES]

     .The Universe was about the size of our solar system and 1013 K hot.
  • 1 second after its inception, the electromagnetic and weak nuclear forces appeared as the Universe cooled to 109 K.
  • 3 minutes later, protons and neutrons fused into nuclei.
  • After 100,000 years, the electrons and the nuclei came together to form atoms; photons separated from matter and there was light.
  • In the next 1,000,000,000 years the Universe became clumpy as galaxies began to take shape.
  • Ever since then, the Universe has cooled down to 3 K, galaxies have developed, generations of stars have passed, creating heavier elements, and life has appeared.^ In the next 1,000,000,000 years the Universe became clumpy as galaxies began to take shape.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ Ever since then, the Universe has cooled down to 3 K, galaxies have developed, generations of stars have passed, creating heavier elements, and life has appeared.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ At 10E-35 seconds, the Universe expanded to the size of a softball and the strong nuclear force separated.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     .Our galaxy, the Milky Way, contains about 200,000,000,000 stars and lies 1 million light years from its nearest neighbor.
  • The solar system was formed around 4,600,000,000 years ago as dust collapsed into the protostar that was to become the Sun, and into planetesimals orbiting it.^ The solar system was formed around 4,600,000,000 years ago as dust collapsed into the protostar that was to become the Sun, and into planetesimals orbiting it.
    • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

     ^ The Appalachian Mountains were formed by uplifting of the land about 225 million years ago.
    • WVGES Geology: Geology of the New River Gorge 16 January 2010 4:31 UTC www.wvgs.wvnet.edu [Source type: FILTERED WITH BAYES]

     ^ Scientists believe Earth was formed 4,600 million years ago.
    • SDTV: Episode Resources - Geology 16 January 2010 4:31 UTC www.pbs.org [Source type: FILTERED WITH BAYES]

     The inner planets, from Mercury to Mars, are solid because the solar winds have driven gases away and have a core; the outer planets are larger and consist of gas.

Structure and Composition of the Earth

.The outermost layer of the earth is called the lithosphere (100-200km deep); it is followed by a plastic asthenosphere (150-400km deep).^ The outermost layer of the earth is called the lithosphere (100-200km deep); it is followed by a plastic asthenosphere (150-400km deep).
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ As the crust broke and thinned, basaltic magma generated 50 to 100 kilometers deep in the earth rose to the surface.
  • LakeSuperiorStreams - Regional Geology 16 January 2010 4:31 UTC www.duluthstreams.org [Source type: FILTERED WITH BAYES]

 ^ Introductory Courses (6 cr) 100 Global Environmental Change plus one of the following: 102 The Human Landscape 150 The Imperiled Earth: World Environmental Issues .
  • Geosciences 16 January 2010 4:31 UTC www.umass.edu [Source type: Academic]

 .Independent of these classifications, the internal structure of the earth is divided into three main layers: the crust, the mantle and the core.^ Independent of these classifications, the internal structure of the earth is divided into three main layers: the crust, the mantle and the core.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The structure of a specific region of the earth's crust.
  • Geology Definition | Definition of Geology at Dictionary.com 16 January 2010 4:31 UTC dictionary.reference.com [Source type: Academic]
  • University of North Carolina Wilmington - The Career Center - Explore and Research Careers 16 January 2010 4:31 UTC www.uncwil.edu [Source type: Academic]
  • Kids Online Resources - Science, Geology 16 January 2010 4:31 UTC www.kidsolr.com [Source type: FILTERED WITH BAYES]
  • Kid Science Link - Geology Index 16 January 2010 4:31 UTC www.kidsciencelink.com [Source type: Academic]

 ^ These rocks are divided into three classes.
.The crust, which is solid and mainly made up of silicates, can be divided into continental crust and oceanic crust.^ The crust, which is solid and mainly made up of silicates, can be divided into continental crust and oceanic crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The oceanic crust is much thinner than the continental crust, with an average thickness of just 5km.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ However, the largest island, Isabela, is made up of six volcanoes which have flowed into each other, filling the Pacific gap between them.
  • Galapagos Islands .com - Geology of the Galapagos Islands 16 January 2010 4:31 UTC www.galapagosislands.com [Source type: General]

 .The continental crust ranges in thickness from 35-60km.^ The continental crust ranges in thickness from 35-60km.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The oceanic crust is much thinner than the continental crust, with an average thickness of just 5km.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The crust is here assumed to be of approximately uniform thickness, thus a mountain range would be underlain by lighter rocks.
  • Glossary of Geological Terms 16 January 2010 4:31 UTC www.geotech.org [Source type: FILTERED WITH BAYES]

 .It is andesitic in composition, with a Si02 composition of 57% by weight.^ It is andesitic in composition, with a Si0 2 composition of 57% by weight.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .95% of crustal rocks are igneous and metamorphic, while only 5% are sedimentary.^ The classification, origin, occurrence and associations of igneous, sedimentary, and metamorphic rocks.
  • Geology 16 January 2010 4:31 UTC www.shsu.edu [Source type: Academic]

 ^ Recall that there are igneous, sedimentary, and metamorphic rocks.

 ^ Three basic types of rock are igneous, sedimentary, and metamorphic .
  • The Slackpacker's Geology Primer 16 January 2010 4:31 UTC www.slackpacker.com [Source type: FILTERED WITH BAYES]

 .These range from granite near the surface to gabbro, deep down near the mantle.^ These range from granite near the surface to gabbro, deep down near the mantle.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Metamorphic grade of these rocks ranges from middle greenschist in the western part of the mine to middle amphibolite facies in the deep, eastern section of the mine.

 ^ Hot, liquid rock (magma) is injected into existing bedrock, cooling and resolidifying into granite deep below the earth's surface.
  • A Pictorial History of Albuquerque Area Geology - Albuquerque's Environmental Story 16 January 2010 4:31 UTC www.cabq.gov [Source type: FILTERED WITH BAYES]

 .The oceanic crust is much thinner than the continental crust, with an average thickness of just 5km.^ The oceanic crust is much thinner than the continental crust, with an average thickness of just 5km.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ By the end of this project, you will know a lot more about geysers and understand that a geyser is much more than just a water-spouting hole in the ground!

 ^ Employment of environmental scientists is expected to increase by 25 percent between 2006 and 2016, much faster than the average for all occupations.
  • Geology 16 January 2010 4:31 UTC www.lonestar.edu [Source type: FILTERED WITH BAYES]

 .It is denser than the continental crust and mainly composed of basaltic rocks, giving it a SiO2 content of 49% by weight.^ It is denser than the continental crust and mainly composed of basaltic rocks, giving it a SiO 2 content of 49% by weight.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The oceanic crust is much thinner than the continental crust, with an average thickness of just 5km.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ In the transition zone, due to higher pressure at a greater depth, rocks have more closely packed structures than those in the upper mantle and crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .The atmosphere, hydrosphere and biosphere are often also considered to be part of the crust.^ Intersection of the biosphere, atmosphere, hydrosphere, and geosphere.

 ^ The atmosphere, hydrosphere and biosphere are often also considered to be part of the crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Application of basic chemical principles to understanding the origin, distribution and migration of chemical elements in the earth's lithosphere, hydrosphere, atmosphere and biosphere.
  • TCU Geology Graduate Programs 16 January 2010 4:31 UTC www.geo.tcu.edu [Source type: Academic]
.The mantle stretches from the base of the crust to approximately 2900km, and is divided into three zones: the upper mantle, the transition zone and the lower mantle.^ The mantle stretches from the base of the crust to approximately 2900km, and is divided into three zones: the upper mantle, the transition zone and the lower mantle.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Generally speaking, cave animals are divided into three categories: .
  • Ruby Falls\' Geology - Ruby Falls 16 January 2010 4:31 UTC www.rubyfalls.com [Source type: General]

 ^ The transition zone, between the upper and lower mantle, is marked by polymorphic phase transition from spinel and pyroxene to ilmenite and rutile, then eventually to stishovite.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .The upper mantle is rich in dunite, peridotite and eclogite rocks, and is heterogeneous (probably due to partial melting of mantle magmas).^ Magma is continuous extracted from the upper mantle.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Petrology and melting of the upper mantle is discussed.

 ^ The upper mantle is rich in dunite, peridotite and eclogite rocks, and is heterogeneous (probably due to partial melting of mantle magmas).
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .Magma is continuous extracted from the upper mantle.^ Magma is continuous extracted from the upper mantle.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The upper mantle is rich in dunite, peridotite and eclogite rocks, and is heterogeneous (probably due to partial melting of mantle magmas).
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .The transition zone, between the upper and lower mantle, is marked by polymorphic phase transition from spinel and pyroxene to ilmenite and rutile, then eventually to stishovite.^ The transition zone, between the upper and lower mantle, is marked by polymorphic phase transition from spinel and pyroxene to ilmenite and rutile, then eventually to stishovite.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ In the transition zone, due to higher pressure at a greater depth, rocks have more closely packed structures than those in the upper mantle and crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Asteroid and Dinosaurs: An asteroid apparently marked the transition between the dinosaur age and modern biology.
  • Crank Dot Net | geology 16 January 2010 4:31 UTC www.crank.net [Source type: FILTERED WITH BAYES]

 .In the transition zone, due to higher pressure at a greater depth, rocks have more closely packed structures than those in the upper mantle and crust.^ In the transition zone, due to higher pressure at a greater depth, rocks have more closely packed structures than those in the upper mantle and crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Formation of the Appalachians Some rocks in the core of the Appalachian Mountains are more than 1 billion years old and construction of the mountains relates to the Supercontinent Pangea.

 ^ The transition zone, between the upper and lower mantle, is marked by polymorphic phase transition from spinel and pyroxene to ilmenite and rutile, then eventually to stishovite.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 .The lower mantle appears to be homogeneous, with even denser, very closely packed materials.^ The lower mantle appears to be homogeneous, with even denser, very closely packed materials.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ In the transition zone, due to higher pressure at a greater depth, rocks have more closely packed structures than those in the upper mantle and crust.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The rock composing the summit [ Red Lake Peak, 1844 ] consists of a very coarse, dark, volcanic conglomerate; the lower parts appeared to be of a slaty structure .
  • Geology 16 January 2010 4:31 UTC www.longcamp.com [Source type: FILTERED WITH BAYES]
.Physical properties of the earth's core suggest that it is made up mainly of iron and nickel allows.^ Physical properties of the core suggest that it is made up mainly of iron and nickel alloys.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Physical properties of the earth's core suggest that it is made up mainly of iron and nickel allows.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Lesson 3: Density Students explore the properties that allow objects and liquids to float and use this information to infer the composition of the Earth’s layers.

 .The outer core is liquid, while the inner core is solid.^ The outer core is liquid, while the inner core is solid.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The inner planets, from Mercury to Mars, are solid because the solar winds have driven gases away and have a core; the outer planets are larger and consist of gas.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The Earth's core is 2,200 miles thick, and is composed mainly of iron , partly liquid and partly solid.
  • geology@Everything2.com 16 January 2010 4:31 UTC www.everything2.com [Source type: FILTERED WITH BAYES]

 .Physical properties of the core suggest that it is made up mainly of iron and nickel alloys.^ Physical properties of the core suggest that it is made up mainly of iron and nickel alloys.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Physical properties of the earth's core suggest that it is made up mainly of iron and nickel allows.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The continent of Africa is made up of a vast stable crystalline basement of very old rocks, mainly of Precambrian age.

Plate Tectonics

.Because of the interactions between the lithosphere, the asthenosphere, and the mantle underneath, our planet's crust is governed by 'plate tectonics.'^ Because of the interactions between the lithosphere, the asthenosphere, and the mantle underneath, our planet's crust is governed by 'plate tectonics.'
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Moving on, the "Plate Tectonics" area includes the "Continents Over Time" interactive feature which asks visitors to place images of the continents in the correct geologic order.

 ^ This Dynamic Earth: The Story of Plate Tectonics Online book includes historical perspective, developing the theory, understanding plate motions, mantle thermal plumes, & plate tectonics and people.
.Plate tectonics is a theory based on the principle of Uniformitarianism, which reads: "The Present is the Key to the Past."^ Plate tectonics is a theory based on the principle of Uniformitarianism, which reads: "The Present is the Key to the Past."
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The Geological Evolution of the Earth - A visual synopsis of plate tectonics from the Cambrian era to the present .
  • Geology Study - Geology Learning - Geology Facts 16 January 2010 4:31 UTC www.resourcehelp.com [Source type: FILTERED WITH BAYES]

 ^ Their scientific detective work on events in deep geological time helps us to understand the present, and both past and present are key to predicting the future.
  • http://www.canterbury.ac.nz/subjects/geol/ 16 January 2010 4:31 UTC www.canterbury.ac.nz [Source type: Academic]

 .The earth in its current state is the result of natural processes operating over vast periods of time, and can be understood by watching the action of ongoing processes.^ The earth in its current state is the result of natural processes operating over vast periods of time, and can be understood by watching the action of ongoing processes.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ The Abiotic Theory of Petroleum Formation Most scientists believe that oil comes from organic material that has been transformed by Nature over a very long period of time.

 ^ To help make the Earth a better place, you must understand the processes that operate in its interior and on its surface.
  • Geology and Environmental Geosciences 16 January 2010 4:31 UTC www.lafayette.edu [Source type: Academic]

Volcanism

.There are three(3) types of lavas formed by volcanoes.^ There are three(3) types of lavas formed by volcanoes.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]

 ^ Generally, the individual islands form from single shield volcano's eruptions of basaltic lava flows expanding its shores.
  • Galapagos Islands .com - Geology of the Galapagos Islands 16 January 2010 4:31 UTC www.galapagosislands.com [Source type: General]

 ^ There is a distinctive line showing where the collision occured and each continent was formed by a different type of rock.

 .Mafic, Intermediate, and Felsic.^ Mafic, Intermediate, and Felsic.
  • General Geology - Wikibooks, collection of open-content textbooks 16 January 2010 4:31 UTC en.wikibooks.org [Source type: FILTERED WITH BAYES]
Mafic(Basaltic)
  • %SiO2: < 50%
  • %FeMg: 4%
  • Temp: up to 1500C
  • Viscosity: Low
  • Eruptive Behavior: gentle
  • Distribution: divergent plate boundries, hot spots, convergent plate boundries
Intermediate(Andesitic)
  • %SiO2: ~60%
  • %FeMg: ~3%
  • Temp: ~1000C
  • Viscosity: Intermediate
  • Eruptive Behavior: explosive
  • Distribution: convergent plate boundries
Felsic (Rhyolitic)
  • %SiO2: >70%
  • %FeMg: 2%
  • Temp: 700C
  • Viscosity: High
  • Eruptive Behavior: explosive
  • Distribution: hot spots in continental crusts (Yellowstone National Park), convergent plate boundries

Simple English

File:MSH80 david johnston at camp 05-17-80
The geologist, David Johnston, on the side of Mount St. Helens.

Geology is the study of the nonliving things that the Earth is made of. Geology is the study of soil and rocks. The people that study geology are called geologists. By studying the soil and rocks that the Earth's surface is made of, Geologists can learn more about the history of the Earth.

Some of the important events (things that happen) in the Earth's history are floods, volcanic eruptions, earthquakes, orogeny (mountain building), and plate tectonics (movement of continents). Some Geologists study soil and rocks to find minerals, like metals and oil, which are underground.

Geology is divided into smaller subjects that just study one part of Geology.

Some of these subjects are:

  • Petrology - the study of rocks how they form and where they are from.
  • Mineralogy - the study of minerals.
  • Stratigraphy - the study of layered sedimentary rocks and how they were deposited.
  • Structural geology - the study of folds and faults and how mountains are formed by uplift.
  • Geomorphology - the study of the shape (=morphology) of the surface of the Earth and the formation of soil from rock.
  • Historical geology - the history of the events that shaped the Earth in the last 4.5 million years.
  • Palaeontology - the study of fossils (the remains of animals from long ago).
  • Hydrogeology - the study of water under the surface of the Earth
  • Volcanology - the study of volcanoes on land or under the ocean.
  • Seismology - the study of earthquakes and strong ground-motion.
  • Engineering Geology - the study of geologic hazards (such as landslides and earthquakes) applied to civil engineering.
  • Petroleum Geology - the study of petroleum deposits in sedimentary rocks.

Contents

Types of rock

Rocks can be found in all sorts of shapes and colours. Some are very hard and some are soft. Some rocks are very common, while others are rare. However, all the different rocks belong to three categories or types, igneous, sedimentary and metamorphic.

Igneous rock

Igneous rock is rock that has been made by volcanic action. Igneous rock is made when the lava (melted rock on the surface of the Earth) or magma (melted rock below the surface of the Earth) cools down and becomes hard. Igneous rock formed from magma that has become solid inside the earth is called intrusive igneous rock. Igneous rock formed from lava that has become solid on the outside of the Earth is called extrusive igneous rock. This can happen because of the eruption of a volcano. Some extrusive igneous rock types are basalt, andesite, rhyolite, tuff, obsidian, and pumice. Examples of intrusive igneous rock types are gabbro, diorite, and granite.

Sedimentary rock

Sedimentary rock is rock that has been made from "sediment". "Sediment" is all solid pieces of stuff that are moved by the wind, water, or glaciers. Sediment can be made from clay, sand, gravel and the bodies and shells of animals. The sediment gets dropped in a layer at the bottom of a river or sea. As the sediment piles up, the lowers layers get squashed together. Slowly they set hard into rock. Some sedimentary rocks are made of just one type of sediment, all about the same size, such as sand. Other sedimentary rocks will have large and small lumps, and pieces made of different types of rock. Well-known sedimentary rocks are sandstone and limestone.

Metamorphic rock

Metamorphic rock is rock that has been changed. The word "metamorphosis" means "change". Sometimes an igneous, or a sedimentary rock can be heated, or squashed under the ground, so that it changes. Metamorphic rock is often harder than the rock that it was before it changed. One well-known metamorphic rock is marble which is valued for its different colours, and because it can be carved and polished. Slate is a metamorphic rock that is a useful building material.

Faults

All three kinds of rock can be changed by being heated and squeezed by forces in the earth. When this happens, faults (cracks) may appear in the rock. Geologists can learn a lot about the history of the rock by studying the patterns of the fault lines. Earthquakes are caused when a fault breaks suddenly.

Soil

Soil is the stuff on the ground made of lots of "particles" (or tiny pieces). The particles of soil come from rocks that have broken down, and from rotting leaves and animals bodies. Soil covers a lot of the surface of the Earth. Plants of all sorts grow in soil.

To find out more about types of rocks, go to Rock (geology). To find out more about soil, go to Soil.

Principles of Geology

Geologists use some simple ideas which help them to understand the rocks and soil that they are studying. These ideas are called the "Principles of Geology".

  1. Understanding the past: Geologist James Hutton said "The present is the key to the past". He meant that the sort of changes that are happening to the Earth's surface now are the same sorts of things that happened in the past. Geologists can understand things that happened millions of years ago, by looking at the changes which are happening today.
  2. Horizontal strata: The layers in a sedimentary rock must have been horizontal (flat) when they were deposited. (laid down).
  3. The age of the strata: Layers at the bottom must be older than layers at the top, unless all the rocks have been turned over.
  4. In sedimentary rocks that are made of sand or gravel, the sand or gravel must have come from an older rock.
  5. The age of faults: If there is a crack or fault in a rock, then the fault is younger than the rock. Rocks are in strata (lots of layers). A geologist can see if the faults go through all the layer, or only some. This helps to tell the age of the rocks.
  6. The age of a rock which cuts through other rocks: If an igneous rock cuts across sedimentary layers, it must be younger than the sedimentary rock.
  7. The relative age of fossils: A fossil in one rock type must be about the same age as the same type of fossil in the same type of rock in a different place. Likewise, a fossil in a rock layer below must be earlier than one in a higher layer.
Appalachian

A fault cutting through older sedimentary rocks

Schunemunk conglomerate and

Sedimentary rock made from white pieces of older rock, that were broken up and mixed with red sand at the bottom of a river.

Zimbabwe great

The Zimbabwe Great Dyke: A big band of igneous rock cuts between sedimentary rocks. This picture was taken from a satellite.

DirkvdM

Beaches are interesting places to study Geology,

Microplis dans filon d'

This rock-face in France contains the mineral Mica.

Geological

A simple, important tool for the Geologist.

Drill-bit 5 7-8inch

Geologists often use drills like this to take "samples" of stone from the Earth.

Diamond

A young Butcher Bird is standing on a box of samples of rock that have been drilled from underground.

Exploration

Geologists look at some samples of rock, to find minerals for mining.

S East

A map showing the geology of South East England. This area has been studied for hundreds of years.

Southern-ocean sediment

A map showing the different soils and rocks under the Southern Ocean. Geologists are finding new information about this area.

682px-Plates tect2

This map shows the main "plates" of the Earth's surface and which way they are moving.

Deep sea vent chemistry

This diagram shows what happens when a volcano erupts under the ocean

Other pages

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