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Lassen Volcanic National Park
IUCN Category II (National Park)
Location Shasta, Lassen, Plumas, and Tehama Counties, California, USA
Nearest city Redding
Coordinates 40°29′17″N 121°30′18″W / 40.48806°N 121.505°W / 40.48806; -121.505Coordinates: 40°29′17″N 121°30′18″W / 40.48806°N 121.505°W / 40.48806; -121.505
Area 106,000 acres (42,900 ha)
Established August 9, 1916
Visitors 395,057 (in 2007)
Governing body National Park Service
Map of Lassen Volcanic National park
Mount Shasta from Lassen Peak

Lassen Volcanic National Park is a United States National Park in northeastern California. The dominant feature of the park is Lassen Peak; the largest plug dome volcano in the world and the southern-most volcano in the Cascade Range. Lassen Volcanic National Park started as two separate national monuments designated by President Theodore Roosevelt in 1907: Cinder Cone National Monument and Lassen Peak National Monument.

The source of heat for volcanism in the Lassen area is subduction off the Northern California coast of the Gorda Plate diving below the North American Plate. The area surrounding Lassen Peak is still active with boiling mud pots, stinking fumaroles, and churning hot springs. Lassen Volcanic National Park is one of the few areas in the world where all four types of volcano can be found (plug dome, shield, cinder cone, and strato).

The park is accessible via State Routes SR 89 and SR 44. SR 89 passes north-south through the park, beginning at SR 36 to the south and ending at SR 44 to the north. SR 89 passes immediately adjacent the base of Lassen Peak.

There are a total of five vehicle entrances to the park: the north and south entrances of SR 89, and unpaved roads entering at Drakesbad and Juniper Lake in the south, and Butte Lake in the northeast. The Park can also be accessed by trails leading in from Caribou Wilderness to the east, as well as the Pacific Crest Trail, and two smaller trails leading in from Willow Lake and Little Willow Lake to the south.

A large lodge (the Lassen Chalet) with concession facilities formerly was located near the south-west entrance, but was demolished in 2005. A new, full-service visitor center was constructed in the same location, and opened to the public in 2008. Near the old lodge location was also located Lassen Ski Area, which ceased operation in 1992; all infrastructure has been removed.



Native Americans have inhabited the area long before white settlers first saw Lassen. The natives knew that the peak was full of fire and water and thought that it would one day blow itself apart.[1]

White immigrants in the mid-19th century used Lassen Peak as a landmark on their trek to the fertile Sacramento Valley. One of the guides to these immigrants was a Danish blacksmith named Peter Lassen, who settled in Northern California in the 1830s. Lassen Peak was named after him.[1] Nobles Emigrant Trail was later cut through the park area and passed Cinder Cone and the Fantastic Lava Beds.

Inconsistent newspaper accounts reported by witnesses from 1850-1851 described seeing "fire thrown to a terrible height" and "burning lava running down the sides" in the area of Cinder Cone. As late as 1859 a witness reported seeing fire in the sky from a distance, attributing it to an eruption. Early geologists and volcanologists who studied the Cinder Cone concluded the last eruption occurred between 1675 and 1700. After the 1980 eruption of Mount St. Helens, the United States Geological Survey (USGS) began reassessing the potential risk of other active volcanic areas in the Cascade Range. Further study of Cinder Cone estimated the last eruption occurred between 1630 and 1670.

The Lassen area was first protected by being designated as the Lassen Peak Forest Preserve. Lassen Peak and Cinder Cone were later declared as U.S. National Monuments in May 1907 by President Theodore Roosevelt.[2]

Brokeoff Mountain, Lassen Peak, and Chaos Crags, from left to right. The area of Lassen Peak that was lost during the 1914-15 volcanic event is visible in this picture, encompassing the sliver of snow.

Starting in May 1914 and lasting until 1921, a series of minor to major eruptions occurred on Lassen. These events created a new crater, and released lava and a great deal of ash. Fortunately, because of warnings, no one was killed, but several houses along area creeks were destroyed. Because of the eruptive activity, which continued through 1917, and the area's stark volcanic beauty, Lassen Peak, Cinder Cone and the area surrounding were declared a National Park on August 9, 1916.[1]

The 29-mile (47 km) Main Park Road was constructed between 1925 and 1931, just 10 years after Lassen Peak erupted. Near Lassen Peak the road reaches 8,512 feet (2,594 m), making it the highest road in the Cascade Mountains. It is not unusual for 40 ft (12 m) of snow to accumulate on the road near Lake Helen and for patches of snow to last into July.

In October 1972, a portion of the park was designated as Lassen Volcanic Wilderness by the US Congress (Public Law 92-511). Since then, additional park land has been added for a total of 104,594 acres of wilderness, comprising most of the park. The National Park Service manages the wilderness in keeping with the Wilderness Act of 1964, with minimal developed facilities, signage, trails and bridges only where "essential at key stream crossings." The management plan of 2003 adds that, "The wilderness experience offers a moderatee to high degree of challenge and adventure." [3]

In 1974 the United States Park Service took the advice of the USGS and closed the visitor center and accommodations at Manzanita Lake. The Survey stated that these buildings would be in the way of a rockslide from Chaos Crags if an earthquake or eruption occurred in the area.[1] An aging seismograph station remains. However, a campground, store, and museum dedicated to Benjamin F. Loomis stands near Manzanita Lake, welcoming visitors who enter the park from the northwest entrance.

After the Mount St. Helens eruption, the USGS intensified its monitoring of active and potentially active volcanoes in the Cascade Range. Monitoring of the Lassen area includes periodic measurements of ground deformation and volcanic-gas emissions and continuous transmission of data from a local network of nine seismometers to USGS offices in Menlo Park, California.[4] Should indications of a significant increase in volcanic activity be detected, the USGS will immediately deploy scientists and specially designed portable monitoring instruments to evaluate the threat. In addition, the National Park Service (NPS) has developed an emergency response plan that would be activated to protect the public in the event of an impending eruption.

Visitors To Lassen National Park by Year [5]
Year Recreational Visitors
2008 377,361
2007 395,057
2006 388,741
2005 365,535
2004 379,667

This table shows that visitors to Lassen increased in 2007 but have since fallen off below 2004 levels in 2008. The National Park Service counts visitors to Lassen National Park by using in-road inductive loops at all the vehicle entrances to count vehicles entering the park. Buses and other non reportable vehicles are subtracted from the vehicle counts and then a persons-per-vehicle multiplier of 3 is multiplied by the vehicle number.[6]

Geography and climate

Map of Lassen area showing hydrothermal features (red dots) and volcanic feature or remnant (yellow cones). Also shown is the outline of Brokeoff Volcano.

The park is located near the northern end of the Sacramento Valley. The western part of the park features great lava pinnacles (huge mountains created by lava flows), jagged craters, and steaming sulphur vents. It is cut by glaciated canyons and is dotted and threaded by lakes and rushing clear streams.

The eastern part of the park is a vast lava plateau more than one mile (1.6 km) above sea level. Here are found small cinder cones (Fairfield Peak, Hat Mountain, and Crater Butte).[7] Forested with pine and fir, this area is studded with small lakes, but it boasts few streams. Warner Valley, marking the southern edge of the Lassen Plateau, features hot spring areas (Boiling Springs Lake, Devils Kitchen, and Terminal Geyser).[7] This forested, steep valley also has large meadows that have wildflowers in spring.

Lassen Peak is made of dacite, and is one of the world's largest plug dome volcanoes. It is also the southernmost non-extinct volcano of the Cascade Range (specifically, the Shasta Cascade part of the range). 10,457-foot (3,187 m) tall volcano sits on the north-east flank of the remains of Mount Tehama, a stratovolcano that was a thousand feet (305 m) higher than Lassen and 11 to 15 miles (18 to 24 km) wide at its base.[1] After emptying its throat and partially doing the same to its magma chamber in a series of eruptions, Tehama either collapsed into itself and formed a two-mile (3.2 km) wide caldera in the late Pleistocene or was simply eroded away with the help of acidic vapors that loosened and broke the rock, which was later carried away by glaciers.

On the other side of the present caldera is Brokeoff Mountain (9,235 feet or 2,815 m), which is an erosional remnant of Mount Tehama and the second highest peak in the park. Mount Conrad, Mount Diller, and Pilot Pinnacle are also remnant peaks around the caldera.

Sulphur Works is a geothermal area in between Lassen Peak and Brokeoff Mountain that is thought to mark an area near the center of Tehama's now-gone cone. Other geothermal areas in the caldera are Little Hot Springs Valley, Diamond Point (an old lava conduit), and Bumpass Hell (see Geothermal areas in Lassen Volcanic National Park).

Broken face of Brokeoff Mountain

The magma that fuels the volcanoes in the park is derived from subduction off the coast of Northern California.

Cinder Cone and the Fantastic Lava Beds, located about 10 miles (16 km) northeast of Lassen Peak, is a cinder cone volcano and associated lava flow field that last erupted about 1650. It created a series of basaltic andesite to andesite lava flows known as the Fantastic Lava Beds.

There are four shield volcanoes in the park; Mount Harkness (southwest corner of the park), Red Mountain (at south-central boundary), Prospect Peak (in northwest corner), and Raker Peak (north of Lassen Peak). All of these volcanoes are 7,000-8,400 feet (2,133-2,560 m) above sea level and each is topped by a cinder cone volcano.

During ice ages, glaciers have modified and helped to erode the older volcanoes in the park. The center of snow accumulation and therefore ice radiation was Lassen Peak, Red Mountain, and Raker Peak. These volcanoes thus show more glacial scarring than other volcanoes in the park.

Despite not having any glaciers currently, Lassen Peak does have 14 permanent snowfields ([8]).

Since the entire park is located at medium to high elevations, the park generally has cool-cold winters and warm summers below 7,500 feet (2,300 m). Above this elevation, the climate is harsh and cold, with cool summer temperatures. Precipitation within the park is high to very high due to a lack of a rain shadow from the Coast Ranges. The park gets more precipitation than anywhere in the Cascades south of the Three Sisters. Snowfall at the Lassen Peak Chalet at 6,700 feet (2,040 m) is around 430 inches (1,100 cm) despite facing east. Up around Lake Helen, at 8,200 feet (2,500 m) the snowfall is around 600–700 inches (1,500–1,800 cm), making it probably the snowiest place in California. In addition, Lake Helen gets more average snow accumulation than any other recording station located near a volcano in the Cascade range, with a maximum of 178 inches (450 cm).[9] Snowbanks persist year-round.

Kings Creek with Lassen Peak on the horizon


Penstemons at Lassen

Lying at the northern end of the Sierra Nevada forests ecoregion, Lassen Volcanic National Park preserves a landscape nearly as it existed before Euro-American settlement: its 27,130 acres (10,980 ha) of old growth include all of its major forest types.[10][11]

At elevations below 6,500 feet the dominant vegetation community is the mixed conifer forest. Ponderosa and Jeffrey Pines, Sugar Pine, and White Fir form the forest canopy for this rich community that also includes species of manzanita, gooseberry, and ceanothus. Common wildflowers include iris, spotted coralroot, pyrola, violets, and lupin.[12]

Above the mixed-conifer forest is the major community of the Red Fir forest. Between elevations of 6,500 and 8,000 feet, Red Fir, Western White Pine, Mountain Hemlock, and Lodgepole Pine dominate a community less diverse than the mixed-conifer forest. Common plants include satin lupine, woolly mule's-ears and pinemat manzanita.[12]

Subalpine areas include the upper limit for the growth of standing trees. From 8,000 feet to treeline, plants are fewer in overall number with exposed patches of bare ground providing a harsh environment. Rock spirea, lupin, Indian paintbrush, and penstemon are a few of the rugged members of this community. Trees in this community include Whitebark Pine and Mountain Hemlock.[12]


Lassen Peak from the summit of Brokeoff Mountain. Photo shows 1915 tongue of lava and Vulcan's Eye.

Formation of basement rocks

Cinder Cone from the Fantastic Lava Beds
Thermal vents at Sulfur Works

In the Cenozoic, uplifting and westward tilting of the Sierra Nevada along with extensive volcanism generated huge lahars (volcanic-derived mud flows) in the Pliocene which became the Tuscan Formation. This formation is not exposed anywhere in the national park but it is just below the surface in many areas.

Also in the Pliocene, basaltic flows erupted from vents and fissures in the southern part of the park. These and later flows covered increasingly large areas and built a lava plateau. In the later Pliocene and into the Pleistocene, these basaltic flows were covered by successive thick and fluid flows of andesite lava, which geologists call the Juniper lavas and the Twin Lakes lavas. The Twin Lakes lava is black, porphyritic and has abundant xenocrysts of quartz (see Cinder Cone).

Another group of andesite lava flows called the Flatiron, erupted during this time and covered the southwestern part of the park's area. The park by this time was a relatively featureless and large lava plain. Subsequently, the Eastern basalt flows erupted along the eastern boundary of what is now the park, forming low hills that were later eroded into rugged terrain.

Volcanoes rise

Lassen Peak as seen from Lake Helen

Pyroclastic eruptions then started to pile tephra into cones in the northern area of the park.

Mount Tehama (also known as Brokeoff Volcano) rose as a stratovolcano in the southeastern corner of the park during the Pleistocene. It was made of roughly alternating layers of andesitic lavas and tephra (volcanic ash, breccia, and pumice) with increasing amounts of tephra with elevation. At its height, Tehama was probably about 11,000 feet (3,400 m) high.

Approximately 350,000 years ago its cone collapsed into itself and formed a two-mile (3.2 km) wide caldera after it emptied its throat and partially did the same to its magma chamber in a series of eruptions. One of these eruptions occurred where Lassen Peak now stands, and consisted of fluid, black, glassy dacite, which formed a layer 1,500 feet (460 m) thick (outcroppings of which can be seen as columnar rock at Lassen's base).

Lassen Peak from Devastated Area

During glacial periods (ice ages) of the present Wisconsinan glaciation, glaciers have modified and helped to erode the older volcanoes in the park, including the remains of Tehama. Many of these glacial features, deposits and scars, however, have been covered up by tephra and avalanches, or were destroyed by eruptions.

Roughly 27,000 years ago (older data gave an age of 18,000 years), Lassen Peak started to form as a dacite lava dome quickly pushed its way through Tehama's destroyed north-eastern flank. As the lava dome pushed its way up, it shattered overlaying rock, which formed a blanket of talus around the emerging volcano. Lassen rose and reached its present height in a relatively short time, probably in as little as a few years. Lassen Peak has also been partially eroded by Ice Age glaciers, at least one of which extended as much as 7 miles (11 km) from the volcano itself.

Since then, smaller dacite domes formed around Lassen. The largest of these, Chaos Crags, is just north of Lassen Peak. Phreatic (steam explosion) eruptions, dacite and andesite lava flows and cinder cone formation have persisted into modern times.

Bumpass Hell contains boiling springs, mudpots, and fumaroles

In Television

Lassen National Park was featured on the October 18, KIXE special Nature: Caught In The Act. The show featured two 3 minute clips, both filmed by filmmaker Brian Swierczynski. The clips featured some of the interesting locations and wildlife of Lassen including, Sulfur Works, Lake Helen, Lake Manzanita, Bampass Hell, Butte Lake, Fantastic Lava Beds, Cinder Cone, and Painted Dunes. Wildlife featured included, deer, geese, garter snakes, an Alligator Lizard, a Bald Eagle, and a weasel. The show also featured a never before filmed underwater lava field at Butte Lake.[citation needed]


Short video showing some of the attractions of Mount Lassen

See also

1938 poster for Lassen Volcanic National Park


  1. ^ a b c d e Geology of National Parks, p. 466.
  2. ^ Geology of U.S. Parklands, p. 154.
  3. ^ NPS 2003 General Management Plan, Wilderness Zone accessed 4 Sept., 2009
  4. ^ USGS: Volcano Hazards of the Lassen Volcanic National Park Area, California
  5. ^ National Park Service Public Use Statistics Office accessed 3 October 2009
  6. ^ Public Use Reporting and Counting Instructions accessed 3 October 2009
  7. ^ a b "Geology Fieldnotes for Lassen Volcanic National Park California" (accessed 7 October 2006)
  8. ^
  9. ^ Cascade Snow
  10. ^ Franklin, Jerry, F; Fites-Kaufmann, Jo Ann (1996), "Assessment of Late-Successional Forests of the Sierra Nevada", Status of the Sierra Nevada, Sierra Nevada Ecosystem Project. Final Report to Congress, pp. 627–671, 
  11. ^ Bolsinger, Charles L.; Waddell, Karen L. (1993), Area of old-growth forests in California, Oregon, and Washington, United States Forest Service, Pacific Northwest Research Station, Resource Bulletin PNW-RB-197, 
  12. ^ a b c "Plants". United States National Park Service: Lassen Volcanic National Park. Retrieved January 13, 2009. 


 This article incorporates public domain material from websites or documents of the National Park Service.

External links

Travel guide

Up to date as of January 14, 2010

From Wikitravel

Lassen Volcanic National Park [1] is a United States national park that is located at the southern terminus of the Cascade Mountains in the Shasta Cascades region of California, approximately 50 miles east of Redding. Within the park's 165 square miles / 106,000 acres are numerous volcanic features including four types of volcanoes, steam vents, mud pots, and painted dunes. In addition, with nearly 79,000 acres designated as wilderness area and fewer than 400,000 visitors per year, the park is an ideal place for a nature getaway.



Cinder Cone National Monument and Lassen Peak National Monument were established by proclamation of Theodore Roosevelt on May 6, 1907 to be administered by the U.S. Forest Service. Volcanic eruptions from Lassen Peak in 1914 and 1915 resulted in national publicity. The two monuments and surrounding areas were included in Lassen Volcanic National Park, established in 1916, administered by the National Park Service of the Department of the Interior.And is also a very exciting place to be.


Beneath Lassen Volcanic's peaceful forests and gem-like lakes lies evidence of a turbulent and fiery past. 600,000 years ago, the collision and warping of continental plates led to violent eruptions and the formation of lofty Mt. Tehama (also called Brokeoff Volcano.) After 200,000 years of volcanic activity, vents and smaller volcanoes on Tehama's flanks-including Lassen Peak-drew magma away from the main cone. Hydrothermal areas ate away at the great mountain's bulk. Beneath the onslaught of Ice Age glaciers, Mt. Tehama crumbled and finally ceased to exist. But the volcanic landscape lived on: in 1914, Lassen Peak awoke. The Peak had its most significant activity in 1915 and minor activity through 1921.

All four types of volcanoes in the world are found in the park. Over 150 miles of trails and a culturally significant scenic highway provide access to volcanic wonders including steam vents, mudpots, boiling pools, volcanic peaks, and painted dunes.

Flora and fauna

Although Lassen is primarily known for its volcanic geology, the park boasts a rich diversity of plant and animal life. Over 700 flowering plant species grace the park, providing shelter and food for 250 vertebrates as well as a host of invertebrates including insects.

This great diversity of life forms is due to two factors: the geographic location of the park and the abundance of habitats that occur there.

Situated at the southern end of the Cascade Range geologic province, Lassen Volcanic National Park lies at the crossroads of three great biological provinces: the Cascades range to the north, the Sierra Nevada mountains to the south and the Great Basin desert to the east.

The myriad habitats of Lassen Volcanic National Park are produced by variations in environmental conditions such as elevation (5,000 to 10,457 feet), moisture (precipitation is greater on the western than the eastern side of the park), substrate (rock type and soil depth), temperature, insolation (amount of sun) and prior disturbance (both natural and human-caused).


Snow covers much of the park mid-October through mid-June. The Park Road (the main road that connects Hwy. 89 through the Park) is usually closed late October through mid-June. During years of heavy snowfall, the road may open significantly later. Please call the Park for road and trail condition updates. Many of the main park attractions are snow covered and inaccessible by car and foot during the winter. The months of July, August, and September may bring mostly sunny skies with warm daytime temperatures and cool nighttime temperatures.

Get in

By plane

The nearest major airports are in Redding and Chico, with additional options in Reno.

By car

The best access to the park is by private automobile. Auto rental services are available in Redding, Red Bluff, Chico, Susanville or Reno. The park is located fifty miles east of Red Bluff on highway 36, and 50 miles east of Redding on highway 44.

By bus

Greyhound and Trailways bus lines serve cities within 60 miles of the park, although neither visits the park.


Park entrance fees are $10 for private vehicles and $5 for individuals on foot, bike and motorcycle. All entrance fees are valid for seven days. The Annual Pass is available for $25, allowing park entry for one year. Alternatively, the National Parks and Federal Recreational Lands Pass can be purchased for $80, allowing free entry to all national park areas for one year.

Get around

The main roads in the park are paved, although many are closed by snow except from June until September. Allow at least three hours to drive across the park and to make stops. Current road conditions are available online.

  • Sulphur Works. On Highway 89, about one mile +(1.6 km) north of the Southwest Entrance. A small geothermal area with mudpots, fumaroles and hot water flow. Its small parking lot is located right on the highway. A boardwalk allows for closer viewing of the features.  edit
  • Devastated Area. Located in the north section of the park on Highway 89. This area was located in the path of the pyroclastic flow from Lassen's eruption. All of the vegetation in the area was destroyed by hurricane force winds and burning hot gasses and mud. Since the eruption, the area is regrowing but there is still ample evidence of the destruction. A short, fairly level interpretive trail points out the results of the devastation and the subsequent natural recovery process.  edit
  • Hike to Bumpass Hell, [2]. On Highway 89, near Lassen Peak. This is the largest geothermal area in the park and features boiling pools, mudpots and roaring fumaroles seen from a wooden boardwalk. A large parking lot is found at the trailhead to Bumpass Hell. The geothermal area can be reached via a 3-mile (4.8 km) hiking trail. The trail has a 300 foot (91 m) elevation gain/loss. The elevation of the trail is around 8,000 feet (2,430 m) so care should be taken if you are not used to high altitudes. The trail is buried under snow until late spring, sometimes till mid-summer, depending on the previous winter's snowfall.  edit
  • Climb Lassen Peak, [3]. The high mountain pass of Highway 89 allows easy access to the summit of Lassen Peak. The 2.5 mile (4 km) trail to the summit begins from a parking lot on the highway. The trip to the peak and back is a total of five miles (8 km) with a climb of about 2,000 feet (610 m). The average time for the round trip is 3-5 hours. The elevation of the trail is from 8,000 feet (2,430 m) to 10,457 feet (3,187 m) so care should be taken if you are not used to high altitudes.  edit
  • Fishing, [4]. Fishing is allowed in Manzanita Lake, located just inside the West Entrance, Juniper Lake in the southeast corner of the Park (reached via unpaved road from the town Chester) and Butte Lake in the northeast corner of the Park (reached unpaved road from Highway 44). All three lakes allow fishing from the shore or from a boat. All three have a boat launch ramp. A California fishing license is required. The lakes have natural trout populations. Only single-hook, barbless, artificial lures are allowed in Manzanita Lake.  edit
  • Climb Cinder Cone. Located in the Butte Lake area in the northern part of the park, this extinct volcano is a perfect cone that looks like what you think a volcano should look like, complete with a hole in the middle you can walk down into. The trip to the top and back is about four miles (6.5 km) with a short but really steep climb at the end of about 500(?) feet (310 m) up the side of the cone itself on really loose sand-like material (coming down is easy - and fun, like skating on sand). From the top you can see the old lava flows of the "Devastated Area" of the park. The average time for the round trip is 4 hours. Very sunny, so bring lots of water.  edit
  • Manzanita Lake Camper Store, Ph: (530) 335-7557. Located at Manzanita Lake and open daily from late May through early September, this store offers food, restrooms, pay phone, showers, laundromat, and a gas station.
  • Peak Necessities. Located in the Lassen Peak parking area and open daily from mid-June through early September, this store offers food and gift sales.
  • Lassen Chalet Gift Shop & Snack Bar. Located in the Southwest area, this store offers snacks and gifts.
  • Drakesbad Guest Ranch (Open early June through early October, weather permitting), Ph: (530) 529-1512, [5]. Drakesbad Guest Ranch is a ranch that is over 100 years old, with baths and pool fed by local hot springs. Accommodations are rustic (most without electricity) and include a bathroom, beds, use of pool, three meals and housekeeping. Rates (per person) start around $110 per night.
  • Butte Lake (Open June through September, weather permitting), Ph: (877) 444-6777. Located six miles south on dirt road via Highway 44 East, seventeen miles from Old Station, this campground offers 101 sites for $14 per night. Amenities include a picnic table, campfire ring, bearproof box, drinking water, flush and vault toilets, boat launch, fishing, and swimming (no hookups or dump station). Each site accommodates up to three tents or one RV to 35' with a limit of 6 people at each site. Reservations are available for loop B sites, all others are first-come, first-served.
  • Crags (Open late May through September, weather permitting). Located five miles south of Manzanita Lake, this campground offers 45 sites for $12 per night. Amenities include a picnic table, campfire ring, bearproof box, vault toilets, and drinking water (no hookups or dump station). Each site accommodates up to three tents or one RV to 35’ with a limit of 6 people at each site. All sites are first-come, first-served.
  • Juniper Lake (Open July through September, weather permitting). Located on the east shore of Juniper Lake via 13-mile road the campground is accessible from the town of Chester on Highway 36 East (look for signs to Drakesbad and Juniper Lake, at the Chester Fire Station, turn onto Feather River Drive, then after about a half mile, bear right and follow signs to Juniper Lake). There are 18 sites for $10 per night, with amenities including a picnic table, campfire ring, bearproof box, vault toilets, swimming, and fishing (no water, hookups or dump station). Each site accommodates up to three tents (no RVs) with a limit 6 people at each site. All sites are first-come, first-served. Note that the last six miles into Juniper Lake is rough dirt road and not recommended for buses, motor homes or trailers.
  • Manzanita Lake (Open late May through September, weather permitting), Ph: (877) 444-6777. Located adjacent to and south of Manzanita Lake, this campground has 179 sites for $16 per night during summer, and $10 per night in late September. Amenities include a picnic table, campfire ring, bearproof box, drinking water, flush toilets, drinking water, boat launch, fishing, and swimming (no hookups, dump station available for an extra fee). There is a pay phone, food, showers, laundromat, and gift shop in the nearby at the Camper Store. Each site accommodates up to three tents or one RV to 35' with a limit of 6 people at each site. Reservations are available for loop A & C, with all other sites first-come, first-served.
  • Southwest Walk-In (Open year-round). Located on the east side of Visitor Center parking area (near Southwest Entrance Station). This campground has 21 walk-in sites for $10 per night. Amenities include a picnic table, campfire ring, bearproof box, flush toilets, and drinking water (not available April through June). Each site accommodates up to three tents with a limit of 6 people at each site. All sites are first-come, first-served.
  • Summit Lake North (Open July through early September, weather permitting), Ph: (877) 444-6777. Located twelve miles south of Manzanita Lake and 17.5 miles north of Southwest Entrance, this campground offers 46 sites for $16 per night. Amenities include a picnic table, campfire ring, bearproof box, drinking water, flush toilets, drinking water, and swimming (no hookups or dump station). Each site accommodates up to three tents or one RV to 35' with a limit of 6 people at each site. Reservations are available for loop B, with all other sites first-come, first-served.
  • Summit Lake South (Open July through September, weather permitting), Ph: (877) 444-6777. Located twelve miles south of Manzanita Lake and 17.5 miles north of Southwest Entrance, this campground offers 48 sites for $14 per night. Amenities include a picnic table, campfire ring, bearproof box, drinking water, pit toilets, drinking water, and swimming (no hookups or dump station). Each site accommodates up to three tents with a limit of 6 people at each site. Reservations are available in loops C & D, with all other sites first-come, first-served.
  • Warner Valley (Open June through September, weather permitting). Located one mile west of Warner Valley Ranger Station via dirt road, and 17 miles north of Chester, this campground is not recommended for trailers. The eighteen sites are $14 per night in the summer, and $10 at other times. Amenities include a picnic table, campfire ring, bearproof box, drinking water (mid-June through September only), pit toilets, and fishing in the stream. Each site accommodates up to three tents with a limit of 6 people at each site. No reservations are available.

Stay safe

Be aware that the majority of the Park is at high elevations so care should be taken to avoid altitude sickness.

Always stay on the paths and trails around geothermal areas. This mineral crusts can form over mudpots and hot springs that appear to be solid ground. These crusts can collapse leading to immersion in boiling water. The Bumpass Hell geothermal area is named for a man who broke through a crust and ended up having his leg amputated due to the burns he sustained.

  • Subway Cave, [6]. Near the town of Old Station, 1/4 mile (0.4 km) north of the junction of Highways 44 and 89. Subway Cave is a lava tube formed 20,000 years ago. A 1/3 mile (0.5 km), self-guided trail leads through 1,300 feet (396 m) of the lava tube. The lava tube has interpretive signs but is not lit so flashlights are required. The floor is rough and uneven and the temperature is 46°F (7.8°C) year round. Sturdy shoes and warm clothing are recommended. Free.  edit
This is a usable article. It has information for getting in as well as some complete entries for restaurants and hotels. An adventurous person could use this article, but please plunge forward and help it grow!


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