The Full Wiki

More info on Argyre Planitia

Argyre Planitia: Wikis


Note: Many of our articles have direct quotes from sources you can cite, within the Wikipedia article! This article doesn't yet, but we're working on it! See more info or our list of citable articles.


From Wikipedia, the free encyclopedia

Argyre basin topo.jpg
Topography of Argyre basin and its surroundings
Coordinates 49°42′S 316°00′E / 49.7°S 316.0°E / -49.7; 316.0Coordinates: 49°42′S 316°00′E / 49.7°S 316.0°E / -49.7; 316.0
Diameter 1800 km
Depth 5.2 km
Eponym Argyre

Argyre Planitia is a plain located in the Argyre impact basin in the southern highlands of Mars. Its name comes from a map produced by Giovanni Schiaparelli in 1877; it refers to Argyre, a mythical island of silver in Greek mythology.

Argyre lies between -35 and -61 deg S and 27 and 62 deg W, centered at 49°42′S 316°00′E / 49.7°S 316.0°E / -49.7; 316.0. The basin is approximately 1120 miles (1800 kilometers) wide, believed to be the second-largest impact basin on Mars after Hellas Planitia, and drops 3.2 miles (5.2 kilometers) below the surrounding plains.

The basin was possibly formed by a giant impact during a Heavy Bombardment Period of the early Solar System, approximately 3.9 billion years ago, and may be one of the best preserved ancient impact basins from that hypothetical event. Argyre is surrounded by rugged massifs which form concentric and radial patterns around the basin. Several mountain ranges are present, including Charitum and Nereidum Montes.

Four large Noachian epoch channels lie radial to the basin. Three of these channels (Surius Valles, Dzígai Valles, and Palacopas Valles) flowed into Argyre from the south and east through the rim mountains. The fourth, Uzboi Vallis, appears to have flowed out from the basin's north rim to the Chryse region and may have drained a lake of melting ice within the basin. A smaller outflow channel named Nia Valles is relatively fresh-looking, and probably formed during the early Amazonian after the major fluvial and lacustrine episodes had finished.

The original basin floor is buried with friable, partially deflated layered material that may be lake sediment. No inner rings are visible, however isolated massifs within the basin may be remnants of an inner ring.

The crater Galle, located on the east rim of Argyre at 51°S, 31°W, strongly resembles a smiley face.

See also

External links

Coordinates: 49°42′S 316°00′E / 49.7°S 316°E / -49.7; 316



Got something to say? Make a comment.
Your name
Your email address