Gatos

Mons is a large volcano located in the Atla Regio region of Venus.

Sapas Mons measures about 400 kilometers (250 mi) across and 1.5 kilometers(0.93 mi) high. Its flanks show numerous overlapping lava flows. The dark flows on the lower right of the radar image are thought to be smootherthan the brighter ones near the central part of the volcano. Many of the flows appear to have been erupted along the flanks of the volcano rather thanfrom the double summit. This type of flank eruption is common on large volcanoes on Earth, such as the Hawaiian volcanoes. The summit area has twoflat-topped mesas, whose smooth tops give a relatively dark appearance in the radar image. Also seen near the summit are groups of pits, some aslarge as one kilometer (0.6 mile) across. These are thought to have formed when underground chambers of magma were drained through other subsurfacetubes and lead to a collapse at the surface. A 20-kilometer-diameter (12 mi) impact crater northeast of the volcano is partially buried by the lavaflows. Little was known about Atla Regio prior to the Magellan probe. The new data, acquired in February 1991, show the region to be composed of atleast five large volcanoes such as Sapas Mons, which are commonly linked by complex systems of fractures or rift zones. If comparable to similarfeatures on Earth, Atla Regio probably formed when large volumes of molten rock upwelled from areas within the interior of Venus known as 'hot spots.'