McLaughlin Crater viewed from orbit - small 0.550 km (0.342 mi) portion of 90.92 km (56.50 mi) diameter crater floor is shown - (MRO, HiRISE) (January, 2013). | |
Planet | Mars |
---|---|
Region | Oxia Palus quadrangle |
Coordinates | [ ⚑ ] : 21°54′N 337°38′E / 21.9°N 337.63°E[1] |
Diameter | 90.92 km (56.50 mi)[1] |
Depth | 2.2 km (1.4 mi)[2] |
McLaughlin Crater is an old crater in the Oxia Palus quadrangle of Mars, located at [ ⚑ ] 21°54′N 337°38′E / 21.9°N 337.63°E. It is 90.92 km (56.50 mi)[1] in diameter and 2.2 km (1.4 mi)[2] deep. The crater was named after Dean B. McLaughlin, an American astronomer (1901-1965).[1][3] The Mars Reconnaissance Orbiter has found evidence that the water came from beneath the surface between 3.7 billion and 4 billion years ago and remained long enough to make carbonate-related clay minerals found in layers.[2][4] McLaughlin Crater, one of the deepest craters on Mars, contains Mg-Fe clays and carbonates that probably formed in a groundwater-fed alkaline lake. This type of lake could have had a massive biosphere of microscopic organisms.[5]
![]() | Original source: https://en.wikipedia.org/wiki/McLaughlin (Martian crater).
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