|
Jake Matijevic (or Jake M) is a pyramidal rock on the surface of Aeolis Palus, between Peace Vallis and Aeolis Mons ("Mount Sharp"), in Gale crater on the planet Mars. The "approximate" site coordinates are: . The rock was encountered by the ''Curiosity rover'' on the way from Bradbury Landing to Glenelg Intrique in September 2012 and measures about height and width. The rock was named by NASA after (1947–2012), a mathematician-turned-rover-engineer, who played a critical role in the design of the six-wheeled rover, but died just days after the ''Curiosity rover'' landed in August 2012. Matijevic was the surface operations systems chief engineer for the Mars Science Laboratory Project and the project's ''Curiosity rover''. He was also a leading engineer for all of the previous NASA Mars rovers including ''Sojourner'', ''Spirit'' and ''Opportunity''. The rover team determined the rock to be a suitable target for the first use of Curiosity's contact instruments, the Mars Hand Lens Imager (MAHLI) and the Alpha particle X-ray spectrometer (APXS). Analytical studies, performed on the rock by the Curiosity rover in October 2012, suggest the ''Jake M'' rock is an igneous rock but found to be high in elements consistent with feldspar, such as sodium, aluminum and potassium, and lower concentrations of magnesium, iron and nickel than other such rocks previously found on Mars. The mineral content and elemental abundance indicates ''Jake M'' rock may be a mugearite, a sodium rich oligoclase-bearing basaltic trachyandesite. Igneous rocks similar to the ''Jake M'' rock are well known but occur rarely on Earth. On Earth, such rocks form when magma, usually found in volcanoes, rises to the surface, cools and partially solidifies with certain chemical elements, while the warmer liquid magma portion becomes enriched with the left-behind elements.〔 By remarkable coincidence, the Martian locality Glenelg is also the name of a small settlement in north-west Scotland that is east of type locality for mugearite at Mugeary on the island of Skye.〔 The ''Jake M'' rock is a ventifact with a volcanic fabric.〔Zasada, Patrick (2013): Entstehung des Mars-Gesteins „Jake Matijevic“. – (Sternzeit – Z. astron. Vereinig. ), (issue 2/2013 ): 98-101. ''ISSN 0721-8168'', (in German).〕 Its pyramidal shape was formed by eolian drifted grains of sand. The little cavities on its surface were formed by the blast-effect, which is caused by different flow dynamics at the micro-relief.〔 On the surface one could see the marks of the main wind direction, by which ''Jake M'' was formed.〔 On September 27, 2013, NASA scientists reported that ''Jake M'' rock was a mugearite and very similar to terrestrial mugearite rocks. ==See also== * Aeolis quadrangle * Composition of Mars * Geology of Mars * List of rocks on Mars * Matijevic Hill * Mugearite * Timeline of Mars Science Laboratory 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Jake Matijevic (rock)」の詳細全文を読む スポンサード リンク
|