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Home > Art, Film & Photography > Argyre Quadrangle: Hale, Charitum Montes, Argyre Planitia, Galle, Nereidum Montes, Hartwig, Lohse, Bond, Green, Arkhangelsky, Baltisk, Jezza
Argyre Quadrangle: Hale, Charitum Montes, Argyre Planitia, Galle, Nereidum Montes, Hartwig, Lohse, Bond, Green, Arkhangelsky, Baltisk, Jezza

Argyre Quadrangle: Hale, Charitum Montes, Argyre Planitia, Galle, Nereidum Montes, Hartwig, Lohse, Bond, Green, Arkhangelsky, Baltisk, Jezza


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About the Book

Chapters: Hale, Charitum Montes, Argyre Planitia, Galle, Nereidum Montes, Hartwig, Lohse, Bond, Green, Arkhangelsky, Baltisk, Jezza, Wirtz. Source: Wikipedia. Pages: 42. Not illustrated. Free updates online. Purchase includes a free trial membership in the publisher's book club where you can select from more than a million books without charge. Excerpt: The Argyre quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program. The Argyre quadrangle is also referred to as MC-26 (Mars Chart-26). The Argyre quadrangle covers the area from 0 to 60 west longitude and from 30 to 65 south latitude on Mars. It contains Galle crater, which resembles a smiley face. Gullies are common in some latitude bands on Mars. Usually, gullies are found on the walls of craters or troughs, but Nereidum Montes, a set of mountains, has gullies in some areas (See the image below). Gullies occur on steep slopes, especially craters. Gullies are believed to be relatively young because they have few, if any craters, and they lie on top of sand dunes which are themselves young. Usually, each gully has an alcove, channel, and apron. Although many ideas have been put forward to explain them, the most popular involve liquid water either coming from an aquifer or left over from old glaciers. There is evidence for both theories. Most of the gully alcove heads occur at the same level, just as one would expect of an aquifer. Various measurements and calculations show that liquid water could exist in an aquifer at the usual depths where the gullies begin. One variation of this model is that rising hot magma could have melted ice in the ground and caused water to flow in aquifers. Aquifers are layers that allow water to flow. They may consist of porous sandstone. This layer would be perched on top of another layer that prevents water from going down (in geological terms it would be...More: http: //booksllc.net/?id=21559519


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Product Details
  • ISBN-13: 9781157398288
  • Publisher: Books LLC
  • Publisher Imprint: Books LLC
  • Height: 152 mm
  • No of Pages: 44
  • Spine Width: 3 mm
  • Weight: 77 gr
  • ISBN-10: 1157398286
  • Publisher Date: 15 Sep 2010
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Hale, Charitum Montes, Argyre Planitia, Galle, Nereidum Montes, Hartwig, Lohse, Bond, Green, Arkhangelsky, Baltisk, Jezza
  • Width: 229 mm


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