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  2. Areography - Wikipedia

    en.wikipedia.org/wiki/Areography

    Areography, also known as the geography of Mars, is a subfield of planetary science that entails the delineation and characterization of regions on Mars. [ 1 ] [ 2 ] [ 3 ] Areography is mainly focused on what is called physical geography on Earth; that is the distribution of physical features across Mars and their cartographic representations.

  3. File:CK12 Earth Science.pdf - Wikipedia

    en.wikipedia.org/wiki/File:CK12_Earth_Science.pdf

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  4. File:THE NATURE OF THE EARTH.pdf - Wikipedia

    en.wikipedia.org/wiki/File:THE_NATURE_OF_THE...

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  5. File:High School Earth Science 1-13.pdf - Wikipedia

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    Original file (1,275 × 1,650 pixels, file size: 95.26 MB, MIME type: application/pdf, 510 pages) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  6. Aerography - Wikipedia

    en.wikipedia.org/wiki/Aerography

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  7. Geology of Mars - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Mars

    The northern part is an enormous topographic depression. About one-third of the surface (mostly in the northern hemisphere) lies 3–6 km lower in elevation than the southern two-thirds. This is a first-order relief feature on par with the elevation difference between Earth's continents and ocean basins. [12]

  8. Planetary cartography - Wikipedia

    en.wikipedia.org/wiki/Planetary_cartography

    Planetary cartography, or cartography of extraterrestrial objects (CEO), is the cartography of solid objects outside of the Earth. Planetary maps can show any spatially mapped characteristic (such as topography, geology, and geophysical properties) for extraterrestrial surfaces. [1]

  9. Mars habitability analogue environments on Earth - Wikipedia

    en.wikipedia.org/wiki/Mars_habitability_analogue...

    On Earth, although temperatures on Earth briefly get cold enough for dry ice to form in the Antarctic interior at high altitudes, the partial pressure of carbon dioxide in Earth's atmosphere is too low for dry ice to form because the depositional temperature for dry ice on Earth under 1 bar of pressure is −140 °C (−220 °F) [13] and the ...