Tempe Terra
Tempe Terra is a heavily cratered highland region in the northern hemisphere of the planet Mars. Located at the northeastern edge of the Tharsis volcanic province, Tempe Terra is notable for its high degree of crustal fracturing and deformation. The region also contains a large number of small shield volcanoes, lava flows, and other volcanic structures.
The region is named after the albedo feature Tempe, first used by astronomer E.M. Antoniadi in 1930 to describe a bright patch of terrain centered near 40°N, 70°W. The name comes from the Vale of Tempe, a valley located south of Mount Olympus and celebrated by the ancient Greeks for its beauty. The International Astronomical Union (IAU) formally designated the region Tempe Terra in 1979. Terra (pl. terrae) is a Latin descriptor term used in planetary geology for continent-like highland regions (i.e., extensive land masses) on other planets.[1]
Location and description
Tempe Terra is located in the eastern half of the Arcadia quadrangle (MC-03) and the western edge of the Mare Acidalium quadrangle (MC-04) in Mars' western hemisphere. It is centered at 39°42′N 289°00′E / 39.7°N 289°ECoordinates: 39°42′N 289°00′E / 39.7°N 289°E and spans about 2,700 km at its broadest extent.[1] The region extends from about 30° to 54°N and from 265° to 310°E, covering approximately 2.1 million km2,[2] or an area roughly equivalent to that of Saudi Arabia. It is bordered to the east by Chryse and Acidalia Planitiae, to the north by the low-lying plains of Arcadia and Vastitas Borealis, and to the south by the huge outflow channel system of Kasei Valles.
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MOLA map showing boundaries for Tempe Terra and other regions. Colors indicate elevations.
Geology
Tempe Terra occupies a transition zone between the old, heavily cratered highlands of the Martian south and the geologically younger, lowland terrain of the north. Tempe Terra contains the northernmost exposures of ancient highland crust on the planet.[3] The region is transected by large numbers of linear to curvilinear normal faults and grabens with ages that span much of Mars' geologic history. Research on extension, or rifts in the crust, has suggested Tempa Terra may be the most highly strained geologic region on Mars[4] with a lot of low shield volcanoes.
There is evidence of valleys in Tempe Terra, including stream meanders, as in the image below.
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Channels, as seen by HiRISE under HiWish program. Stream appears to have eroded through a hill.
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Stream meander and cutoff, as seen by HiRISE under HiWish program.
Gullies
Martian gullies are small, incised networks of narrow channels and their associated downslope sediment deposits, found on the planet of Mars. They are named for their resemblance to terrestrial gullies. First discovered on images from Mars Global Surveyor, they occur on steep slopes, especially on the walls of craters. Usually, each gully has a dendritic alcove at its head, a fan-shaped apron at its base, and a single thread of incised channel linking the two, giving the whole gully an hourglass shape.[5] They are believed to be relatively young because they have few, if any craters. A subclass of gullies is also found cut into the faces of sand dunes which themselves considered to be quite young. On the basis of their form, aspects, positions, and location amongst and apparent interaction with features thought to be rich in water ice, many researchers believed that the processes carving the gullies involve liquid water. However, this remains a topic of active research. The pictures below show a variety of gullies and gully features.
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A variety of gullies originating at different levels are visible in this HiRISE image that was taken under the HiWish program.
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This enlargement of a small part of the previous image shows terraces along a gully channel. The terraces were created when a new channel cut through the old surface. This means that the gully was not in a single event. Water must have flowed more than once in this location.
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Gullies in a crater. Some seem to be young, others are well developed. Picture was taken by HiRISE under the HiWish program.
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Gullies along mesa wall in North Tempe Terra, as seen by HiRISE under HiWish program
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Close view of gully apron, as seen by HiRISE under HiWish program Note this is an enlargement of the previous image.
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Close view of gully alcove, as seen by HiRISE under HiWish program Note this is an enlargement of a previous image.
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Gullies on wall of mesa, as seen by HiRISE under HiWish program
Other images from Tempe Terra
The pictures below are probably formed from ice. The Martian surface displays many differed types of holes, pits, depressions, and hollows that are believed to have been caused by large amounts of ice disappearing from the ground. When the ice leaves, the ground collapses. Because of the thin atmosphere on the planet, the ice sublimates—goes directly from a solid phase to a gas phase. Dry ice does that on the Earth. Eskers form when a stream runs under a glacier and deposits material that is left behind when the glacier disappears.
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Hollows formed by erosion on floor of crater, as seen by HiRISE under HiWish program
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Esker, as seen by HiRISE under the HiWish program.
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Layers, as seen by HiRISE under HiWish program Location is Tempe Terra in Arcadia quadrangle.
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Layers, as seen by HiRISE under HiWish program Location is Tempe Terra Note: this is an enlargement of the previous image.
See also
References
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Wikimedia Commons has media related to Tempe Terra. |
- 1 2 Gazetteer of Planetary Nomenclature. http://planetarynames.wr.usgs.gov.
- ↑ Neesemann, A.; van Gasselt, S; Hauber, E; Neukum, G. (2010) Insights to the Evolution of the Tempe Terra Region, Mars: Refinements of Geologic and Tectonic Units. 41st Lunar and Planetary Science Conference; LPI:Houston, TX, Abstract #2685. http://www.lpi.usra.edu/meetings/lpsc2010/pdf/2685.pdf.
- ↑ Frey, H.V.; Grant, T.D. 1990. Resurfacing History of Tempe Terra and Surroundings. J. Geophys. Res., 95(B9), 14,249–14,263.
- ↑ Golombek, M.P.; Tanaka, K.L.; Franklin, B.J. (1996). "Extension across Tempe Terra, Mars, from measurements of fault-scarp widths and deformed craters". JGR-Planets 101 (E11).
- ↑ Malin, M., Edgett, K. 2000. Evidence for recent groundwater seepage and surface runoff on Mars. Science 288, 2330–2335.
