Arabia quadrangle

Image of the Arabia Quadrangle (MC-12). The region is dominated with heavily cratered highlands; the northeast part contains Cassini Crater.

The Arabia quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program. The Arabia quadrangle is also referred to as MC-12 (Mars Chart-12).^[1]

The quadrangle contains part of the classic area of Mars known as Arabia. It also contains a part of Terra Sabaea and a small part of Meridiani Planum.It lies on the boundary between the young northern plains and the old southern highlands. The quadrangle covers the area from 315° to 360° west longitude and 0° to 30° north latitude.

Description

The surface of the Arabia quadrangle appears to be very old because it has a high density of craters, but it is not near as high in elevation as typical old surfaces. On Mars the oldest areas contain the most craters; the oldest period is called Noachian after the quadrangle Noachis.^[2] The Arabia area contains many buttes and ridges. Some believe that during certain climate changes an ice-dust layer was deposited; later, parts were eroded to form buttes.^[3] Some outflow channels are found in Arabia, namely Naktong Vallis, Locras Valles, Indus Vallis, Scamander Vallis, and Cusus Valles.^[4]

Layers

Many places in Arabia are shaped into layers.^[5] The layers can be a few meters thick or tens of meters thick. Recent research on these layers by scientists at California Institute of Technology (Caltech) suggest that ancient climate change on Mars caused by regular variation in the planet's tilt, or obliquity may have caused the patterns in the layers. On Earth, similar changes (astronomical forcing) of climate results in ice-age cycles.

A recent study of layers in craters in western Arabia revealed much about the history of the layers. Although the craters in this study are just outside the boundary for the Arabia quadrangle the findings would probably apply to the Arabia quadrangle as well. The thickness of each layer may average less than 4 meters in one crater, but 20 meters in another. The pattern of layers measured in Becquerel crater, suggests that each layer was formed over a period of about 100,000 years. Moreover, every 10 layers were bundled together into larger units. The 10-layer pattern is repeated at least 10 times. So every 10-layer pattern took one-million years to form.

The tilt of the Earth's axis changes by only a little more than 2 degrees; it is stabilized by the relatively large mass of our moon. In contrast Mars's tilt varies by tens of degrees. When the tilt (or obliquity) is low, the poles are the coldest places on the planet, while the equator is the warmest—as on Earth. This causes gases in the atmosphere, like water and carbon dioxide, to migrate pole ward, where they freeze. When the obliquity is higher, the poles receive more sunlight, causing those materials to migrate away. When carbon dioxide moves from the poles, the atmospheric pressure increases, maybe causing a difference in the ability of winds to transport and deposit sand. Also, with more water in the atmosphere sand grains may stick and cement together to form layers. This study of the thickness of layers was done using stereo topographic maps obtained by processing data from the high-resolution camera onboard NASA's Mars Reconnaissance Orbiter.^[6]

Recent research leads scientists to believe that some of the craters in Arabia may have held huge lakes. Cassini Crater and Tikonravov Crater probably once were full of water since their rims seem to have been breached by water. Both inflow and outflow channels have been observed on their rims. Each of these lakes would have contained more water than Earth's Lake Baikal, our largest freshwater lake by volume. The watersheds for lakes in Arabia seem to be too small to gather enough water by precipitation alone; therefore it is thought that much of their water came from groundwater.^[7]

Another group of researchers proposed groundwater with dissolved minerals came to the surface, in and later around craters, and helped to form layers by adding minerals (especially sulfate) and cementing sediments. Upon close examination, Arabia layers appear to have a slight tilt. This tilt supports formation with the action of a rising water table. A water table generally follows the topography. Since the layers slope slightly down toward the northwest, the layers may have been created by groundwater, rather than a single large sea that has been suggested.

This hypothesis is supported by a groundwater model and by sulfates discovered in a wide area.^[8][9] At first, by examining surface materials with Opportunity Rover, scientists discovered that groundwater had repeatedly risen and deposited sulfates.^{[10][11][12][13][14]} Later studies with instruments on board the Mars Reconnaissance Orbiter showed that the same kinds of materials exist in a large area that included Arabia.^[15]

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  Layers in Monument Valley. These are accepted as being formed, at least in part, by water deposition. Since Mars contains similar layers, water remains as a major cause of layering on Mars.

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  Layers in Gill crater (Martian crater), as seen by HiRISE under HiWish program.

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  Close-up of layers in Gill crater, as seen by HiRISE under HiWish program.

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  Close-up of layers on edge of a mesa in Gill crater, as seen by HiRISE under HiWish program.

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  Layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program. Pedestal crater is within the much larger Tikhonravov Crater.

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  Layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program. Pedestal crater is within the much larger Tikhonravov Crater.

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  Close-up of some layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program.

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  Close-up of some layers under cap rock of a pedestal crater and a dark slope streak, as seen by HiRISE under HiWish program.

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  Layers in a butte in Arabia, as seen by HiRISE under HiWish program.

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  Layers in Arabia, as seen by HiRISE under HiWish program.

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  Wide view of layers, as seen by HiRISE under HiWish program

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  Close view of layers, as seen by HiRISE under HiWish program

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  Close view of layers, as seen by HiRISE under HiWish program At least one layer is light-toned which may indicated hydrated minerals.

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  Close view of layers, as seen by HiRISE under HiWish program

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  Wide view of layers, as seen by HiRISE under HiWish program

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  Close view of layers from previous image, as seen by HiRISE under HiWish program

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  Close view of layers from previous image, as seen by HiRISE under HiWish program

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  Close view of layers from a previous image, as seen by HiRISE under HiWish program

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  Wide view of layered mesas and buttes, as seen by HiRISE under HiWish program

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  Close view of layered butte, as seen by HiRISE under HiWish program

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  Layered butte, as seen by HiRISE under HiWish program

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  Layered butte, as seen by HiRISE under HiWish program

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  Close view of layers and dunes, as seen by HiRISE under HiWish program Light-toned material may contain hydrated minerals.

Craters

Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak.^[16] The peak is caused by a rebound of the crater floor following the impact.^[17] Sometimes craters display layers. Since the collision that produces a crater is like a powerful explosion, rocks from deep underground are tossed unto the surface. Hence, craters can show us what lies deep under the surface.

Some craters in Arabia are classified as pedestal craters. A pedestal crater is a crater with its ejecta sitting above the surrounding terrain and thereby forming a raised platform. They form when an impact crater ejects material which forms an erosion resistant layer, thus protecting the immediate area from erosion. As a result of this hard covering, the crater and its ejecta become elevated, as erosion removes the softer material beyond the ejecta.^[18] Some pedestals have been accurately measured to be hundreds of meters above the surrounding area. This means that hundreds of meters of material were eroded away. Pedestal craters were first observed during the Mariner missions.^[18][19][20]

Researchers believe over 200 new craters are formed each year on Mars, based on study of years of HiRISE images.^[21][22]

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  Pedestal craters and layers in Tikonravev Crater in Arabia, as seen by Mars Global Surveyor (MGS) with the Mars Orbiter Camera, under the MOC Public Targeting Program. Layers may form from volcanoes, the wind, or by deposition under water. Some researchers believe this crater once held a massive lake.

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  Pedestal craters form when the ejecta from impacts protect the underlying material from erosion. As a result of this process, craters appear perched above their surroundings.

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  Drawing shows a later idea of how some pedestal craters form. In this way of thinking, an impacting projectile goes into an ice-rich layer—but no further. Heat and wind from the impact hardens the surface against erosion. This hardening can be accomplished by the melting of ice which produces a salt/mineral solution thereby cementing the surface.

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  Pedestal crater within Tikonravov Crater, as seen by HiRISE under HiWish program

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  Close view of layers along edge of pedestal crater from previous image, as seen by HiRISE under HiWish program

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  Close view of layers along edge of pedestal crater from previous image, as seen by HiRISE under HiWish program Some dark slope streaks are visible.

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  Pasteur Crater Floor, as seen by HiRISE. The scale bar is 1,000 meters long

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  Henry Crater Mound, as seen by HiRISE. The scale bar is 500 meters long

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  Mounds in craters like Henry are formed by the erosion of layers that were deposited after the impact.

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  Crater in the middle of Cassini, as seen by HiRISE. Layers may have been deposited under water since it is believed that Cassini once held a giant lake.

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  Masursky Crater Floor, as seen by HiRISE.

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  HiRISE images showing discovery of a new crater with HiWish program A study of the dark areas around new craters like this revealed that dark patches fade by global atmospheric dust deposition and are more likely to occur at higher-latitude sites, lower-elevation sites, and at sites with smaller central craters. Changing back to the surrounding albedo takes on average 15 martian years.^[1]

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  New crater, as seen by HiRISE under HiWish program. The new crater indicated with the white arrow is about 10 yards across and was probably created by the collision with an object the size of a large watermelon. This crater did not appear in earlier images of the same region.

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  Eastern edge of Janssen Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

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  Layers and dark slope streaks in northeastern edge of Janssen Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter). Note: this is an enlargement of the previous image of Janssen Crater.

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  Maggini Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

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  Marth Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

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  Marth Crater showing dunes, as seen by CTX camera (on Mars Reconnaissance Orbiter).Note: this is an enlargement of the previous image of Marth Crater.

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  Teisserenc de Bort Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

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  Northern wall of Teisserenc de Bort Crater showing dark slope streaks, as seen by CTX camera (on Mars Reconnaissance Orbiter). Note this is an enlargement of the previous image.

1. ^ Daubar, I., C. Dundas, S. Byrne, P. Geissler, G. Bart, A. McEwen, P. Russell, M. Chojnacki, M. Golombek 2016. Changes in blast zone albedo patterns around new martian impact craters. Icarus: 267, 86-105.

Possible methane

One study with the Planetary Fourier Spectrometer in the Mars Express spacecraft found possible methane in three areas of Mars, one of which was in Arabia. One possible source of methane is from the metabolism of living bacteria.^[23] However, a recent study indicates that to match the observations of methane, there must be something that quickly destroys the gas, otherwise it would be spread all through the atmosphere instead of being concentrated in just a few locations. There may be something in the soil that oxidizes the gas before it has a chance to spread. If this is so, that same chemical would destroy organic compounds, thus life would be very difficult on Mars.^[24][25]

Deformation bands

The Mars Reconnaissance Orbiter showed deformation bands in Capen Crater, located in the Arabia quadrangle. Deformation bands are small faults with very small displacements.^[26] They often proceed large faults. They develop in porous rocks, like sandstone. They can restrict and/or change the flow of fluids like water and oil. They are common in the Colorado Plateau.^[27] Good examples form in the Entrada Sandstone in the San Rafael Swell in Utah.^[28] The bands represent failure by localized frictional sliding.^[29][30] The bands on Mars are a few meters wide and up to a few kilometers long. They are caused by the compression or stretching of underground layers. Erosion of overlying layers make them visible at the surface. Capen Crater was unnamed before the discovery of deformation bands. It was named for Charles Capen, who studied Mars at JPL's Table Mountain Observatory in California and at Lowell Observatory in Arizona.^[31]

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  The group of lines running up and down in the image are believed to be deformation bands. They can be thought of as small faults.

Geological history

Recent studies, reported in the journal Icarus, have suggested that the area underwent several phases in its formation:

• A large basin, maybe from an impact, was produced early in Martian history. It was so early that Mars still had a magnetic field generated by movements in a liquid core. Present day Arabia possesses a remnant magnetism from that ancient era.
• Sediments flowed into the basin. Water entered the basin.
• Because Tharsis, on the other side of Mars, became so massive, the area around Arabia was pushed out. As it bulged upward, there was increased erosion which exposed old layers. When portions of a planet that can be subject to erosion rise, there is greatly increased erosion; Earth's Grand Canyon became very deep because it was eroded into a high plateau.
• Over the following 4 billion years, the area was modified by various geological processes. Central peaks and ejecta shapes indicate that parts of Arabia are still water enriched.^[32][33][34]

Dark slope streaks

Streaks are common on Mars. They occur on steep slopes of craters, troughs, and valleys. The streaks are dark at first. They get lighter with age.^[35] Sometimes they start in a tiny spot, then spread out and go for hundreds of meters. They have been seen to travel around obstacles, like boulders.^[36] It is believed that they are avalanches of bright dust that expose a darker underlying layer. However, several ideas have been advanced to explain them. Some involve water or even the growth of organisms.^[37][38][39] Streaks appear in areas covered with dust. Much of the Martian surface is covered with dust. Fine dust settles out of the atmosphere covering everything. We know a lot about this dust because the solar panels of the Mars Rovers get covered with dust, thus reducing the electrical energy. The power of the Rovers has been restored many times by the wind, in the form of dust devils, cleaning the panels and boosting the power. So, we know that dust settles from the atmosphere then returns over and over.^[40] Dust storms are frequent, especially when the spring season begins in the southern hemisphere. At that time, Mars is 40% closer to the sun. The orbit of Mars is much more elliptical then the Earth's. That is the difference between the farthest point from the sun and the closest point to the sun is very great for Mars, but only a slight amount for the Earth. Also, every few years, the entire planet is engulfed in global dust storms. When NASA's Mariner 9 craft arrived there, nothing could be seen through the dust storm.^[17][41] Other global dust storms have also been observed, since that time.

Research, published in January 2012 in Icarus, found that dark streaks were initiated by airblasts from meteorites traveling at supersonic speeds. The team of scientists was led by Kaylan Burleigh, an undergraduate at the University of Arizona. After counting some 65,000 dark streaks around the impact site of a group of 5 new craters, patterns emerged. The number of streaks was greatest closer to the impact site. So, the impact somehow probably caused the streaks. Also, the distribution of the streaks formed a pattern with two wings extending from the impact site. The curved wings resembled scimitars, curved knives. This pattern suggests that an interaction of airblasts from the group of meteorites shook dust loose enough to start dust avalanches that formed the many dark streaks. At first it was thought that the shaking of the ground from the impact caused the dust avalanches, but if that was the case the dark streaks would have been arranged symmetrically around the impacts, rather than being concentrated into curved shapes.^[42][43]

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  Tikonravev Crater Floor, as seen by Mars Global Surveyor, under the MOC Public Targeting Program. Click on image to see dark slope streaks and layers.

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  Tikhonravov Basin Streaks and layers, as seen by HiRISE. Scale bar is 500 meters long.

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  Dark slope streaks near the top of a pedestal crater, as seen by HiRISE under the HiWish program.

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  Dark slope streaks and layers near a pedestal crater, as seen by HiRISE under the HiWish program.

Linear ridge networks

Linear ridge networks are found in various places on Mars in and around craters.^[44] Ridges often appear as mostly straight segments that intersect in a lattice-like manner. They are hundreds of meters long, tens of meters high, and several meters wide. It is thought that impacts created fractures in the surface, these fractures later acted as channels for fluids. Fluids cemented the structures. With the passage of time, surrounding material was eroded away, thereby leaving hard ridges behind. Since the ridges occur in locations with clay, these formations could serve as a marker for clay which requires water for its formation.^[45][46][47] Water here could have supported past life in these locations. Clay may also preserve fossils or other traces of past life.

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  Linear ridge network, as seen by HiRISE under HiWish program Dark line is not part of the picture. Data was not gathered for that area.

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  Enlargement of previous image of linear ridge network, as seen by HiRISE under HiWish program

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  Dikes in Arabia, as seen by HiRISE, under the HiWish program. These straight features may indicate where valuable ore deposits may be found by future colonists. Scale bar is 500 meters. They may be part of linear ridges, hence related to impact craters.

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  Close-up of a complex group of ridges. The ridges may be the remains of old streams and/or linear ridge networks. Image taken by HiRISE under the HiWish program.

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  Small, straight ridges Image taken by HiRISE under the HiWish program.

Other landscape features in Arabia quadrangle

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  Map of Arabia quadrangle with major craters.

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  Naktong Vallis, as seen by HiRISE.

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  Indus Vallis, as seen by HiRISE.

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  Boulders and their tracks from rolling down a slope, as seen by HiRISE under HiWish program Arrows show two boulders at the end of their tracks.

Other Mars quadrangles

0°N 180°W / 0°N 180°W / 0; -180

0°N 0°W / 0°N -0°E / 0; -0

90°N 0°W / 90°N -0°E / 90; -0

MC-01

Mare Boreum

MC-02

Diacria

MC-03

Arcadia

MC-04

Mare Acidalium

MC-05

Ismenius Lacus

MC-06

Casius

MC-07

Cebrenia

MC-08

Amazonis

MC-09

Tharsis

MC-10

Lunae Palus

MC-11

Oxia Palus

MC-12

Arabia

MC-13

Syrtis Major

MC-14

Amenthes

MC-15

Elysium

MC-16

Memnonia

MC-17

Phoenicis

MC-18

Coprates

MC-19

Margaritifer

MC-20

Sabaeus

MC-21

Iapygia

MC-22

Tyrrhenum

MC-23

Aeolis

MC-24

Phaethontis

MC-25

Thaumasia

MC-26

Argyre

MC-27

Noachis

MC-28

Hellas

MC-29

Eridania

MC-30

Mare Australe

The thirty cartographic quadrangles of Mars, defined by the United States Geological Survey.^[48][51] The quadrangles are numbered with the prefix "MC" for "Mars Chart."^[52] Click on a quadrangle name link and you will be taken to the corresponding article. North is at the top; 0°N 180°W / 0°N 180°W / 0; -180 is at the far left on the equator. The map images were taken by the Mars Global Surveyor.

[]

Interactive Mars map

Interactive imagemap of the global topography of Mars. Hover your mouse to see the names of over 25 prominent geographic features, and click to link to them. Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor. Reds and pinks are higher elevation (+3 km to +8 km); yellow is 0 km; greens and blues are lower elevation (down to −8 km). Whites (>+12 km) and browns (>+8 km) are the highest elevations. Axes are latitude and longitude; Poles are not shown.

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See also

References

External links

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