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VL1 Digs A Deep Hole On Mars
PIA00529
Sol (our sun)
Camera 1
| Title |
VL1 Digs A Deep Hole On Mars |
| Original Caption Released with Image |
VIKING LANDER DIGS A DEEP HOLE ON MARS -- This six-inch-deep, 12- inch-wide, 29-inch-long hole was dug Feb. 12 and 14 by Viking Lander 1 as the first sequence in an attempt to reach a foot beneath the surface of the red planet. The activity is in the same area where Lander 1 acquired its first soil samples last July. The trench was dug by repeatedly backhoeing in a left-right-center pattern. The backhoe teeth produced the small parallel ridges at the far end of the trench (upper left). The larger ridges running the length of the trench are material left behind during the backhoe operation. What appears to be small rocks along the ridges and in the soil at the near end of the trench are really small dirt clods. The clods and the steepness of the trench walls indicate the material is cohesive and behaves something like ordinary flour. After a later sequence, to be performed March 1 and 2, a soil sample will be taken from the bottom of the trench for inorganic soil analysis and later for biology analysis. Information about the soil taken from the bottom of the trench may help explain the weathering process on Mars and may help resolve the dilemma created by Viking findings that first suggest but then cast doubt on the possibility of life in the Martian soil. The trench shown here is a result of one of the most complex command sequences yet performed by the lander. Viking l has been operating at Chryse Planitia on Mars since it landed July 20, 1976. |
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Viking Lander 1's U.S. Flag
PIA00565
Sol (our sun)
Camera 1
| Title |
Viking Lander 1's U.S. Flag on Mars Surface |
| Original Caption Released with Image |
The flag of the United States with the rocky Martian surface in the background is seen in this color picture taken on the sixth day of Viking Lander 1 on Mars (July 26). The flag is on the RTG (Radioisotope Thermoelectric Generator) wind screen. Below the flag is the bicentennial logo and the Viking symbol which shows an ancient Viking ship. This Viking symbol was designed by Peter Purol of Baltimore, winner of the Viking logo contest open to high school science students. To the right is the Reference Test Chart used for color balancing of the color images. At the bottom is the GCMS Processor Distribution Assembly with the wind screens unfurled demonstrating that the GCMS cover was deployed properly. The scene in the background is looking almost due west on Mars. The lighter zone at the far horizon is about 3 km (nearly 2 miles) from the Lander. The darker line below this is a hill crest much closer to the Lander (about 200 m or about 650 feet). The picture was taken at local Mars Time of 7:18 A.M., hence the relatively dark sky and the far horizon illuminated by the sun just rising behind the Lander. |
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Big Joe in the Chryse Planit
PIA00572
Sol (our sun)
Camera 1
| Title |
Big Joe in the Chryse Planitia |
| Original Caption Released with Image |
Near the Viking 1 Lander on the Chryse Plains of Mars, 'Big Joe' stands a silent vigil. This large, often-photographed dark rock has a topping of reddish fine-grained silt that spills down its sides. It is about 2 meters (6.6 feet) long and lies about 8 meters (26 feet) from the spacecraft. The rough texture of the sides shows it to be coarse grained. Big Joe appears to be part of a field of large blocks that has a roughly circular alignment and which may be part of the rim of an ancient degraded crater. Some of the other blocks of the field can be seen to the left, extending out toward the horizon, perhaps 1.5 kilometers (1 mile) away. Drifts of fine-grained material cover the surface to the right and left of Big Joe. The part of the Lander that is visible in the lower left is the cover of the nuclear power supply. |
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Vivid Colors of the Viking L
PIA00564
Sol (our sun)
Camera 1
| Title |
Vivid Colors of the Viking Lander 1 Scene |
| Original Caption Released with Image |
Viking 1 obtained this color picture of the Martian surface and sky on July 24. Camera Number 1 facing southeast, captured part of the spacecraft's gray structure in the foreground. A bright orange cable leads to one of the descent rocket engines. Orange-red surface materials cover most of the surface, apparently forming a thin veneer over darker bedrock. A zone of large dark boulders is present in the far-field. The sky has a reddish cast, which is probably due to scattering and reflection from reddish sediment suspended in the lower atmosphere. This picture has been radiometrically calibrated, using information on camera performance acquired before launch. Although the colors are very vivid, the fidelity with which the bright orange cable is reproduced suggests that the intense colors of the Martian surface are, in fact, real. |
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Surface Changes in Chryse Pl
PIA00532
Sol (our sun)
Camera 1
| Title |
Surface Changes in Chryse Planitia |
| Original Caption Released with Image |
At the conclusion of the Viking Continuation Mission (May to November, 1978), all four cameras on the Viking Landers - two on each spacecraft - continued to function normally. During the two and one-half years since the landers touched down on Mars, images totaled 2,255 for Viking Lander 1 and 2,016 for Viking Lander 2. The surface around the landers was completely photographed by the end of 1976, subsequent images acquired during 1977-1978 have concentrated on searching for changes in the scene - changes which can be used to infer both the types of erosive processes which modify the landscape around the landers and the rates at which these processes may occur. The major surface changes have included the water-ice snow seen by Lander 2 during the winter at Utopia Planitia, and a thin dust layer deposited at both sites during the dust storms of 1977. The most recently identified change occurred at Chryse Planitia between VL-1 sols 767 (Sept. 16, 1978) and 771 (Sept. 20, 1978) as seen in the lower photo. Picture at top, selected to show similar lighting conditions, was taken during sol 25 (August 15, 1976). The change (A) appears as a small circle-like formation on the side of a drift in the lee, or downwind, side of Whale Rock. This is believed to have been a small-scale landslide of an unstable dust layer which had accumulated behind the rock. Interpretation of this feature would be difficult without an earlier change (B) near Big Joe, a slump which occurred between sols 74 and 183. The new slump is approximately 25- 35 meters from the lander, and just under a meter across. The slumping probably was initiated by the daily heating and cooling of the surface by solar radiation. More importantly, it is now believed that, based on the repeated occurrence of such slumping features, a dust layer which overlies the surface may in fact be redistributed fairly regularly during periods of high wind activity. There are no obvious indications of fossil slump features, therefore similar features must be destroyed on a regular basis. After the end of February, when Viking operations essentially terminate, Lander 1 will continue preselected observations over a period of possibly up to 10 years, following the instructions stored in its computer memory. Earth commands will be required only to initiate data transmission to Earth. During this time, it is now anticipated that one of the yearly planetwide global dust storms may reach an intensity necessary to shift the dust cover around the lander significantly. |
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Boulder 'Big Joe' And Surfac
PIA00397
Sol (our sun)
Camera 1
| Title |
Boulder 'Big Joe' And Surface Changes On Mars |
| Original Caption Released with Image |
This pair of pictures from Viking Lander 1 at Mars' Chryse Planitia shows the only unequivocal change in the Martian surface seen by either lander. Both images show the one-meter (3-foot) high boulder nicknamed 'Big Joe.' Just to the lower right of the rock (right photo) is a small-scale slump feature. The picture at left shows a smooth, dust-covered slope, in the picture at right the top surface layer can be seen to have slipped downslope. The event occurred sometime between Oct. 4, 1976, and Jan 24, 1977. (Pictures taken before Oct. 4 do not show the slump, the first picture in which it appears was taken Jan. 24.) The surface layer, between one-half and one centimeter (one-fifth to one-third inch) thick, is apparently less cohesive than the underlying material. The layer that slipped formed a 30-centimeter-long (11.8-inch) 'tongue' of soil and a patch of exposed underlying material. The triggering mechanism for the event is unknown, but could have been temperature variations, wind gusts, a seismic event, or perhaps the lander's touchdown on July 20, 1976. |
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Northeast View from Viking L
PIA00387
Sol (our sun)
Camera 1
| Title |
Northeast View from Viking Landing Site |
| Original Caption Released with Image |
This Mars view looks northeast from Viking 1 and completes the 360 panorama of the landing site begun earlier with the spacecraft's other camera. A layer of haze can be seen in the Martian sky. Large dark boulders dominate the scene. The largest boulder (center) is about 3 meters (10 feet) wide and one meter (3 feet) high. Rocks in the foreground are lighter and appear mottled. The rocks may have been derived from lava flows or stream deposits which are visible on orbiter images. These deposits may have been redistributed by impact craters. The fine material visible between the rocks has dune morphology and appears to have been deposited by wind. |
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Example of Weathering And Su
PIA00386
Sol (our sun)
Camera 1
| Title |
Example of Weathering And Sun Angle |
| Original Caption Released with Image |
The letter 'B' or perhaps the figure '8' appears to have been etched into the Mars rock at the left edge of this picture taken yesterday by the Viking 1 Lander. It is believed to be an illusion caused by weathering processes and the angle of the sun as it illuminated the scene for the spacecraft camera. The object at lower left is the housing containing the surface sampler scoop. |
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The Meteorology Instrument o
PIA00392
Sol (our sun)
Camera 1
| Title |
The Meteorology Instrument on Viking Lander 1 |
| Original Caption Released with Image |
Those Martian weather reports, received here daily from more than 200 million miles away, start right here at Viking l's meteorology instrument. Mounted atop the extended boom, the meteorology sensors face away from the spacecraft. They stand about four feet above the surface and measure atmospheric pressure, temperature, wind velocity and wind direction. The cable parallel to the boom is connected inside the spacecraft body with the electronics for operating the sensors, reading the data and preparing it for transmission to Earth. A second Mars weather station will begin operation next month when Viking 2 lands somewhere in the planet's northern latitude Viking 2 arrives at Mars and goes into orbit tomorrow (August 7). |
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The United States Flag Stand
PIA00388
Sol (our sun)
Camera 1
| Title |
The United States Flag Stands On The Surface Of Mars |
| Original Caption Released with Image |
The flag of the United States stands on the surface of Mars. It is mounted on the housing of Viking 1's nuclear power system. Also seen are the U.S. Bicentennial symbol and a student designed Viking emblem. The bright flat surface near the center is the seismometer container. This picture was taken on July 23 at about 2:30 p.m. Mars time. The view is west of the spacecraft and includes a series of low hills. The blocky hill in the center appears to be part of a crater rim. The dark, rocky stripes may be material ejected from the crater. The light areas are dune-like and may be accumulations of windblown sand or dust. |
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Sand Dunes And Large Rocks R
PIA00391
Sol (our sun)
Camera 1
| Title |
Sand Dunes And Large Rocks Revealed By Camera 1 |
| Original Caption Released with Image |
Sand dunes and large rocks are revealed in this panorama picture of Mars, the first photograph taken by Viking l's Camera 1 on July 23. The horizon is approximately 3 kilometers (2 miles) away. The left and right thirds of this picture are the same areas that were photographed on July 20 (Sol O) by Camera 2 and provide stereo coverage. The middle third reveals a part of the Martian surface not seen on the July 20 panorama. The late afternoon sun is high in the sky over the left side of the picture. The support struts of the S-band high-gain antenna extend to the top of the picture. The American flags are located on the two RTG (Radioisotope Thermoelectric Generator) wind screens. In the middle third of the picture, the rocky surface is covered by thick deposits of wind-blown material, forming numerous dunes. At the center of the picture on the horizon are two low hills which may be part of the rim of a distant crater. Two very large rocks are visible in the middleground, the nearer one is 3 meters (10 feet) in diameter and is 8 meters (25 feet) from the spacecraft. A cloud layer is visible halfway between the horizon and the top of the picture. The meteorology boom is located right of center. Behind it, the 'White Mesa' is visible, which could be seen on the far left side of the Sol O Camera 2 panorama. In the near ground are numerous rocks about 10 cm (4 inches) across, with horseshoe-shaped scour marks on their upwind side and wind tails in their lee. The fine-grained material in front of them contains small pits formed by impact of material kicked out by the Lander spacecraft's rocket engines. |
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Viking Lander's Buried Footp
PIA00390
Sol (our sun)
Camera 1
| Title |
Viking Lander's Buried Footpad #3 |
| Original Caption Released with Image |
One of Viking l's three feet, which should be visible in this view, lies buried beneath a cover of loose Martian soil. This picture, taken Sunday (August 1), is the first to show the buried footpad #3. If not buried, the edge of the foot would be seen extending across the picture about midway between top and bottom. The foot sank about five inches, and fine-grained soil slumped into the depression and over the foot. The cracked nature of the surface near the slump area and the small, steep cliff at left indicates that the material is weakly cohesive. The surface material here is very similar mechanically to lunar soil. |
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Trench Excavated By Viking 1
PIA00389
Sol (our sun)
Camera 1
| Title |
Trench Excavated By Viking 1 Surface Sampler |
| Original Caption Released with Image |
This image, received today, shows the trench excavated by Viking 1 surface sampler. The trench was dug by extending the surface sampler collection head in a direction from lower right toward the upper left and then withdrawing the surface sampler collector head. Lumpy piles of material at end of trench at lower right was pulled by plowing from trench by the backhoe which will be used to dig trenches later in the mission. Area around trench has ripple marks produced by Martian wind. The trench which was dug early on Sol 8, is about 3 inches wide, 2 inches deep and 6 inches long. Steep dark crater walls show the grains of the Martian surface material stick together (have adhesion). The doming of the surface at far end of the trench show the granular material is dense. The Martian surface material behaves somewhat like moist sand on Earth. Evidence from the trench indicate a sample was collected and delivered to the experiments after repeated tries. The biology experiment level full indicator indicates a sample was received for analysis. The X-Ray fluorescence experiment has no indication to show it received a sample. The GCMS experiment level full indicator suggests no sample was received but this matter is being investigated. |
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Martian Dune Field
PIA00393
Sol (our sun)
Camera 1
| Title |
Martian Dune Field |
| Original Caption Released with Image |
This spectacular picture of the Martian landscape by the Viking 1 Lander shows a dune field with features remarkably similar to many seen in the deserts of Earth. The dramatic early morning lighting - 7:30 a.m. local Mars time--reveals subtle details and shading. Taken yesterday (August 3) by the Lander s camera #1, the picture covers 100 , looking northeast at left and southeast at right. Viking scientists have studied areas very much like the one in this view in Mexico and in California (Kelso, Death Valley, Yuma). The sharp dune crests indicate the most recent wind storms capable of moving sand over the dunes in the general direction from upper left to lower right. Small deposits downwind of rocks also indicate this wind direction. Large boulder at left is about eight meters (25 feet) from the spacecraft and measures about one by three meters (3 by 10 feet). The meteorology boom, which supports Viking s miniature weather station, cuts through the picture s center. The sun rose two hours earlier and is about 30 above the horizon near the center of the picture. |
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Afternoon on Chryse Planitia
PIA03165
Sol (our sun)
Camera 1
| Title |
Afternoon on Chryse Planitia - Viking Lander 1 Camera 1 Mosaic |
| Original Caption Released with Image |
During the Viking Mission, the Viking Lander Camera System acquired many high-resolution images of the scene at Chryse Planitia. Using individual camera events, which occurred on many days throughout the mission, computer mosaics have been created for the site as viewed by each of the two cameras on the spacecraft. Two sets of mosaics were produced of Chryse Planitia, one pair for camera 1 and 2 images acquired in the early morning and one pair for camera 1 and 2 images acquired in the mid-afternoon. Each complete mosaiced scene extends 342.5 degrees in azimuth, and from approximately 5 degrees above the horizon to 60 degrees below. A complete mosaic incorporated approximately 15 million picture elements (pixels). This mosaic was produced in the early morning (14:00-15:30) by the Camera 1 system on Viking Lander 1. See PIA03166 [ http://photojournal.jpl.nasa.gov/catalog/PIA03166 ]for the afternoon Camera 2 mosaic and PIA03163 [ http://photojournal.jpl.nasa.gov/catalog/PIA03163 ]and PIA03164 [ http://photojournal.jpl.nasa.gov/catalog/PIA03164 ]for the morning mosaics. |
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Morning on Chryse Planitia -
PIA03164
Sol (our sun)
Camera 1
| Title |
Morning on Chryse Planitia - Viking Lander 1 Camera 2 Mosaic |
| Original Caption Released with Image |
During the Viking Mission, the Viking Lander Camera System acquired many high-resolution images of the scene at Chryse Planitia. Using individual camera events, which occurred on many days throughout the mission, computer mosaics have been created for the site as viewed by each of the two cameras on the spacecraft. Two sets of mosaics were produced of Chryse Planitia, one pair for camera 1 and 2 images acquired in the early morning and one pair for camera 1 and 2 images acquired in the mid-afternoon. Each complete mosaiced scene extends 342.5 degrees in azimuth, and from approximately 5 degrees above the horizon to 60 degrees below. A complete mosaic incorporated approximately 15 million picture elements (pixels). This mosaic was produced in the early morning (7:00-8:00) by the Camera 2 system on Viking Lander 1. See PIA03163 [ http://photojournal.jpl.nasa.gov/catalog/PIA03163 ]for the morning Camera 1 mosaic and PIA03165 [ http://photojournal.jpl.nasa.gov/catalog/PIA03165 ]and PIA03166 [ http://photojournal.jpl.nasa.gov/catalog/PIA03166 ]for the afternoon mosaics. |
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Morning on Chryse Planitia -
PIA03163
Sol (our sun)
Camera 1
| Title |
Morning on Chryse Planitia - Viking Lander 1 Camera 1 Mosaic |
| Original Caption Released with Image |
During the Viking Mission, the Viking Lander Camera System acquired many high-resolution images of the scene at Chryse Planitia. Using individual camera events, which occurred on many days throughout the mission, computer mosaics have been created for the site as viewed by each of the two cameras on the spacecraft. Two sets of mosaics were produced of Chryse Planitia, one pair for camera 1 and 2 images acquired in the early morning and one pair for camera 1 and 2 images acquired in the mid-afternoon. Each complete mosaiced scene extends 342.5 degrees in azimuth, and from approximately 5 degrees above the horizon to 60 degrees below. A complete mosaic incorporated approximately 15 million picture elements (pixels). This mosaic was produced in the early morning (7:00-8:00) by the Camera 1 system on Viking Lander 1. See PIA03164 [ http://photojournal.jpl.nasa.gov/catalog/PIA03164 ]for the morning Camera 2 mosaic and PIA03165 [ http://photojournal.jpl.nasa.gov/catalog/PIA03165 ]and PIA03166 [ http://photojournal.jpl.nasa.gov/catalog/PIA03166 ]for the afternoon mosaics. |
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Afternoon on Chryse Planitia
PIA03166
Sol (our sun)
Camera 1
| Title |
Afternoon on Chryse Planitia - Viking Lander 1 Camera 2 Mosaic |
| Original Caption Released with Image |
During the Viking Mission, the Viking Lander Camera System acquired many high-resolution images of the scene at Chryse Planitia. Using individual camera events, which occurred on many days throughout the mission, computer mosaics have been created for the site as viewed by each of the two cameras on the spacecraft. Two sets of mosaics were produced of Chryse Planitia, one pair for camera 1 and 2 images acquired in the early morning and one pair for camera 1 and 2 images acquired in the mid-afternoon. Each complete mosaiced scene extends 342.5 degrees in azimuth, and from approximately 5 degrees above the horizon to 60 degrees below. A complete mosaic incorporated approximately 15 million picture elements (pixels). This mosaic was produced in the early morning (14:00-15:30) by the Camera 2 system on Viking Lander 1. See PIA03165 [ http://photojournal.jpl.nasa.gov/catalog/PIA03165 ]for the afternoon Camera 1 mosaic and PIA03163 [ http://photojournal.jpl.nasa.gov/catalog/PIA03163 ]and PIA03164 [ http://photojournal.jpl.nasa.gov/catalog/PIA03164 ]for the morning mosaics. |
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