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1976 July-September - NASA Ames History Office

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National Aeronautics and<br />

Space Ad ministration<br />

<strong>Ames</strong> Research Center<br />

Moffett Field Caldornia 94035<br />

VOLUME XVIlt NUMBER 23<br />

Successful landing on Mars for Viking 1<br />

Upper left<br />

Jury 29. <strong>1976</strong><br />

Viking ] landed in one of the lowest regions on<br />

the surface of Mars Center of the landing elhpse<br />

instTibed on this photomosaie of frames is located at<br />

224° N Lat. 4Z5~ W L~mg inChr)sePlanitia The<br />

new location i~ about 740 kilometers (460 miles)<br />

northwest of the original <strong>July</strong> 4 landing site and<br />

240 kilometers (150 miles) west of an alternate site<br />

where the spacecraft was to touch dowt~ on Jul) 17<br />

This area ~ nearl) three kilometers (two miles)<br />

below Mars ’ mean "sea level "" It is a ehannelled lowland<br />

northeast of the great /¢Jartlan ~,olcanoes and<br />

the Tharsis Plateau the high altitude equatorial<br />

region.<br />

Lower left<br />

First panoramw view by Vtk#zg l from the surthee<br />

o/ Mars tTop) 7he out-otZJbeas spacecraft<br />

component toward left center is the housing for the<br />

Viking sample arm, which is not yet depto3 ed. Parallel<br />

lines #1 the SkF are an art(tat! and are not real<br />

features. However. the change of brightness from<br />

horiz~m toward~ -~enith and towards the right (west)<br />

L~ accurately reflected tn this picture, taket~ in late<br />

Martian afternoon At the horizon to the left is a<br />

plateau-like prominence much brighter than the<br />

/oreground material between the rocka. The horizon<br />

features are approximateZ) three k~tometers<br />

(1 8 miles) away At left ts a collection of finegrained<br />

mater~al remmLwent of sand dunes¯ The<br />

dark ~inuous markings in le/t .if>reground are of<br />

unknown origin. Some unidentd?ed shapes can be<br />

perceived on the hilh eminence at the horizon<br />

towards the right Pa&he.~ ~l bright sand can be<br />

discerned amg~ttg the r(~c ks and bouMers in middle<br />

distance In r~gh: toregmund are two peculiarh<br />

.rhaped r~wks which may posribh be vent~tacts produced<br />

bl’ wind abrasum on Mars: .4 horizontal chmd<br />

stratum c~tn be rrusde out halfway O’om the horLzon<br />

to the top of the picture eBottomt At le¢t is seet~<br />

the low gaJ~? antenna f~r receipt ojcommands From<br />

the Earth The pro/ection~ cm or near the hurL-on<br />

ma)" represdnt lhe rolls alL, rant ltnpact craters [tl<br />

right .{bregr~mnd are color charts .l}~r Lander camera<br />

calibration, a mirror tbr the |qking magnetic propertWs<br />

cvperPm’nt and part of a grid on the top of the<br />

Lander bad!..4t upper right is the high-gain dish<br />

antetma /or direct commut~icatiotl betweetr latlded<br />

spacecraJ? and Earth Toward the right edge is an<br />

array ~ff smooth free-grained material wtmh shows<br />

some hint of ripple structure and may be the beginning<br />

of a large dune field oft to the right t~.f the<br />

picture, which joins with dunes seen at the top h’ft<br />

in this 300° panorami~ flew. Sume of the rocks<br />

appear to be undercut on one side and parttalh<br />

buried b~ drifting sand on the othet~

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