Earth observations taken during the STS-60 mission

STS060-83-004 (3-11 Feb 1994) --- In this winter scene of the Grand Canyon of Arizona, the canyon is particularly well revealed because snow lies on the rims of the canyon, and exits mid-right; the Little Colorado River enters from the left, joining the Colorado just upstream of its big bend. Visitors to the South Rim can view the canyon in both the east-west and north-south reaches. The South Rim is closer to centers of transportation so that tourists mostly see the canyon from this area, that is from about 7,000 feet. The canyon floor lies at 2,000 feet in this sector. The most heavily snow covered area is the highest, reaching more than 9,000 feet (bottom right). Visitors see this protected area by hiking and mule and helicopter rides. The ecology of this part of the Colorado has been changed since the building of a lake upstream: river water is now derived from snow melt water from the bottom of the lake. This water is much colder than the water which used to flow through the canyon. According to NASA scientists, the view is unusual because the snow also reveals so well the higher country around the canyon, a swath stretching from bottom right to middle left of the view. This higher swath is an arch of uplifted rocks known as the Kaibab Plateau, raised vertically by tectonic forces in the recent geologic past. Despite this up parching, the Colorado River managed to maintain its course to the sea by cutting an ever deeper canyon into the Plateau. The white snow cover hides the fact that the Kaibab Plateau is thickly forested and thus appears dark green in summer, except in areas of clear-cutting. Since the Plateau reaches altitudes of 6 to 9,000 feet, it is both cooler and moister than the surrounding lower desert floor (top and bottom in this view) - where sparse vegetation and rocky country appear as brown colors. The zone of dark color running parallel to the snow line is all that can be seen of the pine forest on the south flanks of the Plateau.