| ISS013 Earth Sciences and Image Analysis Photographic Highlights |
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| ISS013-E-65526 |
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| Dune Types in the Issaouane Erg, Eastern Algeria: This view
from one of the smaller dune seas in the central Sahara Desert shows
the complex but regular patterns produced in deserts where wind and
sand both abound. The image is centered at 26.9 North, 7.4 East, over
eastern Algeria. Geologists now know that dune seas (also called
ergs) exhibit at least three orders of dune size. The biggest dunes,
called mega-dunes, probably took hundreds of thousands of years to
accumulate, starting when the Sahara began turning arid roughly 2.5
million years ago. Rivers became smaller, failed to reach the sea,
and deposited their sand load in the desert. Wind did the rest,
blowing the sand into aerodynamic dune forms. Superimposed on the
mega-dunes are mesoscale dunes (the prefix meso- means
“intermediate.”) Whereas the mega-dunes are apparently stationary,
studies based on aerial photographs in other parts of the world show
that mesoscale dune crests move in the course of decades. The
smallest dunes form and reform the fastest, meandering over the backs
of the larger dunes. In this image, the mega-dunes appear as big, rolling lumps that zigzag toward the upper right. The “streets” between these biggest dune chains have been swept clean of sand in places, showing their original surfaces of pale mud and salts. The pale beige-grey of these areas contrasts with the otherwise burnt orange hues. Mesoscale dunes, some of which form octopus-like crests, or star dunes, mark the backs of the mega-dunes. The smallest dunes appear in patches on the eastern sides of the mega-dunes as a tracery of closely spaced crests. Interestingly, the crest orientation of the small dunes differs from the orientation of the mesoscale dunes. This difference is a common effect of local shifts in wind direction, which is influenced by dune height. The orientation trends in the mega-dunes coincide with two of the four major trends identified in the Great Eastern Sand Sea (or Grand Erg Oriental) immediately to the north. Each orientation shift likely implies a shift in the direction of the dominant wind that formed the dunes, attesting to the climate shifts that have occurred since sand began to accumulate in the central Sahara. |
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This service is provided by the International Space Station program and the JSC Astromaterials Research & Exploration Science Directorate. Recommended Citation: Image Science and Analysis Laboratory, NASA-Johnson Space Center. "The Gateway to Astronaut Photography of Earth." . |
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