Olympia Undae

Scaled Image

Image Credit: NASA/JPL/ASU

About this image

This VIS image of Olympia Undae was collected during north polar spring. The dunes are still partially covered by the winter frosts; as the region heats up the frost will dissipate to reveal the dark sand beneath. The density of dunes and the alignments of the dune crests varies with location, controlled by the amount of available sand and the predominant winds over time.

Olympia Undae is a vast dune field in the north polar region of Mars. It consists of a broad sand sea or erg that partly rings the north polar cap from about 120° to 240°E longitude and 78° to 83°N latitude. The dune field covers an area of approximately 470,000 km2 (bigger than California, smaller than Texas). Olympia Undae is the largest continuous dune field on Mars. Olympia Undae is not the only dune field near the north polar cap, several other smaller fields exist in the same latitude, but in other ranges of longitude, e.g. Abolos and Siton Undae. Barchan and transverse dune forms are the most common. In regions with limited available sand individual barchan dunes will form, the surface beneath and between the dunes is visible. In regions with large sand supplies, the sand sheet covers the underlying surface, and dune forms are found modifying the surface of the sand sheet. In this case transverse dunes are more common. Barchan dunes "point" down wind, transverse dunes are more linear and form parallel to the wind direction. The "square" shaped transverse dunes in Olympia Undae are due to two prevailing wind directions.

Please see the THEMIS Data Citation Note for details on crediting THEMIS images. 

Context

Image ID: 
V95223007 (View data in Mars Image Explorer)
81.624
206.115
95223
2023-06-02 23:41
Thu, 2024-01-04
VIS
512 pixels (19 km)
1824 pixels (68 km)
0.037544 km/pixel
0.0378538 km/pixel

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