Thaindian News

Washington, October 11 (ANI): The map shows two lava flows: the younger flow exhibits flow structures, pressure ridges as well as the central lava channel.

An older flow visible in the lower portion has a smoother surface owing to gradual accumulation of sediments

Two striking depressions lying almost at right angles to the lava flow are also visible in the upper portion of the imaged region.

These structures are related to grabens that existed earlier (grabens are depressional features formed by faults in the crust).

It is likely that the lava flows invaded the grabens partially or filled them up completely. Where a graben was only partially filled, the original dimensions are still recognisable.

In the upper left of the nadir image is a portion of this feature that remains unmodified by the younger lava flows.

Existing impact craters have also been transformed by the lava flows. The two larger craters show different stages of modification.

The largest crater was not affected by the lava flow, but the ejecta blanket formed during the impact is partially covered in lava.

The second largest crater has been flooded almost entirely, although minor portions of the rim are still preserved. It is likely that the lava entered through a breach in the rim, filling it up.

Fully covered impact craters, whose outlines are still visible, are also known as ghost craters. One such ghost crater is located in the immediate vicinity of the second largest impact crater.

The colour scenes have been derived from the three HRSC-colour channels and the nadir channel.

The perspective views have been calculated from the digital terrain model derived from the stereo channels. (ANI)