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Table 1 Key features of the three investigated landslides

From: Inferring the high velocity of landslides in Valles Marineris on Mars from morphological analysis

Features

Melas Chasma

Ophir Labes

Coprates Labes

Runout (km)

100–120

40/60/65

65

Deposit area (km2)

2500

2700

1900

Source area (km2)

70

60

330

Fall height (km)

9

6

4.5

Volume, Quantin et al. (2004a) (km3)

376

458

346

Fahrböschung

0.075

0.120

0.069

  1. We list the runout distance, the area of the deposit and of the source, the maximum fall height, the estimated volume, and the Fahrböschung (i.e., the fall height divided by the runout)