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Climatic Geomorphology
Figure 12.1. Hamada covered by lag angular boulders. In the central part, there is a small closed hollow
(referred to as a "daya" in the Sahara) filled with fine deposits lighter in colour. This deposit may come
from eolian material, which has been reworked by run-off. Rann, Thar Desert, India.
Figure 12.2. Typical reg of rounded clasts developed on an alluvial plain. Bhojka, Thar Desert, India.
Climatic Geomorphology
Figure 12.1. Hamada covered by lag angular boulders. In the central part, there is a small closed hollow
(referred to as a "daya" in the Sahara) filled with fine deposits lighter in colour. This deposit may come
from eolian material, which has been reworked by run-off. Rann, Thar Desert, India.
Figure 12.2. Typical reg of rounded clasts developed on an alluvial plain. Bhojka, Thar Desert, India.