Formation
Erosion of the clay underlay of the basalt plateau (cap) started to create a v-valley. The edges of the cap broke off. These blocks travelled downwards along the hill sides towards the bottom of the valley, where they accumulated. They fill now a portion of the valley which is about 1.4 km long and up to 350 m wide. There is no evidence of another valley world wide, composed of a huge number of basalt rocks, resting on a clay base.
Read more about this topic: Horeke Basalts
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