Fig. 17

Formation and evolution of the accumulation basins on Imhotep. A) Primordial void into the nucleus, resulting from its formation process. B) Progressive erosion of the surface and thinning down of the layer of material above the void. C) and D) collapse of the thin upper layer. E) Enlargement of the basin and infill with eroded material of the edges. Possible formation of overhangs.
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