The ones associated with the fault you observed in the GigaPan image:
- Extension of the crust
- Tensional environment
- Normal fault
When rocks slip through each other in a fault, the upper or overlying blocks along the fault plane are called hanging walls or headwalls. The underlying blocks are called foot walls. Tectonic basins are formed by crustal activity. A dimple is a fold where the originally horizontal layer is folded and the two legs of the fold are folded.
Tectonic activity is the movement of large portions of the Earth's crust called tectonic plates. Crustal activity is the cause of phenomena such as earthquakes and volcanoes. Gneiss is a type of metamorphic rock that forms when the sedimentary or igneous rock is subjected to extreme temperatures and pressures.
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