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The formation of sedimentary rocks through sediment deposition and the impact of tectonic processes such as uplift and erosion. Topics include original horizontality, superposition, cross-cutting relationship, and different types of faults and unconformities.
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Typology: Summaries
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uplift
erosion
sediment deposited more sediment deposited more sediment deposited more sediment deposited
sediment deposited more sediment deposited and lithified to form sedimentary rock
rocks deformed by tectonic stress rocks uplifted and eroded
sediment deposited and lithified
Later, clasts derived from the lower unit are included in the next later of sediment
Any rock in the Earth’s crust
Magma intrudes, picking up inclusions from the surrounding rock, then cools to form igneous rocks with inclusions
undisturbed rocks tectonic stress causes the rock to fracture and shoves the upper block up over the lower block
reverse fault
sediment deposited
sediment deposition stops. Time passes. New sediment may be deposited, but is eroded away.
sediment deposition begins again. The contact betwen the sedimentary units is a disconformity
sediment deposited and lithified to form sedimentary rocks and buried
rocks tilted by tectonic stress, uplifted to the surface and eroded
new sediment deposited on top of erosional surface, forming and angular unconformity.
disconformity
angular unconformity
metamorphic and/or igneous rock forms deep within the Earth
Rock units uplifted to the surface of the Earth and eroded
uplift
erosion
uplift
erosion
nonconformity
Sediment deposited on non-conformity
tectonic stress causes the rock to fracture and lower block slides down relative to upper block
normal fault