Angular unconformity :D
Erosion
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Child is the full form of child.
simplest form, reduced form, free form
An unconformity is a gap in the sedimentary rock record. This animation shows the formation of an angular unconformity-one where the layers above and below the unconformity are not parallel to each other, but form an angle.
Tilted strata lie below the unconformity; bedding in younger strata above is parallel to the unconformity.
Deposition: Sediments must be deposited on a surface, such as a rock layer or land surface. Erosion: The deposited sediments must then be removed through processes like weathering and erosion, exposing the underlying surface to create an unconformity.
It is usually due to erosion of lack of deposition.
Angular unconformity :D
angular unconformity
1) Deposition of sediment 2) Rocks are uplifted and eroded 3) Erosion of strata 4) New rock is laid down on top of older rock 5) Uplift and erosion exposes the unconformity at the surface
unconformity
Angular unconformity is a type of unconformity in which tilted or folded rock layers are overlain by horizontal rock layers. This indicates a period of deformation and erosion followed by deposition of younger sedimentary layers. It represents a gap in the geologic record.
Well...there are two definitions of unconformity... Unconformity: the stop in rock sequence indicating interruption of sedimentation, commonly accompanied by erosion of rocks below the break. Sentence: The scientist predicted that an unconformity occurred at the area, theorizing why it was smaller than the other volcanic and sedimentary rock sequences. Or... Unconformity: inconsistency, incongruity Sentence: The unconformity of the schedule threw off the secretary; her boss had always been so uptight about his agenda, so today was quite the change.
An unconformity is a gap in the rock record where erosion, sedimentation, or tectonic activity has disrupted the sequence of layers. The presence of an unconformity implies that a significant amount of time has passed because it represents a hiatus in deposition or significant geological events that have occurred in between the layers. Geologists can use the presence of unconformities to infer periods of erosion, uplift, or non-deposition that separate the layers, indicating a lengthy temporal gap in the rock record.
an angular unconformity.