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
Unconformity
The relative age of a fault or igneous intrusion that cuts through an unconformity is younger than the unconformity but older than the rock it cuts through. This is because the fault or intrusion must have formed after the deposition of the rock layers below the unconformity but before the deposition of the rock layers above the unconformity.
We can not see you diagram so can not answer your question. However unconformities come in these typesDisconformitiesNonconformitiesAngular unconformitiesParaconformitiesButtress unconformitiesBlended unconformities
Tilted strata lie below the unconformity; bedding in younger strata above is parallel to the unconformity.
Angular unconformity :D
angular unconformity
Unconformities are surfaces that represent gaps in the geologic record that formed wherever layers were not deposited for a time or else layers were removed by erosion.
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.
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.
An unconformity indicates a period where deposition stopped, followed by erosion and then renewed deposition. The environment during the unconformity formation may have been characterized by tectonic activity, sea level changes, or climate shifts, which interrupted the sedimentation process. The presence of an unconformity suggests a dynamic geological history in that area.