sedimentary
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.
Uneven rock layers.
Apologies, but I do not know what unconformity you are referring to. However, I can tell you that conglomerate IS present as an unconformity in many cases due to the nature of it's formation. Conglomerate is often produced during a flash-flood, so all rock strata from the period appear interrupted by the unconformity of Conglomerate which was deposited very quickly, then after burial was cemented and lithified. My answer, therefore, is that conglomerate is common as an unconformity.
Unconformity
Fossils are most likely to be found in sedimentary rock.
Granite.
The most common type of unconformity is an angular unconformity, where older tilted layers of rock are overlain by younger horizontal layers, indicating a period of deformation and erosion before deposition of the younger layers.
unconformity
An unconformity between two sedimentary layers is most likely produced by a period of erosion or non-deposition that interrupts the sedimentation process. This can occur due to tectonic activity, sea-level changes, or climate shifts that halt sediment accumulation and create a gap in the rock record.
Igneous.
africa.
Sedimentary rock like sandstone
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.
Uneven rock layers.
angular 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.