Tectonic plate consist of lithospheric mantle overlain by crustal
The lower part of the mantle is actually names the mesosphere. It is overlain by the asthenosphere which is part of the upper mantle and this in turn is overlain by the lithosphere which is made up of the very uppermost mantle and the crust.
An angular unconformity is characterized by tilted or folded sedimentary layers overlain by horizontal layers, indicating a period of deformation and erosion before new deposition. In contrast, a nonconformity is marked by the erosion of older igneous or metamorphic rocks, with younger sedimentary layers deposited on top, showing a gap in the geologic record due to uplift and erosion.
Clay can form a barrier to water flow and prevent the formation of a good aquifer. However, if the clay layer is thick and overlain by a permeable layer, it can act as a confining layer for an underlying aquifer, enhancing its ability to hold water. Ultimately, the presence of other factors like the porosity and connectivity of the rock material will determine if a good aquifer can form in a layer of clay.
The type of nonconformity described is known as an "angular unconformity." This occurs when older, tilted sedimentary rocks are eroded and subsequently covered by younger, horizontally deposited sedimentary layers. The angular relationship between the two rock sets indicates a period of geological activity, such as folding or tilting, followed by erosion and new sediment deposition.
Tectonic plate consist of lithospheric mantle overlain by crustal
Tectonic plate consist of lithospheric mantle overlain by crustal
angular unconformity
angular unconformity is the answer because it is tilted
There are 10,000 ways to die and the approach of the one pertinent in any case is overlain by a tremulous cloud of misperceived cares.
angular unconformity
The lower part of the mantle is actually names the mesosphere. It is overlain by the asthenosphere which is part of the upper mantle and this in turn is overlain by the lithosphere which is made up of the very uppermost mantle and the crust.
Sedimentary rocks (most famously those forming Hutton's unconformity formed by steeply dipping tectonically disturbed Silurian greywackes overlain by Devonian sandstones).
An angular unconformity, which is what I think you mean, is not a rock type. It denotes the junction of two strata of rocks where the lower one was tilted by tectonic forces, eroded, then overlain with horizontal parallel strata.
Most of the mesa's in Arizona are sandstone. The area encompasses part of the northern Superstition Mountains and southern Mazatal Mountains. Bedrock in this area consists largely of proterozoic granitic and metamorphic rocks overlain by a thick sequences of early miocene volcanic rock.
Angular unconformities form when previously deposited rock layers are tilted or folded, eroded, and then overlain by younger, horizontal layers. This tilting and erosion create an angular discordance between the older and younger rock layers. This process often signifies a significant gap in the geologic record.
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.