Disconformity
A paraconformity is a type of unconformity where the rock layers are parallel with no visible erosional surface in between. An example would be a horizontal layer of sandstone deposited on top of another horizontal layer of sandstone with no signs of disturbance or erosion between them.
When magma intrudes parallel to another rock layer, the formation is called a "sill." Sills are typically formed when magma cools and solidifies between existing layers of sedimentary rock or other geological formations. This process can create horizontal or nearly horizontal intrusions, resulting in distinctive geological features.
network layer
When magma intrudes parallel to another rock layer, the formation is called a "sill." Sills are typically horizontal or gently inclined and form when magma forces its way between existing rock layers without breaking through to the surface. This process can create distinct mineral compositions and textures within the surrounding rock.
The transition layer between the mixed layer at the surface and the deep water layer.
transport layer processes occur between the applicaitoin layer and internet layer of the TCP/IP and between the session layer and network layer of the OSI model.
The HAL (hardware abstraction layer) is the layer between the OS and the hardware
Make one layer, wait for it to dry, then repeat with the following layer.
An aquifer forms when groundwater pools between a permeable layer and an impermeable layer.
An aquifer forms when groundwater pools between a permeable layer and an impermeable layer.
The stratopause is the layer between the troposphere and the stratosphere.
difference between single layer and double winding