This is indicative of Metamorphic rock
Shale is a type of rock that typically has uneven layers of minerals. These layers are often created through the deposition of clay and silt particles over time, resulting in a distinct banded appearance in the rock.
An example of differential weathering is when a rock formation is composed of both hard and soft layers. Over time, the softer layers erode more quickly, creating uneven surfaces or features like hoodoos in sedimentary rock formations.
Geologists know that rock layers are undisturbed by examining the relationships between the different layers. If the layers are parallel and show no signs of folding, tilting, or faulting, they are likely undisturbed. Additionally, the presence of index fossils can help date the layers and determine if they have been disturbed.
Rock layers that are arched upward typically form anticlines. Anticlines are characterized by an upward curve or fold in rock layers where the oldest layers are found in the center of the fold and the youngest layers are found on the outer edges.
A sill is formed when magma is forced into layers parallel to the surrounding rock layers. Sills are characterized by their tabular shape and are often found intruding between rock layers.
Uneven rock layers.
Shale is a type of rock that typically has uneven layers of minerals. These layers are often created through the deposition of clay and silt particles over time, resulting in a distinct banded appearance in the rock.
What may happen to a rock/mineral is that the softer layers of a rock that are closest to the surface get weathered or eroded away while the harder center parts do not. This usually results in interesting and uneven rock shapes. Also, some weathering isn't exactly even in terms of the surface of a rock.
Yes Karana does sleep on a uneven rock
An example of differential weathering is when a rock formation is composed of both hard and soft layers. Over time, the softer layers erode more quickly, creating uneven surfaces or features like hoodoos in sedimentary rock formations.
Aquifers are permeable layers of rock that have non permeable layers of rock under them so water remains in the permeable layers
Rock layers that are forming are stratifying.
The rock layers will be easily visible.
Sedimentary rock layers. your welcome
there are many layers
A sill is a slab of volcanic rock formed when magma squeezes between layers of rock. It is typically horizontal and parallel to the surrounding rock layers. Sills are distinguishable from dikes, which cut across the rock layers.
Foliated rock has parallel layers.