Ripple marks likely indicate that a rock formed in a sedimentary environment, such as near a shoreline or in a river bed, where the movement of water created the distinct ripple pattern in the sediment before it hardened into rock. These marks provide information about the ancient depositional environment and the direction of water flow at the time of formation.
I think the answer is called ripple marks
In general, ripple marks are those marks left by water or wind or a surface they have affected. Ripple marks caused by water may appear on rock, or on sand caused by water or wind. Use the link below for more information and some pics.
The markings on sedimentary rocks that record the wave motion of wind or water are called ripple marks. They form as sediment is deposited and then ripples are preserved in the rock as it solidifies.
Magma emplacements or Batholith are not sedimentary structures.
Ripple marks likely indicate that a rock formed in a sedimentary environment, such as near a shoreline or in a river bed, where the movement of water created the distinct ripple pattern in the sediment before it hardened into rock. These marks provide information about the ancient depositional environment and the direction of water flow at the time of formation.
Ripple marks in rocks are formed by the action of water or wind moving sediment on the surface of a sedimentary layer. As the sediments get deposited and compacted, the ripple marks are preserved in the rock. These structures provide important clues about the original environment in which the rocks formed.
Sedimentary rocks show fossils, because of pre-existing life forms. They also show ripple marks due to weathering and erosion...
I think the answer is called ripple marks
In general, ripple marks are those marks left by water or wind or a surface they have affected. Ripple marks caused by water may appear on rock, or on sand caused by water or wind. Use the link below for more information and some pics.
Ripple marks
Ripple marks in sedimentary rocks indicate the presence of flowing water, such as in a river or a shallow sea. They form when sediments are deposited by the movement of water, creating distinctive ridges and troughs. Ripple marks can provide insights into the direction and energy of ancient water currents.
The markings on sedimentary rocks that record the wave motion of wind or water are called ripple marks. They form as sediment is deposited and then ripples are preserved in the rock as it solidifies.
Magma emplacements or Batholith are not sedimentary structures.
The presence of ripple marks indicates that the area where the rock formed used to be covered by moving water, such as a river, stream, or a wave-dominated shoreline. Ripple marks provide evidence of past water currents and can help geologists interpret the depositional environment of the rock.
Ripple marks in sandstone can form due to the heat action of hot fluids or gases moving through the sedimentary layers. This process can cause the sand grains to align in a ripple pattern as the sediment is compacted and cemented into rock over time.
The wavy features found on sandstone are known as cross-bedding or ripple marks. They are formed by the movement of water or wind, which creates layers of sediment that are inclined at an angle to the main horizontal layering of the rock. These features can provide information about the direction and intensity of the ancient currents that deposited the sediment.