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I think the answer is called ripple marks
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.
The presence of marine fossils within the limestone is the best observation that shows it was formed from ocean sediments. Marine fossils like shells, corals, or sea creatures preserved within the rock provide direct evidence of its marine origin. Additionally, the presence of ripple marks or cross-bedding in the limestone can also indicate its formation in a marine environment.
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 in sedimentary rock were emplaced in sediments by near shore wave action, covered by additional sediments, and eventually lithified into a solid rock which becomes exposed by weathering and erosion of overlying material over large expanses of time.
Ripple marks typically indicate that a rock formed in a shallow, watery environment, such as a riverbed, lake, or coastal area. These features are created by the movement of water over sediment, leading to the formation of small, wavelike patterns. Consequently, the presence of ripple marks in sedimentary rocks suggests that they were deposited in conditions where currents or waves were active.
I think the answer is called ripple marks
They initially are formed by moving water which arranges sediment in patterned formations. If the ripples in the sediment are covered with other sediments before being obliterated, or if the ripple marks dry, and are then covered with subsequent sediments, they may eventually be preserved in the rock strata.
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.
The presence of marine fossils within the limestone is the best observation that shows it was formed from ocean sediments. Marine fossils like shells, corals, or sea creatures preserved within the rock provide direct evidence of its marine origin. Additionally, the presence of ripple marks or cross-bedding in the limestone can also indicate its formation in a marine environment.
ripple
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.
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.
Dark fringes are formed where destructive interference occurs, canceling out waves and creating areas of low intensity. Bright fringes are formed where constructive interference occurs, combining waves and creating areas of high intensity. These alternating fringes are a result of the superposition of waves in the ripple tank.
Ripple marks in sedimentary rock were emplaced in sediments by near shore wave action, covered by additional sediments, and eventually lithified into a solid rock which becomes exposed by weathering and erosion of overlying material over large expanses of time.
Ripple voltage, in the presence of a filter capacitor, is inversely proportional to load resistance. If the load were zero (resistance infinite), then there would be no ripple voltage. As the load increases (resistance decreases), the ripple voltage increases. The ripple waveform will appear to be sawtooth, with the rising edge following the input AC from the diode's conductioin cycle, and with the falling edge either being linear or logarithmic, depending on load. If the load is resistive, without a regulator, the falling edge will be logarithmic. If the load is constant current, such as with a regulator, the falling edge will be linear.
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.