tidal hypothesis
The hypothesis that states that continents slowly moved to their present-day positions on Earth is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century, suggesting that continents were once part of a single supercontinent called Pangaea and have since drifted apart.
Continental drift plays a role in erosion by influencing the distribution of landmasses and the formation of topographic features. As continents move, they can create new mountain ranges, change the direction of river flow, and alter the patterns of erosion and sediment transport. These changes in topography can impact erosion rates and shape landscapes over long periods of time.
The shape of a continental shelf is mainly controlled by past and present geological processes, such as erosion, sedimentation, and tectonic activity. Sea level changes and climatic conditions can also influence the shape of a continental shelf by impacting erosion and sedimentation rates.
Erosion happens constantly everywhere, from mountains to seashores. Although I would imagine that the greatest amount of erosion would occur in water, so perhaps anywhere from a near shore enviroment down to the continental slope/abyssal plain.
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
The hypothesis that states that continents slowly moved to their present-day positions on Earth is called continental drift. This theory was proposed by Alfred Wegener in the early 20th century, suggesting that continents were once part of a single supercontinent called Pangaea and have since drifted apart.
Continental drift plays a role in erosion by influencing the distribution of landmasses and the formation of topographic features. As continents move, they can create new mountain ranges, change the direction of river flow, and alter the patterns of erosion and sediment transport. These changes in topography can impact erosion rates and shape landscapes over long periods of time.
The shape of a continental shelf is mainly controlled by past and present geological processes, such as erosion, sedimentation, and tectonic activity. Sea level changes and climatic conditions can also influence the shape of a continental shelf by impacting erosion and sedimentation rates.
Continental Erosion
Erosion and sediments from large rivers.
because of erosion over time.
A continental coast is the boundary where a continent meets the ocean. It typically includes a variety of landforms such as cliffs, beaches, and headlands. Continental coasts are subject to processes like erosion, sediment transport, and tectonic activity.
A hypothesis is any idea used to explain and test a scientific idea, while a theory is a hypothesis that has become scientifically accepted. For example, say I hypothesize that rocks in a stream are worn smooth by erosion. This is a hypothesis of sorts. I test this hypothesis by putting rocks in a room and in a stream, and conclude that the stream rocks have been worn smooth. If I complete multiple tests and the scientific community believes in my conclusion, I would call it the Theory of Water Erosion, or something similar.
Erosion happens constantly everywhere, from mountains to seashores. Although I would imagine that the greatest amount of erosion would occur in water, so perhaps anywhere from a near shore enviroment down to the continental slope/abyssal plain.
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
The shape of the continental slope is primarily controlled by gravitational forces, erosion by currents and waves, and tectonic processes such as subsidence and uplift. These forces work together to shape the steep boundary between the continental shelf and the deep ocean floor.
During continental drift, the Pangaea broke into, 2 parts: Gondwana land and Laurasia, they drifted apart and were raised up to form Continental plateaus. Eg: Canandian Shield, Deccan Plt, Plt of West Africa. Soham_Patha Bhavan