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The gently sloping margins of a continent submerged beneath the sea?
The gently sloping margins of a continent submerged beneath the sea are known as continental shelves. These areas are shallow and extend from the shoreline to the continental slope. Continental shelves are important for marine life as they provide a nutrient-rich environment for various species.
What do scientist call the areas of Earth's crust a.faults b.hemisphere c.tectonic plates d. continental shelves?
continental shelves
What is the term for the areas of continents that extend out into ocean water?
The term for the areas of continents that extend out into ocean water is "continental shelf." These regions are submerged and typically feature shallow waters, providing rich ecosystems and significant marine resources. Continental shelves can vary in width and depth, and they play a crucial role in marine navigation and fisheries.
How the continental shelves developed?
The continental shelves were developed in between the glacial periods as the ocean flowed over the continents forming shallow areas along the coasts. The continental shelves developed today were formed like 18000 years ago.
Why are continental shelves the areas of the ocean richest in marine life?
There are many conditions that leave continental shelves the richest area in the ocean for marine life. The biggest factor is the shallow depth of the waters where the continental shelves lay. The constant temperature of these shelves also aid in steady marine life.
What is a submerged land at the edge of a continent called?
Continental Shelves
What processes are responsible for the formation and sculpting of continental shelves?
Continental shelves are primarily formed through a combination of tectonic processes, sediment deposition, and sea-level changes. Tectonic activity can uplift or subside continental margins, while sediment from rivers and coastal erosion accumulates on these shelves. Additionally, during periods of glaciation, lower sea levels expose more of the continental shelf, and as glaciers melt, rising sea levels reshape and inundate these areas. Over time, marine processes such as wave action and currents further sculpt the shelf's features.
What is the continental?
Composed mostly of granite, the continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents and the areas of shallow seabed close to their shores, known as continental shelves
How do continental shelves form?
The continental shelves were developed in between the glacial periods as the ocean flowed over the continents forming shallow areas along the coasts. The continental shelves developed today were formed like 18000 years ago.
What is the crust's continental crust?
Composed mostly of granite, the continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents and the areas of shallow seabed close to their shores, known as continental shelves
What are the three main surface features located in the oceans?
The three main surface features located in the oceans are continental shelves, oceanic ridges, and abyssal plains. Continental shelves are shallow areas adjacent to coastlines, rich in marine life. Oceanic ridges are underwater mountain ranges formed by tectonic activity, while abyssal plains are flat, deep ocean floor regions that cover a significant portion of the ocean's surface. These features play crucial roles in marine ecosystems and oceanic processes.
Were do the thickest deposits of terrigenous sediment typically form?
The thickest deposits of terrigenous sediment typically form in areas close to continental margins, where there is a high input of sediment from rivers, glaciers, and wind. These areas can include continental shelves, slopes, and fans.
