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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.
Ocean crust is typically denser than continental crust because it contains more basalt (rich in iron and magnesium), whereas continental crust is composed of less dense granite (richer in aluminum and silicon).
The oceanic crust is mostly composed of basalt, while the continental crust is primarily made up of granite. Both types of crust contain some amount of silica-rich minerals like feldspar and quartz.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
The Grand Banks off the coast of Newfoundland in Canada is a famous continental shelf known for its rich marine life and historically significant fishing grounds.
The ocean floor can be described in terms of three primary features: the continental shelf, continental slope, and continental margin. The continental shelf is the shallow, submerged extension of the land, where the ocean is relatively shallow and rich in marine life. Beyond the shelf, the continental slope descends steeply to the deep ocean floor, marking the transition from the shallow coastal waters to the deep sea. The continental margin encompasses both the shelf and slope, forming the boundary between the continental crust and the oceanic crust.
Most ocean life is found on the continental shelf, which is the shallow area of the ocean extending from the coastline to the continental slope. This region is rich in nutrients and sunlight, supporting diverse ecosystems, including coral reefs and various fish species. In contrast, the continental slope and ocean deep are less productive due to lower light availability and fewer nutrients. Thus, the continental shelf is the most biologically productive area of the ocean.
The underwater edge of a continent is called the continental shelf. It is the shallow, submerged extension of a continent that extends from the shoreline to the continental slope. The continental shelf is rich in marine life and is important for fishing and oil exploration.
The Grand Banks is a continental shelf, specifically located off the southeast coast of Newfoundland, Canada. This underwater feature extends over a large area with relatively shallow waters, making it rich in marine life and an important fishing ground. The continental shelf is characterized by its gradual incline, contrasting with the steeper continental slope that lies beyond it.
The continental slope is crucial for several reasons. It serves as a transitional zone between the shallow waters of the continental shelf and the deep ocean, playing a key role in marine ecosystems and biodiversity. Additionally, it is rich in resources such as oil, gas, and minerals, making it significant for economic activities like fishing and energy exploration. Furthermore, the slope influences ocean currents and sediment transport, impacting climate and marine life.
Rich Fields's birth name is Richard Wayne Fields.
The continental shelf is a gently sloping, shallow underwater edge of a continent that extends from the shoreline to a steeper drop-off called the continental slope. It is an important part of the ocean ecosystem and is rich in marine life. Oil, gas, and mineral resources can also be found on the continental shelf.
Rich Fields was born on November 30, 1960.
Rich Fields was born on November 30, 1960.
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.
The area where water becomes gradually deeper is known as the continental shelf. This submerged landmass extends from the coastline out to the continental slope, where the seabed begins to steepen more sharply. The continental shelf is typically characterized by relatively shallow waters and is rich in marine life and resources.
This region is known as the continental shelf. It is a gently sloping area of land between the shoreline and the deep ocean. The continental shelf is rich in marine life and is an important area for commercial fishing and oil exploration.