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What else can I help you with?
Does the gulf stream flow over the continental shelf or the continental slope?
continental shelf
A deep ditch carved over by running water?
It's a gully. Rills are smaller ditches cut by running water, but can be plowed over. Once the ditch is so deep it can't be plowed over, it's a gully.
What are the driving forces of continental drift?
The driving Forces of Continental drift are both gravity and the motion of the underground Tectonic Plates.
In the 1930s the theory of continental drift was formed?
The theory of continental drift did originate in the 1930s. Continental drift asserts that the continents were once a single landmass called Pangaea that drifted apart over time.
Why do we have a water cycle?
to recycle the water over and over again.
Region of shallow ocean water over the continental shelf?
neritic
Does the gulf stream flow over the continental shelf or the continental slope?
continental shelf
What are the Rights in the continental shelf?
A continental shelf is an area where a country has some exclusive rights i e exploration of natural resources ,it can construct structures , it has also sovereignty over the water body.Other country only can cruse through without permission of concern country.It constitutes at the beginning of the sea up to the 350 km and it goes until the shelf drifts to deep bottom of sea.Hossain
What zone is a region of shallow water below the low-tide line that extends over the continental shelf?
sublittoral
What is below the low-tide line and out over the continental shelf?
neritic zone
What is Distance from shore zone that is over the continental shelf?
Neritic Zone
What causes a continental slope?
A continental slope is formed by the transition between the continental shelf and the deep ocean floor, characterized by a steep incline. It is primarily caused by geological processes such as erosion, sediment deposition, and tectonic activity, including the movement of tectonic plates. Over time, sediment from the continental shelf is transported down the slope due to gravity and underwater currents, contributing to its formation. Additionally, sea-level changes and glacial activity can also influence the morphology of the continental slope.
Is the grand banks a continental shelf or continental slope?
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.
What has the author Ken Brink written?
Ken Brink has written: 'Programs for computing properties of coastal-trapped waves and wind-driven motions over the continental shelf and slope' -- subject(s): Continental slopes, Computer programs, Continental shelf, Ocean waves
What would happen to the continental shelf if the water level drops dramatically?
If the water level drops dramatically, the continental shelf would become exposed, revealing land that is typically submerged. This could lead to significant ecological changes, as marine habitats would transition to terrestrial environments, impacting the species that rely on these habitats. Additionally, the reduction in water would likely alter sediment distribution and coastal processes, potentially affecting human activities such as fishing and shipping. Over time, the exposed continental shelf could become a new landscape for terrestrial ecosystems to develop.
What is the most common way that material is added to a continental shelf?
The most common way material is added to a continental shelf is through sedimentary processes, primarily from rivers and coastal erosion. Rivers transport sediments from land, depositing them into the ocean as they reach the continental shelf. Additionally, coastal erosion contributes sediments from shorelines, while marine organisms also contribute biological material. These processes collectively build up the sediment layers on the continental shelf over time.
Are ice or icebergs associated with the continental shelf?
Icebergs are not typically associated with the continental shelf; they originate from glaciers or ice sheets that calve into the ocean, usually from land-based ice formations. However, sea ice can form over the continental shelf in polar regions, particularly during winter months. This sea ice is different from icebergs, as it forms from the freezing of seawater rather than from freshwater glaciers. Thus, while sea ice can be linked to the continental shelf, icebergs are generally not.
