False, continental shelves are part of the Coastal Plain
The bottom of the ocean is part of a tectonic plate or continental shelf, or can be on the breach line between two shelves.
Because for the most part, the continental shelves are where the fish are.
Continental Shelf.
The continental shelf typically has the most shallow water on the ocean floor. This is the submerged edge of a continent that extends from the shoreline to a steeper drop-off point called the continental slope. The shallow waters of the continental shelf are important for marine life and are commonly where coastal communities are located.
The part of the ocean floor nearest the continents is called the continental shelf. It is a gently sloping, submerged platform that extends from the shoreline to the continental slope. The continental shelf is important for marine life as it provides a shallow and productive area for various organisms to thrive.
Abyssal plain is a land feature similar to the continental slope, located at the base of the continental rise. It is a flat area of the ocean floor covered with sediment and is considered the most level part of the ocean floor.
The term for the part of a continent that extends beyond the shoreline beneath relatively shallow seawater is the continental shelf. It is an underwater extension of the continent that slopes gently from the shore to the ocean depths.
The richest deposits of oil and gas are often found on continental shelves because these areas were once part of landmasses, where organic material accumulated over millions of years. As the land submerged, this organic material was buried and transformed into oil and gas through geologic processes. The sedimentary conditions and structural features on continental shelves make them ideal for the formation and trapping of oil and gas deposits.
The part on where the continental shelf meets the continental slope creating an edge.
I'm Not Really Sure What You Mean By 'Their Stores' Or 'Their Shelves' But The Are On The Shelves
Continental shelves are submerged underwater extensions of the continent, and they match up because they were once part of the same landmass before sea levels rose. Shorelines may not match due to various factors like erosion, tectonic activity, and changes in sea level over millions of years causing the coastlines to shift and change.
The continental shelf layer is called the shelf break. It is the steepest part of the continental shelf where the seafloor drops off sharply towards the deeper ocean floor.