The continental shelf is the term for part of a continent that extends outward from the landmass beneath shallow seawater. The drop-off point of a continental shelf is called the shelf break. From this point, the continental goes down to the deep ocean floor.
The term "plateau" in "continental shelf" refers to the relatively flat and gently sloping underwater landform that extends from the coastline to the continental slope. Continental shelves are essentially submerged plateaus, characterized by their shallow depth compared to the surrounding ocean floor. This geological feature supports diverse marine ecosystems and is significant for fishing and natural resource exploration.
The continental shelf is the extended perimeter of each continent and associated coastal plain, and was part of the continent during the glacial periods, but is undersea during interglacial periods such as the current epoch by relatively shallow seas (known as shelf seas) and gulfs. The continental rise is below the slope, but landward of the abyssal plains. Its gradient is intermediate between the slope and the shelf, on the order of 0.5-1°. Extending as far as 500 km from the slope, it consists of thick sediments deposited by turbidity currents from the shelf and slope. Sediment cascades down the slope and accumulates as a pile of sediment at the base of the slope, called the continental rise. Under the United Nations Convention on the Law of the Sea, the term continental shelf was given a legal definition as the stretch of the seabed adjacent to the shores of a particular country to which it belongs. See the Territorial waters page for more details.
Differentiate term by term. d/dx[X2 + 2X) = 2X + 2 slope(m) = 2 ------------------
the slope is 2, the number in front of the 'x' term
The other term for slope is gradient
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.
3x + y - 4 = 0 y = -3x + 4 The slope is equivalent to the coefficient term of 'x', also known as 'm'. Therefore, the slope is -3.
The equation y = mx + c, is the equation of a line in slope-intercept form. The m term is the slope or first order deriviative (dy/dx) of the line, and the c term is the y-axis intercept.
solve each equation in terms of y and the slope is the value in front of the x term; the slope of one of them is the negative inverse slope of the other p/q = 3/2
Yes, the slope of a line is the coefficient of the x-term in the line.
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.