The margin of a continent is determined by the location of its tectonic plate boundaries. Convergent boundaries create subduction zones or mountain ranges, while divergent boundaries form rift valleys or mid-ocean ridges along the margins. Transform boundaries can also influence the shape of a continent's margin by creating strike-slip faults.
A continental margin is the zone of transition between a continent and the deep ocean floor. It includes the continental shelf, continental slope, and continental rise. It is an area where sediments from the continent are deposited and tectonic activity can occur.
Technically, a continent is an island. Nonetheless, Australia is a continent.
AnswerThe largest continent is Asia
The European continent.
Continent is a noun.
The confidence interval radius determines the margin of error. If you want more information visit: http://en.wikipedia.org/wiki/Margin_of_error
The leaf margin is the outermost boundry line of the leaf lamena. It determines the shape of the leaf.
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
oceanic crust
Part of the continent that sticks out of the ocean and oit is very active
A continental margin is the zone of transition between a continent and the deep ocean floor. It includes the continental shelf, continental slope, and continental rise. It is an area where sediments from the continent are deposited and tectonic activity can occur.
Contribution margin ratio determines the percentage of variable cost in over all sales while contribution margin per unit tells the variable cost portion in per unit total cost or sales price.
Wordwrap
The continental margin is the zone of ocean floor that separates oceanic crust and continental crust. It accounts for 28% of all oceanic area.
Britain is not located on a destructive plate margin and the ring of fire is an ocean and a continent away.
The continental margin is the submerged outer edge of a continent. It is generally divided into two sections: the continental shelf and the continental slope.
A geosyncline is a belt of sedimentary deposits that accumulate within the ocean along the margin of a continent - on the continental shelf and slope.