Margin

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Margin may refer to:

Contents

Physical or graphical edges

Economics and finance

Figurative edges

Other uses

See also

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Drift or Drifts may refer to:

Choke may refer to:

Obduction is a geological process whereby denser oceanic crust is scraped off a descending ocean plate at a convergent plate boundary and thrust on top of an adjacent plate. When oceanic and continental plates converge, normally the denser oceanic crust sinks under the continental crust in the process of subduction. Obduction, which is less common, normally occurs in plate collisions at orogenic belts or back-arc basins.

Sorcerer may refer to:

A sneaker is a type of shoe originally designed for athletics.

Marginal may refer to:

Kim or KIM may refer to:

The apex is the highest point of something. The word may also refer to:

Private or privates may refer to:

Cob or COB may refer to:

Wishbone commonly refers to Furcula, a fork-shaped bone in birds and some dinosaurs

An earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves.

Frequency refers to how often an event occurs within a given period.

Democracy is a political concept or form of government.

In hydrology, an oceanic basin (or ocean basin) is anywhere on Earth that is covered by seawater. Geologically, most of the ocean basins are large geologic basins that are below sea level.

Variation or Variations may refer to:

An image is an artifact that depicts visual perception, such as a photograph or other two-dimensional picture.

IS may refer to:

Volcanic passive margins (VPM) and non-volcanic passive margins are the two forms of transitional crust that lie beneath passive continental margins that occur on Earth as the result of the formation of ocean basins via continental rifting. Initiation of igneous processes associated with volcanic passive margins occurs before and/or during the rifting process depending on the cause of rifting. There are two accepted models for VPM formation: hotspots/mantle plumes and slab pull. Both result in large, quick lava flows over a relatively short period of geologic time. VPM's progress further as cooling and subsidence begins as the margins give way to formation of normal oceanic crust from the widening rifts.

A continent is a large landmass.