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Divergent Boundary Drawing

Divergent Boundary Drawing - This illustration is from wikipedia and may be freely used. Transform fault (arrows show relative motion) hot spot (arrow = direction of plate motion) great earthquakes since 1900; Divergent boundaries come in two principal varieties that are relevant to historical geology: Web at divergent boundaries where tectonic plates move apart, there will be upwelling material from the mantle to create new seafloor. White arrows show plate motion direction. This occurs above rising convection currents. Web another kind of plate movement is called a divergent boundary. Along these boundaries, earthquakes are common and magma (molten rock) rises from the earth’s mantle to the surface, solidifying to create new oceanic crust. As shown in the drawing above, when earth's brittle surface layer (the lithosphere) is pulled apart, it typically breaks along parallel faults that tilt slightly outward from each other. Web places where plates are coming apart are called divergent boundaries.

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So This Right Here Is The Earth's Crust.

Web now, with that out of the way, let's draw a little diagram of what happens in the early stages of these divergent plate boundaries. Transform fault (arrows show relative motion) hot spot (arrow = direction of plate motion) great earthquakes since 1900; Web at divergent boundaries, sometimes called constructive boundaries, lithospheric plates move away from each other. There are two types of divergent boundaries, categorized by where they occur:

Web At Divergent Boundaries Where Tectonic Plates Move Apart, There Will Be Upwelling Material From The Mantle To Create New Seafloor.

Convergent boundaries occur where two plates are moving toward each other. Web a divergent boundary occurs when two tectonic plates move away from each other. Divergent boundaries come in two principal varieties that are relevant to historical geology: Introduction to teaching plate tectonics.

Web Where Can You See Divergent Boundaries?

This occurs above rising convection currents. The eurasian plate rotates clockwise. Plate boundaries can be categorized in three fundamental types: Web divergent plate boundaries are locations where tensional forces are pulling things apart.

In Locations Where Lithospheric Plates Are Diverging, The Rates Of Divergent Motion Range From 2 To 17 Cm/Year.

In this extensional setting, normal faulting dominates, thinning the crust vertically while stretching it out laterally. Web divergent plate boundaries are locations where plates are moving away from one another. Write a compare and contrast essay describing the type of surface features found at each plate boundary. Along these boundaries, mountains and trenches are common.

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