The deepest point of the Silfra underwater canyon plunges 63 meters (about 206 feet), though this depth is only accessible to highly experienced divers.

The deepest point of the Silfra underwater canyon plunges 63 meters (about 206 feet), though this depth is only accessible to highly experienced divers.

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These cootie catchers are a great way for students to have fun while learning about plate tectonics and earthquakes. There are two versions which contain the following vocabulary terms:   ♦ Convergent boundary, Divergent boundary, Transform boundary, Subduction zone, Fault, Convection current, Hot spot, Tectonic plate                                                                And ♦ Earthquake, Seismic wave, Magnitude, Epicenter, Seismologist, Seismograph, Continental drift, Pangaea

These cootie catchers are a great way for students to have fun while learning about plate tectonics and earthquakes. There are two versions which contain the following vocabulary terms: ♦ Convergent boundary, Divergent boundary, Transform boundary, Subduction zone, Fault, Convection current, Hot spot, Tectonic plate And ♦ Earthquake, Seismic wave, Magnitude, Epicenter, Seismologist, Seismograph, Continental drift, Pangaea

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Divergent oceanic boundary

Divergent oceanic boundary

Teaching plate tectonics! Divergent boundary: cut slit in cardboard and pull out the "oceanic crust" that is being created at the mid- ocean ridge

Teaching plate tectonics! Divergent boundary: cut slit in cardboard and pull out the "oceanic crust" that is being created at the mid- ocean ridge

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Divergent Boundary Model

Divergent Boundary Model

In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts which produce rift valleys. Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the…

In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts which produce rift valleys. Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the…

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