Mod+2+-+Trinity+G

**Convergent Boundries** = =

When plates serving landmasses collide, the crust crumples and buckles into mountain ranges. India and Asia crashed about fifty-five million years ago, slowly giving rise to the Himilaya's, the higheset mountain system on Earth. They grow each day. A plate of ocean dives, called subcation as the over-lying plates life up, it form mountain ranges. The diving plate melts is often spewed out in a volcanic eruption. At ocean-ocean convergent, one plate usually dives beneath the other, forming deep trenches under the water. some of my examples were: **Divergent Boundries**
 * http://science.nationalgeographic.com/science/earth/the-dynamic-earth/plate-techtonic-article.html
 * http;//geology.com/nsta/convergentplate-boundries.html//
 * 1) anoles mountain range is the volcanones above melting plate
 * 2) the himilaya mountains
 * 3) the marina trench

magma from deep in earths mantle rises tword the surface and pushes apart two or more plates. mountains and volcanoes rise along the seam, this renews the ovean floor and widens the giant basins and makes the ridge the longest mountain range. The great Rift Valley in africa form where plates are tugged apart. ridge is a high area compared to surrounding seafloor. = =

some of my examples were:
 * http://science.nationalgeographic.com/science/earth/the-dynamic-earth/plate-techtonic-article.html
 * http;geology.com/nsta/divergentplate-boundries.html
 * 1) The great Rift Valley
 * 2) mid atlantic ridge
 * 3) ocean floor

**Transform Boundries**

where two plates grind past each other along what are called strike-slip faults. These boundries don't produce spectacular features lik mountains or oceans, the haulting motion often triggers earthquakes like the once in sanfrancisco. (devestrated it) some of my examples were:
 * http://science.nationalgeographic.com/science/earth/the-dynamic-earth/plate-techtonic-article.html
 * http;//geology.com/nsta/transformplate-boundries.html
 * 1) san francisco
 * 2) mountains
 * 3) things grinding

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