Term |
Definition |
Platter tectonics |
the idea that Earths outer part is made up of large, moving bits called tectonic plates, the idea explains how plates interact and how those interactions connect with processes including earthquakes and mountain building |
Crustal features |
include those expressed around the surface, (such as mountains, rivers, and lakes) and those less visible (such as scenic feed water lines, earthquake mistake lines, Geological formations, and aquifer formations. ) |
Tectonic plates |
a block of lithosphere that consists of the crust as well as the rigid, outermost part of the layer |
Oceanic crust |
the relatively thin part of the earths brown crust area that underlies the water basins. It is geologically fresh compared with the continental crust and includes basaltic ordinary overlain simply by sediments. |
Continental crust |
may be the layer of igneous, sedimentary, and metamorphic rocks that forms the continents as well as the areas of shallow seabed close to their shores, known as continental shelves. |
Scenic island |
can be an isle that was performed from volcanoes erupting from your ocean floor. |
Pile range |
a line of mountain range connected by high earth. |
Subduction zone |
is the biggest crash scene on Earth. These kinds of boundaries tag the accident between a pair of the planets tectonic discs. The china are items of crust that slowly approach across the planets surface over millions of years. |
Earthquake |
is the apreciable shaking in the surface of the Earth, resulting from the sudden release of energy in the Earths crust that creates seismic waves. |
Converging plates |
form when 2 or more plates move to each other within a collision zone. |
Transform problem boundary |
a strike-slip problem that offsets a mid-ocean ridge in opposing directions on both side associated with an axis of seafloor distributing. |
Folded mountains |
are set up where two or more of Earth’s tectonic discs are pressed together, generally at regions known as convergent plate restrictions and continental collision areas and specific zones. |
Divergent border |
A tectonic boundary in which two discs are getting off each other and new brown crust area is forming from magma that goes up to the Earths surface between the two plates. |
Subduction boundary |
A geologic process in which one advantage of one crustal plate is definitely forced under the edge of another. |
Convergent boundary |
is an definitely deforming area where two (or more) tectonic discs or broken phrases of the lithosphere move toward one another and collide. |
Mid-ocean ridge |
is definitely an underwater mountain system formed by simply plate tectonics. It consists of various mountain range linked in chains, commonly having a area known as a rift running along its spine. |