Unit 3 Flashcards
Identify the evidence for continental drift
the fit of the continents; the distribution of ancient fossils, rocks, and mountain ranges; and the locations of ancient climatic zones.
an undersea mountain chain where new ocean floor is produced at a divergent plate boundary.
Mid- ocean ridge
Sea-floor spreading
The process of molten material from the mantle being pushed upward to the surface of the earth and spreading apart creating new earth
Paleomagnetism
the study of changes in Earth’s magnetic field, as shown by patterns of magnetism in rocks that have formed over time.
Plate tectonics
the idea or theory that the earth’s crust is made of large chunks of land, or plates, that move over time
Lithosphere
layer of the Earth made up of the crust and the rigid part of the upper mantle.
Asthenosphere
The zone of the mantle beneath the lithosphere that consists of slowly flowing solid rock.
Divergent plate boundaries
A tectonic boundary where two plates are moving away from each other and new crust is forming from magma that rises to the Earth’s surface between the two plates.
Convergent boundary
he boundary between two colliding plates.
Continental-continental boundary
Occurs where two plates carrying continental crust push together.
Oceanic- oceanic boundary
When two plates collide one is bent and slides down into the asthenosphere where it melts
Oceanic-continental boundary
Deep Ocean Trenches, Islands Arcs, Earthquakes and Volcanoes occur at this boundary. Oceanic- Continental Convergent Plate Boundary. Occurs when an oceanic and a continental plate collide. The oceanic crust will sub duct because it is older, colder, and denser than the continental crust.
transform
create. earthquakes. A transform fault is. contact between two plates that slide horizontally past one another, commonly connecting two mid-oceanic ridges.
Rifting
A linear belt along which continental lithosphere stretches and pulls apart.
Terrane
a slice of lithosphere that has been added to the margin of a continent during plate collision.
Supercontinent cycle
the quasi-periodic aggregation and dispersal of Earth’s continental crust. There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth’s crust is constantly being reconfigured.
Panthalassa
the global ocean that surrounded pangea.
Deformation
Change in shape and/or volume of rocks in response to stress.
Isostasy
constant balancing between the downward force of the crust and the upward force of the mantle
stress
the force applied to an object. Stresses can be confining, compression, tension, or shear. Rocks under stress may show strain or deformation. Deformation can be elastic or plastic, or the rock may fracture.
Strain
Deformation resulting from stress. Deformation. Change in shape or volume of a rock in response to stress.
Fold
the process by which the strata of rocks bend to form arches (anticlines) and troughs (synclines) as a result of compression within the earth’s crust.
Anticline
An anticline is a fold that arches upward. The rocks dip away from the center of the fold. The oldest rocks are at the center of an anticline and the youngest are draped over them.
Syncline
A downward fold in rock formed by compression in Earth’s crust.