module 4: geology Flashcards
A dynamic planet and constantly changing structure.
A layered sphere.
Earth
interior, is composed of a dense, intensely hot mass of metal, mostly iron, thousands of kilometers in diameter.
Core
surrounding the molten outer core. It is a hot, pliable layer of rock.
Mantle
the cool, lightweight, brittle rock outermost layer of the earth
Crust
publish a sketch showing how the two continents could fit together, jigsaw-puzzle fashion.
Antonio Snider
Climatologist, was struck not only by the matching coastlines, but by geologic evidence from the continents.
Alfred Wegener
may preserve evidence of the ancient climate of the time and place in which the sediments were deposited.
Sedimentary rocks
There are evidences of extensive glaciation in places now located in the tropics
parts of Australia, southern Africa, and South America.
There are coal deposits
Antarctica
fossil plant, remains of which are found in limited areas of widely separated lands
Glossopteris
fossils of a small reptile, similarly dispersed across two continents.
Mesosaurus
the modern continents moving to their present positions via a process
continental drift
study of large scale movement and deformation of the earth’s outer layers
Tectonics
such deformation to the existence and movement of rigid “plates” over a weaker, more plastic layer in the earth’s upper mantle
Plate tectonics
The earth’s crust and uppermost mantle are somewhat brittle and elastic
Lithosphere
meaning “without strength”,
Its lack of strength or rigidity results from a combination of high temperatures and moderate confining pressures that allows the rock to flow plastically under stress.
Asthenosphere
The distribution of earthquakes and volcanic eruptions indicates that these phenomena are far from uniformly distributed over the earth.
Locating Plate Boundaries
lithospheric plates MOVE APART
Divergent plate boundary
most common type of divergent boundary worldwide, and it is already noted the formation of new oceanic lithosphere at these ridges.
SEAFLOOR SPREADING RIDGES
plates are MOVING TOWARD EACH OTHER
Convergent plate boundary
This type of plate boundary, where one plate is carried down below (subducted beneath) another
subduction zone
At an ocean-ocean convergence, the result is commonly a line of volcanic islands
island arc
are frequent during continent-continent collision as a consequence of the large stresses involved in the process
Earthquakes
ridges consist of many short segments slightly OFFSET from one another
Transform Boundaries
The offset is a special kind of fault, or break in the lithosphere
transform fault
naturally occurring, inorganic, solid element or compound with a definite chemical composition and a regular internal crystal structure
mineral
not produced solely by living organisms or by biological processes
Inorganic