The Lithosphere and Tectonic System Flashcards
he theory describing the changing configuration of the continents through time is called
plate tectonics
________________y maintains that the Earth’s outermost solid layer consists of huge, rigid plates that float on a layer of plastic rock. These plates are in slow, constant motion, powered by energy sources deep within the planet. When two plates come together, one may be forced under the other in a process calle________________
plate tectonic theory – subduction
The Earth is an almost spherical body, approximately ___ in radius
6,400 km
The centre of the Earth is occupied by the ___, which is about 3,500 km in radius (two zones: the outer core which has the properties of a liquid; the inner core is solid
core
Even though temperature _____toward the Earth’s centre, the inner core remains solid because ____
increases —— it is under very high pressure
Enclosing the metallic core is the ______, a rock shell about 2,900 km thick, which accounts for about 50 percent of the Earth’s mass. Seismic data indicate that mantle rock is composed of magnesium and iron silicates similar to the ultramaficigneous rock peridotite. Temperatures in the mantle range from about 2,800 °C near the core to about 1,800 °C near the crust, and are maintained by the release of energy through radioactive decay of uranium, thorium, and potassium isotopes.
mantle
The outermost and thinnest of the Earth’s layers is the
crust. It is formed mainly of igneous rock, but also contains substantial proportions of metamorphic rock and a comparatively thin upper layer of sedimentary rock.
Two crustal types are distinguished:
Oceanic crust, which accounts for about 0.1 percent of Earth’s mass, can be up to 10 km thick under the oceans, but is absent beneath the continents. Continental crustaccounts for about 0.4 percent of Earth’s mass and is present only in continental areas where it is generally 30 to 40 km in thickness
lithosphere
a zone of rigid, brittle rock, includes not only the crust, but also the cooler, upper part of the mantle (ranges in thickness from 60 to 150 km, and is thickest under the continents – consisting of lithospheric plates)
athenosphere
Deep within the Earth, the brittle condition of the lithospheric rock gives way gradually to a plastic layer named the asthenosphere, where temperatures reach 1,400 °C (density increases from 3.7 to 5.5 gcm-3 with depth).
The solid Earth originated some 4,600 million years ago. This long period of time can be considered in two different ways from a geological perspective.
he chronostraticapproach to geological time is based on the relative age of rock types and events, and uses fossil assemblages and an idealized set of sedimentary rock strata as its reference. The chronometric approach establishes the absolute age of earth materials from radiometric and other dating methods
Continents can be subdivided into two basic region
active belts where mountain-building processes are still occurring and shield areas composed of old, stable rock. The mountain ranges in the active belts grow either through volcanism or by tectonic activity.
Volcanism can result in massive accumulations of volcanic rock by extrusion of magma, as seen in the Cascade Mountains of western North America. Tectonic activityinvolves the breaking, bending, and upthrusting of the Earth’s crust due to internal forces associated with the collision of the lithosphericplates.
Continental shields
are low-lying continental surfaces, beneath which are complex arrangements of ancient igneous and metamorphic rocks. Some core areas of the shields are composed of rocks dating back to the Archean Eon, 2,500 to 3,800 million years ago
The deepest parts of ocean basins are the_______
e ocean trenches that mark the positions of subduction arcs where oceanic crust is being forced down into the mantle. Of the 22 ocean trenches that have been located, 18 are in the Pacific Ocean, three are in the Atlantic Ocean, and one is in the Indian Ocean. The deepest is the Mariana Trench in the Pacific Ocean, about midway between Indonesia and Japan; it is 2,540 km in length, descends to 11,033 m, and is 69 km in width
The major relief feature of ocean basins is a central ridge, which in the case of the Atlantic Ocean divides the basin approximately in hal
his mid-oceanic ridge consists of submarine hills that rise gradually to a rugged central zone. In the centre of the ridge is a narrow, elongated depression known as the axial rift. The location and form of the axial rift suggest that this is a region where the crust is being pulled apart (the age of the rocks on both sides of the ridge increases symmetrically with distance from the rift).