Ch. 3 Key Terms Flashcards
geosphere
The solid part of Earth that consists of all rock, as well as the soils and loose rocks on Earth’s surface
hydrosphere
all of the water on or near Earth’s surface.
crust
composed almost entirely of light elements. The crust makes up less than 1 percent of Earth’s mass.The crust is Earth’s thinnest layer.
mantle
the layer beneath the crust, makes up 68 percent of the mass of Earth. The mantle is approximately 2,900 km thick and is made of rocks of medium density.
core
Earth’s innermost layer is the core. The core, which has a radius of approximately 3,400 km, is composed of the elements having the greatest density.
lithosphere
Earth’s outer layer is the lithosphere. It is a cool, rigid layer, 15 km to 300 km thick, that includes the crust and uppermost part of the mantle.
asthenosphere
the layer beneath the lithosphere. The asthenosphere is a pliable, solid layer of the mantle made of rock that flows very slowly and allows tectonic plates to move on top of it.
tectonic plate
The lithosphere is divided into pieces called tectonic plates that glide across the underlying asthenosphere in much the same way a chunk of ice drifts across a pond. The continents are located on the tectonic plates and slowly, over eons, move around with them. The major plates include the Pacific, North American, South American, African, Eurasian, andAntarctic plates.
chemical warning
wears down rocks, making them smoother as time passes
erosion
transports the materials elsewhere
atmosphere
Earth is surrounded by a mixture of gases known as the atmosphere. Nitrogen, oxygen, carbon dioxide, and other gases are all parts of this mixture. Earth’s atmosphere changes constantly as these gases are added and removed.
troposphere
The atmospheric layer nearest Earth’s surface is the troposphere. The troposphere extends to about 18 km above Earth’s surface. Almost all of the weather occurs in this layer. The troposphere is Earth’s densest atmospheric layer.
stratosphere
Above the troposphere is the stratosphere. The stratosphere, separated from the troposphere by the tropopause, shown in Figure 2.3, extends from about 18 km to an altitude of about 50 km. Temperatures rise as altitude increases because ozone in the stratosphere absorbs the sun’s ultraviolet(UV) energy and warms the air.
ozone
O3, is a molecule made up of three oxygen atoms. Almost all the ozone in the atmosphere is concentrated in the ozone layer in the stratosphere. Ozone reduces the amount of harmful UV radiation that reaches Earth.
radiation
the transfer of energy as electromagnetic waves. When you stand before a fire or a bed of coals, the warmth you feel has reached you by radiation.