Chapter 12 - Earth History, Earth Interior Flashcards
crust
rigid outermost layer of Earth
volcano
mountain or hill formed by eruptions of lava and rock fragments
cyanobacteria
photosynthetic bacteria
unifortarianism
the principle that the same gradual and nearly imperceptible processes operating now have operated in the past
relative age
compares the age of one object or event with the age of another, without specifying how old either object is
absolute age
age of an object specified in years before the present
superposition principle
states that in a sequence of rock layers, the oldest rocks are at the bottom and the younger rocks are on top
radiometric dating
a method of calculating absolute age that involves using unstable atoms in materials to assign ages to those materials
seismic waves
energy released by earthquakes that travels through Earth’s interior
earthquake
sudden shaking of the ground caused by the movement of Earth’s crust
inner core
portions of the Earth which extends from Earth’s center to abut 5,150 km (3,200 mi) below Earth’s surface
outer core
layer composed of liquid alloys of iron and nickel, extending about 2,900 km (1,800 mi) below Earth’s surface
lower mantle
layer of Earth composted of heated and slowly deforming solid rock that lies between the base of the crust and the outer core
asthenosphere
layer of the mantle found between depths of 100 km and 200 km (62 mi and 124 mi) that is weaker and softer than the layer beneath it
lithosphere
layer of Earth that is relatively strong and consists of Earth’s rigid crust and the rigid lithospheric mantle beneath it, extending to a depth of about 100 km (62 mi)