Unit 12 Flashcards
Inner core
a) solid and dense
b) iron and Nickle exist here in a solid state due to high pressure
c) radius is only 1,220km (760 miles) & surface is 5,150km below sea level
d) incredibly hot at the center; 6000 Celsius/10832 F
outer core
a) Liquid
b) Consist of same materials as inner core
c) Pressure is less, so the molten state prevails
d) 2,250km (1400 miles) & surface lies 2900 km below sea level
e) Temperature ranges 8100-9900 F
Lower mantle
A) Sometimes referred to as Mesosphere
B) 22,230 km thick
C) More solid than upper mantle
D) Composed of iron, magnesium, and silicon compounds
Upper Mantle
A) Extends from the base of the crust to a depth of just 670 KM
B) Less dense and not a solid
C) Interacts with crust
Lower Part of upper mantle
consists of molten rock & called asthenosphere
Upper part of upper mantle
less molten and transitioning into a solid; becomes more rigid and rock like as you approach the surface & called Lithosphere
crust
Mohorovicic “moho” Discontinuity; 1909; Andrija Mohorovicic (Croatian scientist)
Dividing line between the crust and mantle
A) Lies directly above mantle
B) Thickness varies (5km-40km)
C) Elements, minerals, and rocks found here
Continental Crust
portion of earth that forms continent; landmass; thicker; low density; called a root; felsic rocks
Oceanic Crust
thin; more dense; made up of mafic rocks
Underwater Lithosphere: The ocean Basins
Secrets of submerged 71 percent of lithosphere are finally being revealed
Technological advances
- sounding devices have allowed for ocean floor topography mapping
- deep sea submersibles
The Ocean Basins
- Ocean floors have varied topography (not extension of land)
- Divided into three categories: margins of continents, the abyssal zone, systems of ridge surrounded by fractures and reliefs
Continental Shelf
outlines the continents that is shallow (Ocean depths are less than 600ft) Gently sloping, submerged plane at edge of continent. (width 50-700 miles)
Continental slope
begins where the continental shelf ends and plunges steeply downward
Continental rise
transition zone of gently sloping seafloor; pile of debris; leads to abyssal zone