Chapter 3 Flashcards
Who came up with the Continental drift theory?
Alfred Wegner
Continental drift theory
How long ago would this have occurred?
Theory suggesting that all of Earth’s land had once been joined together into a single super-continent surrounded by an ocean
- pangaea: the landmass
- panthalassa: the surrounding ocean
-200 million years ago
What is the centrifugal theory?
Theory that believed the continents were slung toward the equator on the spinning Earth by a centrifugal effect
- inertia coupled with tidal drag on the continents (from the combined effects of the sun and moon) would account for the drifting continents
Is earth’s mantle a solid?
no it reacts to earthquakes, so it is a deformable mass
Seismic waves
low frequency waves generated during earth quakes
What are the types of seismic waves?
Surface waves: move along earth’s surface and the main reason for damage from earthquakes
Body waves: less dramatic, but very useful for analyzing earth’s interior surface
Types of Body waves?
P wave (primary wave): a compressional wave similar in behavior to a sound wave
S wave (secondary wave): a shear wave like that seen in a rope shaken side to side
Seismograpgh
instrument that senses and records earthquakes
Shadow zone
a wide band from which S waves were absent, would be found on the side of the Earth opposite the location of an earthquake
-existence of liquid core and shadow zone 1914, seismographic analysis
Mantle
core boundary
Crust
thin, relatively lightweight outermost layer
- oceanic crust: thin and mostly basait
- continental crust: granite
Mantle
beneath the crust, compose of 68% Earth’s mass and 83% volume
Core
intermost layer
-31.5% earth’s mass, 16% of its volume
Physical layers of the Earth
Lithosphere
Asthenosphere
Lower mantle
Core
Lithosphere
earth’s cool rigid outer layer
-Continental and oceanic crusts
Asthenosphere
hot, partially melted, slowly flowing layer of upper mantle
Lower mantle
extends to the core
- similar composition to the asthenosphere
- hotter but due to rapidly increasing pressure the mantle below the asthenosphere does not melt
Core
Two parts:
- outer layer dense viscous liquid
- inner layer solid
William Thomson
Lord Kelvin
Earth is 80 million yrs old
-based on the rate at which the planet would have cooled from an original molten mass
*drying fruit model: earth shrunk as it cooled
Radioactive decay
though most atoms are stable and do not change some forms of elements are unstable and give off heat when their nuclei break apart (decay)
- radioactive particles ejected in process
- released heat that contributed to Earth’s melting of the original mass
Conduction
Internal heat journeys toward the surface
Convection
heat that arises in the asthenosphere and mantle
- occurs when a fluid or semisolid is heated, expands, and becomes less dense and rises
James Hutton
Uniformitarianism: all of Earth’s geological features and history could be explained by process identical to today’s and these processes must have been at work for a long time
- did not believe in the bibles concept of creation