Some Notes on Planet Earth and Earthquakes Flashcards
Third largest planet from the sun; almost spherical, flattened slightly at the poles
Earth
Earth’s mean distance from the sun
149,500,000 km
Equatorial diameter
12,755 km
Earth’s circumference
40,070 km
Composition of the earth’s atmosphere
78% nitrogen, 21% oxygen, 0.9% argon, and 0.037% carbon dioxide
Composition of the surface of the earth
30% land and 70% water
The land areas on earth are characterized by
plains, valleys, mountains, hills, and plateau
Formed when the lower portions of the earth’s surface are filled up with water
Ocean basin
The highest mountain on land
Mt. Everest (8,800 meters)
The deepest in the Philippines
Marianas trench (11,034 m)
Innermost part of the earth; thought to consist of nickel-alloy
Core
The core is divided into
Outer core - 2,900 km depth (liquid); inner core - 4,980 km (solid)
Temperature in the core is thought to be
4,000 degrees C
The result of the liquid metal in the outer core
Earth’s magnetic field
Lies below the crust; 2,800 km beneath the Earth’s crust; 67% of the Earth’s mass; region of greater rock density
Mantle
Subdivisions of the mantle
Upper and lower mantles
The mantle is primarily composed of
magnesium, silicon and oxygen in the form of silicate materials
Rocky outer layer of the earth
Crust
Type of crust that is about 10 km thick; mostly basaltic rock overlain by muddy sediments
Oceanic crust
Largely granitic composition; more complex in structure; parts of the crust is over 3.6 billion years
Continental crust
Direction where the earth spins on its axis
West to East (counter-clockwise)
Time in which the earth completes one full turn
23 hours, 56 minutes, and 4.09 seconds
Produces day and night
Rotation of the earth
Abrupt motion that propagates through the earth and along its surfaces
Earthquake
Causes earthquakes
Sudden release in rocks of strain accumulated over time as a result of tectonics
Study of earthquakes
Seismology
Where earthquakes mostly occur
Faults (fractures or breaks) and Benoiff zones
The point at which an earthquake originates
Seismic focus or hypocenter
The point on the earth’s surface directly above it
Epicenter
Movements that generate the major proportion; as two plates move past each other they can become jammed
Plate tectonic movements
Released when a sufficient strain has accumulated and the rocks break as the plates spring free
Seismic waves
The force of earthquakes
Magnitude
Measures the force of earthquakes
Richter scale
Richter scale was developed by
Charles Richter in 1935
Use of the Richter scale
Quantifying the magnitude, or strength, of earthquakes
Japan is amongst the most vulnerable location along the
Pacific Asian Ring of Fire