Constant motion & travels a few centimeters every year.
Composed of both continental and oceanic crust
Crust
Uppermost layer of earth & thinnest
composed of hard strong rocks because it is relatively cool, contains dark dense basalt.
humus - decaying organism (reason why crust is dark or brown)
Mantle
The layer that lies directly beneath the crust, thickness of 2,900km
Upper Mantle
Made up of Fe & Mg but poor in silica, 400 km thick & denser than the crust
Asthenosphere
Lies below the lithosphere, part of the upper mantle, layer of weak rocks which extends from about 100-350 km deep, layer where plate floats and involves plate tectonic movements
Lower Mantle
Denser than the upper mantle, has a greater amount of Fe
Core
Innermost layer of the earth, made up of Fe & Ni, inner core - solid; 1300km, outer core - liquid; 2100 km (made of Fe, na hindi agad natutunaw)
Geologists estimated that there are 100,00 active and inactivevolcanoes on earth
Earth's Crust
The boundary between the crust and the mantle, discovered in 1909 by Andrija Mahorovicic, 8 km beneath ocean basins, 32 km beneath continental surfaces
Mohorovicic Discontinuity
An increase in the velocity of the seismic waves
Continental Crust
Makes up earth's landmasses
Oceanic Crust
Found in the ocean floor and is usually thinner than continental crust, forms landforms below the oceans and the seas because it is heavier, denser and darker
Alfred Wegener
German meteorologist and geophysicist, formulated the most complete statement of the continental drift hypothesis
Alfred Wegener's Continental Drift Theory proposed that the continents formed one supercontinent Pangaea and started to drift away
Evidence for Continental Drift
Some types of fossilised animals and plants found in S. Amera and Africa
The shape of the east coast of S. America fits the West of Africa
Matching the rocks formation and mountain chains found in S. America and Africa are identical
Convection Current
Movement of materials caused by the difference in their temperature, the part of the mantle closer to Earth's core is much hotter than the part farther from the core and closer to the lithosphere
Harry Hess
Professor of geology at Princeton University, found father of the unifying theory of plate tectonics
Seafloor Spreading Theory
Basaltic magma from the mantle rises to create a new ocean floor at mid-ocean ridges, great deal of volcanic eruption and earthquake activity occurs at mid-ocean ridges
Subduction
Two plates meet, one plate containing the oceanic lithosphere ascends beneath the adjacent plate
Magnitude
Refers to the energy release by an earthquake, indicates amount of energy released of the epicentre, measured by the open-ended richter scale
Mercalli Scale (Modified)
Used in NZ, HK, Canada, US
PEIS
Phivolcs earthquake intensity scale used in the Philippines
Seismograph
Instrument that detects and measure waves, tool used by scientists to detect earthquakes and its strength
Seismogram
Record produced by the seismograph, perfected by a British scientist John Milne
Richter Magnitude Scale
Device or a standard used by measuring the earthquake, developed by Charles F. Richter of the California Institute of Technology in 1935, mathematical device designed to measure the magnitude of the earthquake in terms of the amount of energy released during an earthquake
Tidal
Gravitational interaction between earth & moon
Tsunami
Caused by earthquakes of magnitude 7.0 and above
Storm Surge (Daluyong)
Caused by atmospheric conditions, low pressure area
Intensity
Measures the strength of trembling produced by the earthquake at a certain place, determined from the effects brought on people, buildings and the environment
Modified Mercalli Scale
Used by countries like NZ, USA, Canada, Hong Kong, descriptive scale from 1 – 12 based on how people feel an earthquake
PHIVOLCS Earthquake Intensity Scale
Used solely by the Philippines, descriptive scale from 1 -7
October 4, 1957 - Soviet rocket launched Sputnik 1 into orbit around the earth, the USSR dominated space exploration until 1961
November 3, 1957 - Sputnik 2 was the first such biological spacecraft, sending the dog Laika into orbit
January 31, 1958: The US successfully launched its first spacecraft – Explorer 1, it discovered the magnetic radiation belts around the Earth called – Van Allen radiation belts
October 1, 1958: Created NASA from National Advisory Committee for Aeronautics (NACA)
July 1958: US Congress passed the National Aeronautics and Space Act (Space Act of 1958)
Jan. 2, 1959: The USSR sent a lunar - Luna 1, the first spacecraft to reach the vicinity of the Moon and the first to leave Earth's gravity
Sept. 12, 1959: Luna 2 is the first spacecraft to hit the moon's surface
Luna 3: circled the Moon and recorded the first photographs of the far side of the moon
April 12, 1961, the dream to travel in space became reality when cosmonaut Yuri Gagarin orbited Earth