Neptunism proposed that all rocks come from deposition from a primordial ocean
Before Plate Tectonics, there was no coherent theory to explain the Earth’s structure and processes
The highest point on the Earth’s surface is Mount Everest, 8,848m (29,030 ft.) high
Continental Drift Theory states that Pangea broke off into two large masses, Laurasia and Gondwanaland, with the Tethys Sea separating them
Seafloor Spreading
1. Discovery of Oceanic Ridge System
2. New crust creation via convection in the mantle pushing old crust away
3. No oceanic crust is older than 200 mya
Continental Drift Theory was proposed by Alfred Wegener in a series of papers from 1910-1928
Continental Drift Theory was rejected due to the inability to explain a credible mechanism for the continental drift
Rocks with increasing age point to pole locations
Theories before Plate Tectonics
Neptunism
Plutonism
Plutonism proposed that all rocks are formed by igneous processes (crystallization from magma)
Continental Drift Theory suggests that continents were once a single large mass (Pangea) surrounded by a large ocean (Panthalassa)
The deepest part of the ocean, the Marianas Trench, is 11,033m (36,199 ft.) deep
Evidences supporting Continental Drift Theory
1. Fit of the continents
2. Fossil evidence
3. Similar lithologies across continents
4. Paleoclimate
Paleomagnetism
Record of magnetic field throughout time
Harry Hess theorized how continents drift via seafloor spreading
Volcanic rocks usually contain magnetite (iron-bearing mineral)
Paleomagnetism
Record of the magnetic field throughout time
Earth has more than one magnetic pole at various times
Plate Tectonics was brought together in 1968 based on evidences presented from continental drift theory, seafloor spreading, and paleomagnetic evidences
Earth’s lithosphere is made up of moderately rigid plates consisting of continental, oceanic, or a combination of both
Plate boundaries can move a few centimeters a year
8 minor plates
Philippine Sea Plate, Nazca Plate, Cocos Plate, Caribbean Plate, Arabian Plate, Scotia Plate, Indian Plate, Juan de Fuca Plate
Apparent Polar Wandering
1. A moving continent retains a record of changing paleomagnetic directions through time that reflect the changing orientations and distances to the pole
2. The resulting path of observed pole positions is called an “apparent polar wander path” or APWP
Divergent Boundary
1. Constructive Plate Boundary: new crust is created in the mid-oceanic ridge and pushes older crust away
2. Continental Rift
3. Mid-Ocean Ridge
Hotspot Volcanism: Formation of Hawaii from a mantle plume, creating chains of volcanic islands due to plate movement
Earthquakes were used to map the plate boundaries
Curie Temperature
Temperature where magnetic minerals change magnetic behavior
Rocks with increasing age point to pole locations increasingly far from present magnetic pole positions
The continents moved relative to each other over time
Plate Tectonics is a unifying theory of geology as it explains how geologic processes and features on Earth are closely related
North is determined by the angle of the earth’s axis (located 11.5 degrees away from true north)
Magnetic Reversals as Evidence to Seafloor Spreading
1. Geomagnetic Reversal - shifting of the pole’s polarity over time
2. Happens every 300,000 years (last reversal happened 770,000 years ago)
3. New crust created in oceanic ridges records this reversal in polarities throughout geologic time
7 major plates
Eurasian, Australian, Pacific, North American, South American, African
Convergent Boundary
1. Destructive Plate Boundary
2. Ocean-Continent Convergent Boundary
3. Ocean-Ocean Convergent Boundary
4. Continent-Continent Convergent Boundary
Tectonic Plate
Slabs of rock that the continents and oceans rest on, consisting of the crust and the uppermost mantle
Distribution of volcanoes has a strong connection with plate boundaries (Pacific Ring of Fire)
Global Positioning System (GPS) data tracks plate motions by satellites, radars, and lasers from different areas
Transform Plate Boundary
Conservative Plate boundary
Philippine Mobile Belt formed by the collision of at least three plates (Sunda Plate, Philippine Plate, Indo-Australian Plate, and Eurasian Plate)
Formation of Hawaii
1. Created from mantle plume, stationary and semi-permanent source of magma
2. Created chains of volcanic islands due to plate movement