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Quiz 1 (Key)
Quiz 1 (Key)

... 27. The Figure below suggests that: a) the western Pacific is very young, b) the south Atlantic opened several million years after the north Atlantic, c) the ocean basins became a feature on the surface of Earth 250 million years ago, d) the age distribution of oceanic crust is an additional evidenc ...
9.2 & 9.3 Plate Tectonics and Actions
9.2 & 9.3 Plate Tectonics and Actions

... Convergent Boundaries  Boundary where 2 plates move together  Results in oceanic lithosphere going beneath an overriding plate, and descending into the mantle  The India Plate pushing upward into Eurasian Plate and creating the Himalayan Mountains ...
Global phosphorus cycle
Global phosphorus cycle

... of surface water CO2 → invasion of atmospheric CO2  P as a limiting nutrient limits CO2 draw-down 2) Assessing paleoceanographic P levels  Cd:Ca ratio in benthic forams as a proxy for DIP  [Cd] is linearly correlated to [PO4] (DIP) in modern oceans. ...
PhET Plate Tectonics Simulation Lab
PhET Plate Tectonics Simulation Lab

... Look at your table for convergent boundaries. Three times the same two types of crust were used, but you switched what side they were on. What do you observe about the results? ______________ _____________________________________________________________________ Look for patterns in density, subducti ...
Plate Tectonics
Plate Tectonics

... The Great Rift Valley in eastern Africa is becoming a divergent plate boundary. Iceland is also. ...
Ocean Floor, Plate Tectonics, Water Test Review
Ocean Floor, Plate Tectonics, Water Test Review

... North American plate South American plate  Seafloor spreading (Henry Hess, new crust is formed) Water  Water cycle (condensation, evaporation, precipitation)  Distribution of water (know the %) - rivers, lakes, ponds - groundwater - oceans and seas - glaciers, ice sheets  Properties of water - s ...
Estimating How Much Sea Level Changes when
Estimating How Much Sea Level Changes when

... At times during the Quaternary Period (approximately the last 2 million years of Earth history), glaciers were much more extensive than they are now. The world’s ocean was the source of the glacial ice, and so sea level was significantly lower when the additional ice was present. As Earth still has ...
The Ocean Acidification Initiative Goal: $2.5 million
The Ocean Acidification Initiative Goal: $2.5 million

... Maine may be particularly sensitive to acidification. Already, subsurface acidity is relatively high and the saturation state of calcium carbonate – the mineral that many organisms need to make shells – is particularly low. There is an urgent need to better understand this changing ocean chemistry a ...
Making Oceans and Continents
Making Oceans and Continents

... Hess’ seafloor spreading in detail Seafloor spreading occurs along relatively narrow zones, called rift zones, located at the crests of ocean ridges called Mid-Ocean Ridges (MOR’s). These are above hot rising mantle. As plates pulled apart, cracks allow low pressure and water to hit mantle. Causes ...
Catastrophic Events
Catastrophic Events

... Volcanic eruptions Meteorite impact Underwater landslides ...
Plants and light in the ocean
Plants and light in the ocean

... Too dark for growth plankton grow only in the top 100 metre-thick layer ...
Plate Tectonics Study Guide
Plate Tectonics Study Guide

... 8) Outer Core: Made of iron & nickel and is liquid. Convection currents here cause plate movement & magnetic field 9) Inner Core: Dense, solid ball of iron and nickel. Has the most pressure and highest temperature of the layers 10) Lithosphere: Upper most part of the mantle and crust. Very rigid and ...
Earthquakes
Earthquakes

... and expands the ground • The first wave to arrive at an earthquake http://daphne.meccahosting.com/~a0000e89/insideearth2.htm ...
PLATE TECTONICS
PLATE TECTONICS

... • The ages and types of rocks in the coastal regions of widely separated areas matched closely. • S. America and Western Africa ...
Discovery Education: Earth`s Spheres interactive text
Discovery Education: Earth`s Spheres interactive text

... The remaining gases are found in the atmosphere in trace amounts. Several of the trace gases have a tremendous impact on the planet. Carbon dioxide, water vapor, methane, sulfur dioxide, ozone, and nitrogen oxides are greenhouse gases. These gases absorb long-wavelength radiation from Earth’s surfac ...
Final_Exam_Review_Answer_Key
Final_Exam_Review_Answer_Key

... 24. Hurricanes typically originate in the trade winds off the coast of Africa. As long as it is in the trade winds, it will travel east to west. Remember that hurricanes intensify over warm water but lose their strength over cooler waters. Pacific waters are cooler waters than water in the Atlantic. ...
4 layers of Earth and Plate Activity notes
4 layers of Earth and Plate Activity notes

... • When plates collide they create mountains this is called a collision zone • Appalachian mountains – Africa collided with North America during formation of Pangea • Destroy sea floor- ocean plates more dense than land plates, when they converge ocean plates slide under land plates ...
How are octopus species related?
How are octopus species related?

... We have seen that continental drift caused Antarctica to be separated from South America about 34 mya. The Drake Passage was formed, creating a cold oxygen-rich deep water environment. The fossil record shows new species of deep water octopus evolved about the same time. When similar species of octo ...
Eons, Eras, Periods and Epochs Dating by radioactive isotopes
Eons, Eras, Periods and Epochs Dating by radioactive isotopes

... Wave height The distance between trough and crest Wave period The time taken for two crests to pass a given point (remains almost constant) λ=V*P The wavelength, λ, is the product of its velocity and period. ...
Continental Drift: The Beginning of Plate Tectonics
Continental Drift: The Beginning of Plate Tectonics

... Idea that all continents were all pieced together 245 million years ago Pangaea = “All Earth” ...
Plate Tectonic Model Rubric
Plate Tectonic Model Rubric

... Drift Theory, Layers of the Earth, Seafloor formation, Parts of the Ocean floor, Theory of Plate Tectonics ...
No Slide Title
No Slide Title

... How are the ocean basins formed? How permanent are these features? What is the age of the ocean floor? What’s the age of the continents? Why are the ocean basins deep and the continents high? ...
2017Geological Oceanography
2017Geological Oceanography

... • These canyons cut into the continental shelf and slope, ending in a deep-sea fan • Sometimes they extend from the mouth of a river that drains sediment and fast flowing water out to sea – Created by erosion like canyons on land ...
EARTHQUAKES.2
EARTHQUAKES.2

... Shear wave or secondary waves vibrate back and forth perpendicular to the direction the wave is moving  Slower than P waves (4-5 kms./s)  TRAVEL THROUGH SOLIDS ONLY ...
Earthquakes
Earthquakes

... Shear wave or secondary waves vibrate back and forth perpendicular to the direction the wave is moving  Slower than P waves (4-5 kms./s)  TRAVEL THROUGH SOLIDS ONLY ...
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Physical oceanography



Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.
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