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Igneous Rocks II: Heat, magma generation, and differentiation
Igneous Rocks II: Heat, magma generation, and differentiation

... can give rise to the observed range? – Could this spectrum be generated from a much narrower source range and the derived liquids modified to yield the observed diversity? ...
Identifying Plate Tectonics Lab 1-34
Identifying Plate Tectonics Lab 1-34

... one another. Neither plate subducts under the other plate and down into the mantle because both plates are made of _____________________ which has a density that is much ___________________ than the density of Basalt / Granite / the Mantle, so neither plate can sink down into it. Since the plates ca ...
Chapter 8 - Earthquakes
Chapter 8 - Earthquakes

... fault lines where the sliding action of these tectonic plates causes vibrations felt as earthquakes. Deformation – stress caused by the bending, tilting or folding of rock layers causing them to change shape. Plastic Deformation – rocks bend but do not break; these do NOT cause earthquakes. Elastic ...
Inside Earth – Chapter 1
Inside Earth – Chapter 1

... on Earth. This fairly small, lizardlike reptile measured 71 centimeters from its nose to the tip of its tail—or about two thirds of a meter. Its body was long and flexible, perfect for swimming swiftly through the water. Mesosaurus was a hunter of small fish and other aquatic animals. Its webbed fee ...
Earth Science Outline What is Earth Science? Branches Geology
Earth Science Outline What is Earth Science? Branches Geology

... b. Epicenter – area on the surface directly above the focus VI. Beaches and Barriers a. Classifying coasts i. Tectonic setting 1. Collision plate margin coast 2. Trailing margin coast ii. Beach 1. Dynamic beach – A beach is a ever-changing landform altered by wind, currents, sea level, deposition an ...
Plate Tectonics
Plate Tectonics

... for the Geosciences, at least! The Earth’s lithosphere (crust) is broken into pieces that move by means of mantle convection currents, and in the process allow continents to move like boxes on a conveyor belt ...
Marine pollution A case study of oceanic pollution and how it affects
Marine pollution A case study of oceanic pollution and how it affects

... nowhere for the water to go when natural agents are taken away. The oceans provide many great benefits which is why the need for protection is necessary. Indications of Problem Pollutants affect the entire aquatic community.6 According to the EPA, the major threat to coastal waters is from urban ru ...
The Marine Environment
The Marine Environment

... Seawalls Structures called seawalls, shown in Figure 16.12, are built parallel to shore, often to protect beachfront properties from powerful storm waves. Seawalls reflect the energy of such waves back toward the beach, where they worsen beach erosion. Eventually, seawalls are undercut and have to b ...
Chapter 1 Planet Earth
Chapter 1 Planet Earth

... and scoured by running water, which moves rocks around and changes their appearance.  Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natural agent, such as wind, water, ice or gravity.  Erosi ...
Unit C UA pt B - LD Industries
Unit C UA pt B - LD Industries

... ________ - relating to waves that travel through Earth as a result of explosions or earthquakes ________ - a large concentration of petroleum confined between layers of impermeable shale ________ - an instrument that records seismic waves ________ - a submerged ridge of rock, sand, or coral that ris ...
Earthquakes and Plate Boundaries
Earthquakes and Plate Boundaries

... • Some earthquakes occur more than 100km below Earth’s surface • The deepest earthquakes occur at convergent plate boundaries – Here the denser oceanic plate subducts into the mantle – These earthquakes release tremendous amounts of energy ...
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4 per eco

... X X ...
Grade 6 Chapter 1 Study Guide
Grade 6 Chapter 1 Study Guide

... movements in the liquid outer core are believed to be responsible for the magnetic field.  Realize that temperature and pressure increase as you travel towards the center of the earth’s core. ...
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06SC_TEST7 - Secondary Science Wiki

... B. The oceanic crust will push the continental crust so that a separation occurs between the two crusts. C. Uplift of the continental crust will occur as the result of pressure applied by the oceanic crust. D. As the two crusts slide past each other, the routes of rivers and streams may be changed. ...
Press Release - English ()
Press Release - English ()

... as cores are collected from 1.2 kilometers depth below the seafloor. Based on previous data from deepsea hydrothermal vents, researchers expect the upper limit of life in the seafloor near 120°C. The hottest life currently catalogued on Earth includes Geogemma barossii, a single-celled organism thri ...
6th Grade Science Formative Assessment 5 Multiple Choice
6th Grade Science Formative Assessment 5 Multiple Choice

... B. The oceanic crust will push the continental crust so that a separation occurs between the two crusts. C. Uplift of the continental crust will occur as the result of pressure applied by the oceanic crust. D. As the two crusts slide past each other, the routes of rivers and streams may be changed. ...
One Hundred Sixth Congress Of the United States of America
One Hundred Sixth Congress Of the United States of America

... a description of each program, the current funding for the program, linkages to other Federal programs, and a projection of the funding level for the program for each of the next 5 fiscal years beginning after the report is submitted. ...
The Mid Atlantic Ridge
The Mid Atlantic Ridge

... Magma rock from the Earth’s mantle has oozed out and built up over millions of years on the floor of the Atlantic Ocean. The magma eases its way up through the Mid Atlantic Ridge, an 18,000 km long plate boundary that runs north to south up and down the floor of the Atlantic Ocean. Iceland lies abov ...
Section: Continental Drift
Section: Continental Drift

... ______1 . The German scientist Alfred Wegener proposed a hypothesis now called a. paleomagnetism. c. floating continents. b. continental drift. d. sea-floor spreading. ______ 2. Wegener hypothesized that the continents formed part of a single land mass, or a. mid-ocean ridge. c. supercontinent. b. m ...
Instructor`s Notes: Chapter 17 Earth`s Interior Earth`s Interior Indirect
Instructor`s Notes: Chapter 17 Earth`s Interior Earth`s Interior Indirect

... Crust- Mantle boundary (Moho) is compositional change at 410 kilometers (255 miles), there is a phase change where less dense mineral due to increased pressure collapse to denser formsOlivine- spinel At 660 kilometers (410 miles) phase change where spinel- perovskite (Mg Fe) Sio3 D” layer -lower 200 ...
P waves
P waves

... (pressure waves). They are the fastest seismic waves, so P waves always travel ahead of other seismic waves. They can also be called primary waves because they are always the first waves of an earthquake to be detected. If you were to tap a gelatin cube, you would notice its elastic-like movement. T ...
17.3-homework - Maples Elementary School
17.3-homework - Maples Elementary School

... _________13. Which of the following best describes what happens when a oceanic plate converges with a continental plate? a. a deep-sea trench and a island arc form b. both plates become fractured, and a series of long faults form on the surface c. both plates crumple and a folded mountain range form ...
Earthquakes
Earthquakes

... in a series of aftershocks ...
Meteorology
Meteorology

... Figure 5-2, simplistic representation In reality, land & water do not respond to solar heating similarly Terrain is uneven ...
An Introduction to the Seafloor and Plate Tectonics
An Introduction to the Seafloor and Plate Tectonics

... by the ocean. The average ocean depth (3800m) is 4.5 times greater than the average elevation on land (840 meters), yet it is only a tiny fraction of the total Earth’s volume on a planetary scale (0.13% of the Earth’s volume). Although the rest of the Earth is composed of rock, it is not homogeneous ...
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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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