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Chapter 8
Chapter 8

... most earthquakes are produced by the rapid release of energy stored in rock that has been subjected to great forces. When the strength of the rock is exceeded, it suddenly breaks, releasing some of its stored energy as seismic waves. ...
Earthquake and Volcano Readings
Earthquake and Volcano Readings

... Earthquakes may also involve vertical crustal movements. During the Alaskan earthquake of 1964, large areas of land were uplifted or dropped down several meters. In fact, some sections of the seafloor along the coast were raised above sea level, becoming dry land. Strong earthquakes can be deadly. ...
Understanding Ocean Acidification Prior Knowledge Summary
Understanding Ocean Acidification Prior Knowledge Summary

... referred to as Entry, Adoption, Adaptation, Interactivity, and Invention. The early levels are very directed and teacher-driven, which provides important first steps when learning something new. The levels of Adaptation through Invention are more student-directed and open up opportunities to design ...
Organic Geochemistry - DISL Sharepoint Site
Organic Geochemistry - DISL Sharepoint Site

... High winds blow sea foam into the air as a person walks across Jeanette's Pier in Nags Head, N.C., Sunday, Oct. 28, 2012 as wind and rain from Hurricane Sandy move into the area. Governors from North Carolina, where steady rains were whipped by gusting winds Saturday night, to Connecticut declared s ...
Nansen-Tutu Centre for Marine Environmental Research
Nansen-Tutu Centre for Marine Environmental Research

... ...
Changes in seismic anisotropy shed light on the nature of the
Changes in seismic anisotropy shed light on the nature of the

... orientation of ocean floor fractures zones at 50 km depth near ridges, around 80 km depth for ocean ages between 80 Ma and 120 Ma, and at 100 km depth under old oceanic plates (Fig. 1). Ocean floor fracture zones are temporally stable features that record plate motion path and can thus be used as pr ...
Convection Currents and the Mantle
Convection Currents and the Mantle

... again and begins to rise. This flow that transfers heat within a fluid is called a convection current. The heating and cooling of the fluid, changes in the fluid’s density, and the force of gravity combine to set convection currents in motion. Convection currents continue as long as heat is added to ...
Buoyancy frequency profiles and internal semidiurnal tide turning
Buoyancy frequency profiles and internal semidiurnal tide turning

... often-used but inexact expressions that involve potential density. Elncertainties in N2(z) are estimated using a Monte Carlo method, where the data are averaged over a range in depth (80-200 m), which is determined by minimizing a cost function. Our principal result, reached from an analysis o f all ...
Salinity
Salinity

... at the surface is 1.025 kg/l. Seawater is denser than both fresh water and pure water (density 1.0 kg/l at 4 °C (39 °F)) because the dissolved salts increase the mass by a larger proportion than the volume. The freezing point of seawater decreases as salt concentration increases. At typical salinity ...
part 1 - North Pacific Marine Science Organization
part 1 - North Pacific Marine Science Organization

... CO2, HCO3-,CO32-), organic carbon (e.g., POC, DOC, Semi-LDOC, RDOC, CDOM), ecological processes (primary production, export production, respiration etc) and even physical oceanographic parameters (e.g., salinity, alkalinity, current, water mass, material flux) and models (box model, numerical model) ...
Plate Tectonics: Earthquake Epicenter
Plate Tectonics: Earthquake Epicenter

... these earthquakes occur at former plate boundaries between the “welded” sections of the plate. For instance, the Appalachian Mountains are the site of a former boundary between North America and Europe over 300 million years ago. They were formed when the two proto-continents crashed into one anothe ...
Notes for the unit
Notes for the unit

... the surface and create a tidal wave of rock and mud. This process is called ...
The dynamics of the marine nitrogen cycle across the last deglaciation
The dynamics of the marine nitrogen cycle across the last deglaciation

... benthic denitrification [Codispoti, 1989] (Figure 1). If the N:P ratio of the nutrient pool is lowered, the rate of export production will decrease due to an even stronger limitation by NO–3 , causing a drop in export production, a lower oxygen demand from organic matter remineralization, and thus hi ...
to Ch. 9 Notes
to Ch. 9 Notes

... 2. Pangaea: the proposed supercontinent that 200 hundred million years ago broke apart and formed the present day continents 3. plate tectonics: the theory that proposes that earth’s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, m ...
Validation of Coastwatch ocean color products
Validation of Coastwatch ocean color products

... Satellite derived values of chlorophyll concentration were extracted from a 5 x 5 pixel box centered on the position of contemporaneous in-situ measurements. SeaWiFS Level L1A files were acquired and processed using the climatologic ancillary meteorological and ozone data. A bio-optical and atmosphe ...
Lecture 2
Lecture 2

... By analyzing the seismograms from many earthquakes, scientists have discovered that three main levels or shells exist within the Earth: CRUST ...
Chapter 8 Powerpoint
Chapter 8 Powerpoint

... • Saltwater and freshwater aquatic life zones cover almost three-fourths of the earth’s surface, with oceans dominating the planet • Key factors determining biodiversity in aquatic systems – Temperature, dissolved oxygen content, availability of food, and access to light and nutrients necessary for ...
EARTHQUAKES: Origins and Predictions
EARTHQUAKES: Origins and Predictions

... Chicago and St. Louis. In the Charleston area, 100 people died as a result of the earthquake, houses cracked and collapsed, sand beds vented explosively into the air and produced craters with surrounding blankets of ejected sand. The earthquake magnitude is estimated between 7.0 and 7.7. Everyday so ...
News
News

... Hafner are members of the Working Group “Marine Debris: Scale and Impact of Trash in Ocean Ecosystems” of the National Center for Ecological Analysis and Synthesis (http://www. nceas.ucsb.edu/). The group’s mission is to (1) construct a theory of marine debris and (2) to determine the type of activi ...
PLATE TECTONICS - Part I
PLATE TECTONICS - Part I

... 1. Seafloor spreading is a double conveyor beltlike process that produces “mirrored” growth of new seafloor between two diverging plates 2. Initiated by continental rifting event 3. Mid-ocean ridges are the most typical geographic expression of active spreading 4. Plates “spread” apart to accommodat ...
Aspasia Zerva - Gateway Coalition
Aspasia Zerva - Gateway Coalition

... Chicago and St. Louis. In the Charleston area, 100 people died as a result of the earthquake, houses cracked and collapsed, sand beds vented explosively into the air and produced craters with surrounding blankets of ejected sand. The earthquake magnitude is estimated between 7.0 and 7.7. Everyday so ...
chpt 7Plate Tectonics
chpt 7Plate Tectonics

... boundaries are areas where plates move together  As crust is added in one area, crust disappears in other areas when seafloor cools, becomes denser and sinks (convergent boundaries)  When oceanic crusts converge with less dense continental crust, the denser oceanic plate sinks under the continenta ...
Types of Seismic Waves
Types of Seismic Waves

... Volcanoes form volcanic mountains and these mountains are then shaped by further eruptions, lava flows, and collapses forever altering the view of this mountain. So explosive was this eruption, that it can alter the height of the mountain by nearly 1,300 feet. other major Volcanic Mountains in North ...
Plate Tetonics
Plate Tetonics

... accepted was because he suggested no mechanism for moving the continents. His belief that the force of Earth’s spin (rotation) was enough to cause the continents to move was not shared by the geologists of the time who knew that rocks were too strong for this to be true. • For an article outlining t ...
Terrigenous Sediments - Lamont
Terrigenous Sediments - Lamont

... Petrography studies allow identification of major lithological components in the sand fraction, as well as potentially diagnostic minerals and/or rock types. This approach has been particularly useful for identifying sources of IRD in the ocean. For example, it was the first line of evidence used to ...
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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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