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Introduction to Earthquake Geophysics
Introduction to Earthquake Geophysics

... ¾The other kind of surface wave is the Rayleigh wave, named for John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885. ¾ A Rayleigh wave rolls along the ground just like a wave rolls across a lake or an ocean. Because it rolls, it moves the groun ...
Glacial-interglacial variations in marine phosphorus cycling
Glacial-interglacial variations in marine phosphorus cycling

... connectivity between water masses during glacial times could have been no more than 30% weaker than today’s. [17] Whatever the debate over open ocean water exchange may be, the case for increased coastal upwelling is particularly strong due to the increased geostrophic circulation (particularly Eckm ...
1/29/17 1 Lecture 9: Earthquakes
1/29/17 1 Lecture 9: Earthquakes

... Seismicity: minor earthquakes in the past month on the southwest flank of Mauna Loa. All recent earthquakes small relative to earthquake sequences before eruptions in 1975, 1984. Deformation: GPS data has been showing variable inflation rate since the start of the current, renewed inflationary perio ...
IBDIOCC - Scientific Committee on Oceanic Research
IBDIOCC - Scientific Committee on Oceanic Research

... This proposal is timely owing to the increasing interest of “Oceans in the High Carbon World.” The proposed work is truly global in scale encompassing Exclusive Economic Zones (EEZs), Extended Continental Shelves and the High Seas (Areas Beyond National Jurisdiction) in all world oceans. There are a ...
Chapter 33 Plate Tectonics
Chapter 33 Plate Tectonics

... – Direction to the magnetic pole at the time the rock was formed – Magnetic latitude of the rock’s location at the time it was formed – The movement of the magnetic pole over time(500 million years) suggests that either the pole moves around or the continents move ...
Multiple Choice Questions
Multiple Choice Questions

... 26. With increasing metamorphism, foliation would change from: a. gneiss, to schist, to phyllite, to slate b. slate, to phyllite, to schist, to gneiss c. phyllite, to slate, to gneiss, to schist d. schist, to gneiss, to slate, to phyllite 27. Which of these two minerals would indicate a higher grade ...
Transatlantic Arctic and Marine Research Initiative
Transatlantic Arctic and Marine Research Initiative

... China and South Korea. It aims at increasing the understanding of climate change in the Arctic region and its impact on socio-economic activities such as marine transportation and tourism, fisheries and aquaculture, and oil and gas extraction. In order to understand the environmental change in the A ...
Waves are “disturbances”
Waves are “disturbances”

... The waves’ height, wavelength, and speed change as they approach the beach – but one wave characteristic does not change: wave period (frequency). Here is another way to think about why waves grow at a beach: the front part of a wave crest is in slightly shallower water than the back part of the wav ...


... Federal Leadership in Ocean Science and Technology Since the mid-1900s, the U.S. government has achieved a leadership role in ocean science and technology. For many years, the U.S. Navy was the major supporter, primarily through the Office of Naval Research (ONR). Since the National Science Foundati ...
Plate Tectonics - Hope Valley Library
Plate Tectonics - Hope Valley Library

... plates get stuck, and when released the energy is in the form of a earthquake. Shock waves are the vibration after a earthquake. Measured by the Richter scale for power and Mercalli scale for effect. There are different types of earthquakes. Surface waves travel only through the crust. Body waves tr ...
Advances in Environmental Biology
Advances in Environmental Biology

... For a long time the attention of researchers from different areas of the Earth sciences was attracted by the results of some observations which evidenced that the northern and southern hemispheres of our planet are asymmetric ones in many respects. Apparently, one of the first scientific evidences c ...
Q.1
Q.1

... Narrow zones (few hundred kms wide, thousands of kms long) in oceans Wider zones on continents (Himalayas - Asia) Sometimes join/divide e.g. Indian ocean Associated with belts of mountains, ocean ridges, volcanoes, rift valleys, island arcs, trenches. (e.g. Himalayas/ Atlantic, Circum-Pacific) Assoc ...
coastal and marine spatial planning – including applications for
coastal and marine spatial planning – including applications for

... predominance of fishing and shipping activities. The advent of sectors such as offshore oil and gas, aquaculture, offshore renewable energy, submarine cables/communications and coastal/near shore tourism and recreation has resulted in increased competition for coastal and ocean space as well as pote ...
The Deepest Place on Earth
The Deepest Place on Earth

... The water in the trench is so cold it is almost freezing. Some areas in the trench are very hot, though. These areas are called hydrothermal vents. The vents are openings in the earth through which very hot water shoots up through the ocean floor like smoke from a chimney. The water from the vents i ...
Our Australia - One Place, Many Stories: Oceans
Our Australia - One Place, Many Stories: Oceans

... The Leeuwin Current runs south along the west coast of Australia, around the south-west corner, and all the way across the Great Australian Bight to Tasmania. Originating in the Indian Ocean, it is the longest coastal current in the world, travelling for about 5000 kilometres along a pathway less th ...


... spreading outward from mid-ocean ridges (ODP Holes 857D and 858G), young mid-ocean ridge flanks (395A, 1024C, 1025C, 1026B, 1027C), and accretionary prisms, where sediments scraped off descending seafloor plates accumulate in front of overriding plates, like debris in front of a locomotive’s cowcatc ...
AGENDA
AGENDA

... 1.9 m by the end of the century, but there are significant unknowns in predicting future sea level including high local variability, and differences in model results. Nonetheless, these values provide science-based planning targets for local decision-makers to implement sea level rise adaptation pro ...
Ocean Basins and Crust
Ocean Basins and Crust

... •Oceanic crust with “thick” deposits of continental material, mostly carried in by turbidity currents (subaqueous mudflows.) Submarine fans (a lot like alluvial fans or deltas) can coalesce, forming the continental rise. Very flat. •Oceanic part (basaltic, can be denser than mantle when old) –Abyssa ...
Pangaea
Pangaea

... The plate tectonics theory came about in the 1960s and 1970s as new information was obtained about the nature of the ocean floor, the distribution of volcanoes and earthquakes, the flow of heat from Earth's interior, and the worldwide distribution of plant and animal fossils. The theory states that ...
Part B - Bakersfield College
Part B - Bakersfield College

... • Ridged lithospheric plates (continents + ocean floor) ride along the soft layer (like hot wax) called the asthenosphere • Plates spread apart, collide, and slide past one another. • EQ’s, crustal deformation, and volcanism take place at plate ...
earthquakes1
earthquakes1

... When S-waves hit the outer liquid core, they stop. This creates a S-wave shadow at locations greater than 103º from the focus of the earthquake. ...
No Slide Title
No Slide Title

... When S-waves hit the outer liquid core, they stop. This creates a S-wave shadow at locations greater than 103º from the focus of the earthquake. ...
Document
Document

... A present-day mantle upwelling beneath Iceland dynamically supports the bathymetry of the North Atlantic Ocean. Varying dynamic support has controlled uplift and subsidence at Earth's surface throughout Neogene times. Intersection of the Mid-Atlantic Ridge with the Iceland plume provides us with a w ...
PowerPoint
PowerPoint

... A. Summer causes heated air to rise over the land and a strong low-pressure cell to develop at surface. B. The rising of heated air causes a net inflow of moisture-bearing winds from the ocean bringing heavy rains to the east coast. C. The situation in the winter is exactly reverse. ...
Opener 1/6/2015 What are “Big Ideas”? What are the four classroom
Opener 1/6/2015 What are “Big Ideas”? What are the four classroom

... 1. What direction do divergent plates move? 2. What are the three types of convergent plate boundaries? 3. What natural hazards are typically caused by transform fault plate boundaries? ...
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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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