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6th grade PASS Review
6th grade PASS Review

... The image below demonstrates the seismic wave activity (P waves and S waves) from a recent earthquake. Analyze how the P waves and S waves move through Earth’s layers. This illustration best supports which of the following? A. The outer core is made of liquid. ...
Earthquake test review 8th grade Earthquake Review for
Earthquake test review 8th grade Earthquake Review for

... ___________________ 1. The theory of plate tectonics suggests that Earth’s crust is broken into sections called plates. ____________________2. The uppermost portion of the mantle is liquid. ____________________3. The lower portion of the crust and the upper portion of the mantle is called the core. ...
Slow and Steady
Slow and Steady

... pushed up. If one plate goes underneath the other during collision, deep trenches in the ocean and volcanic islands form. This can be seen in the island chain of Hawaii. Plate boundaries also exist where plates pull away from each other. These are called divergent plate boundaries. At these boundari ...
Creation and evolution of the oceanic lithosphere: contributions from
Creation and evolution of the oceanic lithosphere: contributions from

... Recent achievements in ocean drilling of the lithosphere have changed fundamentally our view of the crust and upper mantle. Using the strategy of offset drilling in tectonic windows, ocean drilling has shown that the lower ocean crust formed at fast- and slow- spreading ridges differs dramatically i ...
Theory of Plate Tectonics: Mechanism 1
Theory of Plate Tectonics: Mechanism 1

... – collision zones (e.g. Himalaya) and – Subduction zones (e.g. Japan, Andes, Aleutians) ...
The Dynamic Earth – Plate Tectonics
The Dynamic Earth – Plate Tectonics

... In 1965 Wilson proposed the concept that the crust of the Earth is a mosaic of interacting plates – hence “plate tectonics” These plates move relative to each other The continents ride on these plates ...
Plate Boundaries…
Plate Boundaries…

... As the crust widens and thins, valleys form in and around the area Volcanoes too (may become increasingly active) Early in rift formation, streams and rivers flow into the low valleys and long, narrow lakes can be created. Eventually, the widening crust along the boundary may become thin enough that ...
Basic Act on Ocean Policy (Act No. 33 of April 27, 2007) Table of
Basic Act on Ocean Policy (Act No. 33 of April 27, 2007) Table of

... Article 1 The purpose of this Act is, with regard to the oceans, to stipulate the basic principles, to clarify the responsibilities of the State, the local governments, business operators and the citizens as well as to formulate the basic plan with regard to the oceans and other basic matters with r ...
Reconstructing geographical boundary conditions for palaeoclimate
Reconstructing geographical boundary conditions for palaeoclimate

... dynamics to explain how the meridional atmospheric (or sea surface; Bijl et al., 2009) temperature gradient can become so flat in a greenhouse climate. It is therefore essential to try and simulate the past climate with a similar amount of detail as is done for the present to better understand the c ...
Steely-Eyed Hydronauts of the Mariana
Steely-Eyed Hydronauts of the Mariana

... make room for laboratories, dredging equipment, and measuring apparatuses. She and her crew of 243 sailors and scientists set out on a long, meandering circumnavigation of the globe with orders to catalog the ocean’s depth, temperature, salinity, currents, and biology at hundreds of sites–an oceanog ...
Chapter 14 - apel slice
Chapter 14 - apel slice

... assignment: to investigate everything about the sea. Your vessel: a ship powered by sails and a steam engine. On board there are thermometers for measuring the temperature of ocean water and cable for lowering dredges beneath the surface. With the dredges, you scrape sand, muck, and rock from the oc ...
Going Their Separate Ways
Going Their Separate Ways

... This interval is approximately the time needed for the ocean floor to move from the ridge crest to the trenches, where oceanic crust descends into the trench and is destroyed. Meanwhile, magma is continually rising along the mid-oceanic ridges, where the "recycling" process is completed by the creat ...
GLIDERS FOR RESEARCH, OCEAN OBSERVATION AND
GLIDERS FOR RESEARCH, OCEAN OBSERVATION AND

... The group hopes to assess and evaluate the use of a roadmap – for adhering to a number of short- and long-term goals – and tools for the implementation of a sustained and coordinated glider component that meets the standards and expectations of a European Network of Marine Observations, eg. contribu ...
Juniata College Shake, Rattle, and Roll Earthquake Board and
Juniata College Shake, Rattle, and Roll Earthquake Board and

... Surface waves -Seismic waves, slower than P or S waves, that propagate along the Earth's surface rather than through the deep interior. Two principal types of surface waves, Love and Rayleigh waves, are generated during an earthquake. Rayleigh waves cause both vertical and horizontal ground motion, ...
Chapter 2 Earthquakes
Chapter 2 Earthquakes

... 3. Aftershocks- Aftershocks is an earthquake that occurs when a larger earthquake has hit an area. Aftershocks can occur ______, ________ or ___________ after the original earthquake has taken place. 4. Tsunamis- Tsunamis are caused by the _____________of the ocean floor, when an earthquake has caus ...
Lecture 2b: Hot spots
Lecture 2b: Hot spots

...  A large summit caldera develops when the roof collapses into a shallow (<1 km below summit) magma chamber. Most lavas ascend to this summit magma chamber and degas and differentiate there, even if they erupt down on the…  Rift zones that develop when gravitational stresses and push from intruding ...
EARTHQUAKES THE BIG IDEA REVIEW VOCABULARY
EARTHQUAKES THE BIG IDEA REVIEW VOCABULARY

... Earthquakes cause seismic waves that can be devastating to humans and other organisms. Lesson 1: Earthquakes and Plate Boundaries  Most earthquakes occur at plate boundaries when rocks break and move along faults. Lesson 2: Earthquakes and Seismic Waves  Earthquakes cause seismic waves that provid ...
Tracing rays through the Earth
Tracing rays through the Earth

... - local velocity-depth distribution under a particular network - spherical symmetry not perfectly valid due to Earth’s ellipticity Travel times can be classified as “early” or “late” depending on whether the wave passes through a “slow” or “fast” region On global scale, anomalies interpreted in term ...
CLS Optical Metrology Facility
CLS Optical Metrology Facility

... the length of the surface. Typically three tangential and three sagittal slope profiles are acquired for a complete measurement of an optical surface. The FI measures the height map of the optical surface component. The radius of curvature and slope error can then be calculated from this surface hei ...
CLS Optical Metrology Facility - Overview
CLS Optical Metrology Facility - Overview

... the length of the surface. Typically three tangential and three sagittal slope profiles are acquired for a complete measurement of an optical surface. The FI measures the height map of the optical surface component. The radius of curvature and slope error can then be calculated from this surface hei ...
Midterm Review 2
Midterm Review 2

... petrology, and stratigraphy Types of sedimentary rocks are divided into clastic, biologic and chemical Sedimentary rocks commonly form distinctive layers at the surface of the Earth Sedimentary rocks are classified by composition and texture The most common sedimentary rocks are the siliciclastics, ...
Physical and biological response of the Arabian Sea to
Physical and biological response of the Arabian Sea to

... Pudov, 1992; Sadhuram, 2004). Price (1981) attributed this right-side bias of SST reduction to nonlinear mixed-layer current response and the stronger winds located on the right side of the storm track due to storm motion. In the present study even after the passage of cyclone Phyan, the cooling of ...
Earthquake - SchoolNova
Earthquake - SchoolNova

... displacement of the ground produced by the sudden release of energy.  Rocks under stress accumulate strain energy over time.  Stress results from tectonic plate movement, magmatic or volcanic activity.  When stress exceeds strength of rocks, rock breaks and slips.  Rock slippage/rupture occurs a ...
PLATE BOUNDARIES LAB - Science with Ms. Crownhart
PLATE BOUNDARIES LAB - Science with Ms. Crownhart

... 23. What Plate is the island of Madagascar part of? ______________________________ 24. How many miles long is Madagascar from top to bottom (use ruler)?___________________________ 25. Is the State of Hawaii near any plate boundary? _______________ a. Can you think of an explanation of why that volca ...
384. Assessing the Social Impacts of Changes in Fisheries Policy
384. Assessing the Social Impacts of Changes in Fisheries Policy

...  Some fishers may go out fishing for a few hours; others for up to 50 days on the ocean in a single trip • How to get them in same room at same time? Should you even try? ...
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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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