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Ocean Basins - University of Washington
Ocean Basins - University of Washington

... continental and oceanic plates move in same direction at same speed examples – margins around Atlantic Ocean contain: coastal plain (was continental shelf during higher sea level) broad continental shelf continental slope and rise Collision margins continental and oceanic plates move toward each oth ...
179 Core Idea ESS2 Earth`s Systems ESS2.A: EARTH MATERIALS
179 Core Idea ESS2 Earth`s Systems ESS2.A: EARTH MATERIALS

... By the end of grade 5. Earth’s major systems are the geosphere (solid and molten rock, soil, and sediments), the hydrosphere (water and ice), the atmosphere (air), and the biosphere (living things, including humans). These systems interact in multiple ways to affect Earth’s surface materials and pro ...
powerpoint_6.1_Volacanoes_and_Plate_Tectonics
powerpoint_6.1_Volacanoes_and_Plate_Tectonics

... • Most occur along diverging boundaries such as the mid-ocean ridge or in subduction zones. ...
Plate Boundaries foldable
Plate Boundaries foldable

... circular motion, the hot magma rises, cools, then falls back down to the core. This movement causes tectonic plates to meet at plate boundaries . ...
Plate Tectonics
Plate Tectonics

... the subduction is interrupted. • Because the continental crust is made of low density material, it does not sink. • The crust moves upward, folds and buckles and ...
Convection Currents
Convection Currents

... Dense things sink and light things float. ...
Wealth from the Oceans: Use, Stewardship, and Security
Wealth from the Oceans: Use, Stewardship, and Security

... rank for wealth from the oceans with a surprising stewardship and security. 42 percent of the market activity and displaced Because pumping exploded from third to first feeding and lodging as the largest activity. Feedplace from 2002 to 2010, images of offshore plating and lodging receded only a lit ...
origin of tsunami
origin of tsunami

... preceded by another natural hazard – the earthquakes. More than 230,000 lives have been lost in the tsunami 2004 in the 11 stricken countries around the Indian Ocean, which include Indonesia, Sri Lanka, Thailand, India, Maldives, and Somalia. ...
1 Years of the Maritime Continent (YMC) (2017-2019)
1 Years of the Maritime Continent (YMC) (2017-2019)

... - Observing the weather-climate system of Earth’s largest archipelago to improve understanding and prediction of its local variability and global impact Executive Summary The Maritime Continent (MC), a unique mixture of land and ocean straddling the equator between the Indian and Pacific Oceans, is ...
GLY 3171 Geomorphology of the United States Course Description
GLY 3171 Geomorphology of the United States Course Description

... processes and agents that form and fashion land forms, the examination of the present day status of the concept of land evolution to an understanding of the significant landforms of the United States, and the study of the most significant areas of the United States such as the Appalachian highlands, ...
so, where would you predict the highest primary productivity?
so, where would you predict the highest primary productivity?

... available = high productivity (“spring bloom”)  summer: solar radiation available, but nutrients cut-off by seasonal thermocline (doorway closed)  fall: break-down of thermocline = renewed productivity ...
Name____________________________
Name____________________________

... 6. When two plates meet, this is called a ______________________ boundary. 7. Deep canyons where one plate slides under another are called __________________. 8. When two plates slide past each other this is a _______________________ boundary. 9. A _____ ______ is a place where magma works its way ...
summing-up - Zanichelli online per la scuola
summing-up - Zanichelli online per la scuola

... floor of the oceans is not flat and uniform, but has two types of structures of dimensional importance: – the oceanic ridges that constitute a ...
platetectonics
platetectonics

... • the collision between the Eurasian Plate and the Indian Plate that is forming the Himalayas. • northern part of the Pacific Plate and the NW North American Plate that is forming the Aleutian Islands. • the Nazca Plate beneath the South American Plate to form the Andes. • the Pacific Plate beneath ...
Exam 2a – GEOL 1113 Fall 2009
Exam 2a – GEOL 1113 Fall 2009

... _____ 41. A _____ is the first wave to arrive at a recording station following an earthquake. a. Love wave b. Rayleigh wave c. S-wave d. P-wave e. surface wave _____ 42. A single seismometer can determine both distance and direction to the focus of an earthquake. True (T) False (F) _____ 43. A seism ...
EARTH/ENVIRONMENTAL SCIENCE REVIEW GUIDE – ANSWERS!!!
EARTH/ENVIRONMENTAL SCIENCE REVIEW GUIDE – ANSWERS!!!

... 12. Explain how the tilt of Earth’s axis results in seasons. The tilt of Earth’s axis cause seasons by moderating the amount of sunlight that hits the northern and southern hemispheres at different times of the year. For example, in northern hemisphere summer, the northern hemisphere is tilted towar ...
Name Student ID Exam 2c – GEOL 1113 Fall 2009 ____
Name Student ID Exam 2c – GEOL 1113 Fall 2009 ____

... _____ 51. Pelagic sediment is mainly derived from the land and is deposited on the abyssal plains by bottom currents. (T or F) _____ 52. Oceanic trenches: a. are found along all continental margins. b. are typically 8-10 km deep. c. were eroded by rivers during the Ice Ages when sea-level was lower ...
Name Student ID Exam 2b – GEOL 1113 Fall 2009 ____
Name Student ID Exam 2b – GEOL 1113 Fall 2009 ____

... _____ 32. A Benioff earthquake zone is significant in plate tectonic theory because it a. locates rift valleys on continents b. coincides with mid-oceanic ridges c. traces the descent of a sea-floor slab subducting into an oceanic trench or under a continent d. may predict quake locations under tran ...
L03 - D4 - Teacher - Processes of Plate Tectonics
L03 - D4 - Teacher - Processes of Plate Tectonics

... ) – Two plates move towards each other. At the area of collision, one plate is goes down and the other is pushed up. This is dependent on density and thickness of the plates. The collision forms a long trench which can be 8 to 10 km ...
COASTAL PROCESSES
COASTAL PROCESSES

... This is because larger waves have more powerful backwash than the smaller waves that plunges over when breaking. This erodes the coast faster. ...
Introduction to Earthquakes and Seismology
Introduction to Earthquakes and Seismology

... mechanism- weight is freely suspended from a support imbedded in bedrock, weight is attached to a pen and when an earth quake hits, the weight will remain stationary while the frame/support shakes with the earth, the support is connected to a rotating drum with paper on it, and the relative intensit ...
How do ocean plates interact with each other?
How do ocean plates interact with each other?

... plates. Look at the Continental plate. It is made up of the same amount of material, has roughly the same area, but is much thicker. What can you say about the physical properties of the Continental plate? ...
Plate Tectonics
Plate Tectonics

... indicates that the core is mostly composed of iron with less amounts of nickel and other elements. The core is subdivided into the inner and outer core based on differences in mechanical strength. Whereas the outer core is liquid and capable of flow, the inner core is stronger and behaves like a sol ...
Chap 3 marine zones
Chap 3 marine zones

... pointed upward, which helps them catch the scraps of food that fall from shallower waters. ...
Grand Challenges for Seismology
Grand Challenges for Seismology

... role in the dynamics of Earth’s deep interior. How are Earth’s internal boundaries affected by dynamics? Internal boundaries in Earth (and other planets) are associated with the primary compositional layering that resulted from the chemical differentiation of the planet and with mineralogical phase ...
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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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