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Plate Tectonics
Plate Tectonics

... The Earth’s outer core is liquid, melted iron and nickel (metals), which flows due to  convection and the rotation of the Earth. This flowing iron and nickel generates a  magnetic field around the Earth. This is a complicated process and we have  discovered Earth’s ​ magnetic field sometimes reverse ...
How Is Pacific Northwest Climate Changing? (PDF)
How Is Pacific Northwest Climate Changing? (PDF)

... Dalton, P.W. Mote, and A.K. Snover (eds.) Climate Change in the Northwest: Implications for Our Landscapes, Waters, and Communities, Washington D.C.: Island Press. Kunkel, K.E. et al., 2013. Part 6. Climate of the Northwest U.S., NOAA Technical Report NESDIS 142-6. Mote, P.W., 2003. Trends in temper ...
CSIR - National Institute of Oceanography
CSIR - National Institute of Oceanography

... cycling and fluxes. NIO has been studying benthos from different habitats. Their type, abundance and distribution are adversely affected by pollution and coastal disturbance. The ongoing deoxygenation and acidification make these organisms vulnerable to ...
Earthquakes - NewPathWorksheets.com
Earthquakes - NewPathWorksheets.com

... Earthquakes are measured by machines called seismographs. The different seismic waves are measured and recorded on a paper or drum (or as a computerized image) called a seismogram. The first up tick on a seismogram records the arrival of the P-waves. The next significant up tick is the arrival of th ...
Workshop Report
Workshop Report

... Ocean Acidification is now recognized as one of the greatest threats to Alaska’s marine ecosystems Recent observations in the Gulf of Alaska, Chukchi and Bering Seas (Yamamoto-Kawai et al., 2009; Bates et al., 2009; recent work of author Mathis and colleagues) suggest that acidification rates are hi ...
The California Current - Department of Marine and Coastal Sciences
The California Current - Department of Marine and Coastal Sciences

... • Cool water current ...
Scientific Ocean Drilling - Division on Earth and Life Studies
Scientific Ocean Drilling - Division on Earth and Life Studies

... beyond the timeframe that can be captured using instruments or ice cores. This record provides critical insights into conditions in Earth’s past, including when atmospheric carbon dioxide levels were similar to or higher than they are today—information that could help scientists understand how the E ...
Plate Tectonics
Plate Tectonics

... The 4 main features of plate tectonics are: • The Earth's crust is broken into a series of plates (crustal plates) or pieces. • These plates are continually, moving, spreading from the center, sinking at the edges, and being regenerated. • Convection currents beneath the plates move the crustal pla ...
EDT - OceanExplorer
EDT - OceanExplorer

... buoyant and continues to move upward towards the Earth’s surface. ...
How does thermal energy move around in the Earth?
How does thermal energy move around in the Earth?

... . On their maps, they will click once to start drawing a profile, and double-click to finish the profile line. An elevation profile of the line they defined will appear in the Elevation Profile tab. They can place their cursor on the elevation profile to view corresponding points along the profile l ...
Lecture 10: Ocean Circulation Basic Ocean Current
Lecture 10: Ocean Circulation Basic Ocean Current

... (from Oceanography by Tom Garrison) (Figure from The Earth System) ESS228 Prof. Jin-Yi Yu ...
Climate Zones - Lourdes Academy
Climate Zones - Lourdes Academy

... Climate and Altitude • Higher the altitude - cooler the climate.  • Precipitation–the falling of moisture such as rain or snow.  • Adiabatic cooling - As the air rises over mountains, it cools and drops its moisture. ...
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... Focus - the point underground where the rocks breaks and the earthquake begins; usually located at a depth of less than 100km (60 miles). Epicenter - point on the surface DIRECTLY above the focus. Surface waves travel out from the epicenter. Primary (P) Waves - travel the fastest of the three waves ...
Career Pathways in the Geosciences
Career Pathways in the Geosciences

... Hydrologists are concerned with water from the moment of precipitation until it evaporates into the atmosphere or is discharged into the ocean; for example, they study river systems to predict the impacts of flooding. Marine geologists investigate the ocean-floor and ocean-continent boundaries; they ...
Plate Tectonics
Plate Tectonics

... Why is it difficult to determine Earth’s inner structure? How are seismic waves used to provide evidence about Earth’s interior? List Earth’s three main layers What is the difference between the lithosphere and the asthenosphere? In which layer is each located? ...
Dynamic Earth
Dynamic Earth

... -fossils of tropical plants found in continents now in polar regions -fossils of the same species found across oceans ...
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sxES_G6_RNG_ch04-A_070-073.fm

... a. Some continents match up like jigsaw puzzle pieces. b. Different rock structures are found on different continents. c. Fossils of tropical plants are found near the equator. d. Continental glaciers once covered South Africa. ...
The inside of the Earth
The inside of the Earth

... – Similar to CAT scans, which look inside people ...
Slide 1
Slide 1

... a. continents were once joined b. the Earth was about 6000 years old c. there was no evidence to suggest that the Earth was changing d. all rocks on Earth were of the same age ...
Chapter 8: Volcanoes The Big Idea: Volcanoes form as a result of
Chapter 8: Volcanoes The Big Idea: Volcanoes form as a result of

... The Big Idea: Volcanoes form as a result of tectonic plate motions and occur where magma reaches Earth’s surface. ...
When the Earth Moves: Seafloor Spreading and Plate Tectonics
When the Earth Moves: Seafloor Spreading and Plate Tectonics

... rock—magma—was welling up from below the crust. From this hint of a mechanism that could explain the midocean ridges, Hess developed a new synthesis of earth science in his well-known 1962 paper, “The History of Ocean Basins.” Although he characterized the essay as “geopoetry,” as if to warn other s ...
Study of frontal zones in the crozet-kerguelen region
Study of frontal zones in the crozet-kerguelen region

... temperature increases from 4 to 14°C and salinity from 34.0 to 35.3°/00 over a distance of only about 100 miles. South of the zone, therefore, and identifted on the surface by the thermal front, the Antarctic Convergence is marked by the sinking of isotherms and the deepening of the salinity minimum ...
Chapter 5 Fast Changes on Earth: Earthquakes
Chapter 5 Fast Changes on Earth: Earthquakes

... A tsunami is a giant wave caused by an earthquake on the ocean floor. Supporting Detail 1. A tsunami is a giant ocean wave a. Usually caused by an earthquake on the ocean floor b. some caused by underwater landslides or volcanoes 2. The force of the earthquake causes a large wave to form 3. As the w ...
Background Information for Plate Tectonics Rock Formation
Background Information for Plate Tectonics Rock Formation

... up the lower asthenosphere. This materials becomes less dense than the material above it and it starts to rise. Gravity pulls the cooler material down towards the core. Because the lower mantle and lithosphere are solid the asthenosphere continuously flows up and down. 4. These convection currents i ...
Forsyth, D.W., Lay, T., Aster, R.C., and Romanowicz, B. (2009). Grand challenges for seismology
Forsyth, D.W., Lay, T., Aster, R.C., and Romanowicz, B. (2009). 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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