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Investigating Earth`s Interior
Investigating Earth`s Interior

... 6. What do you notice about temperature as you move from the outer layers towards the center? __Temperature increases as depth increases.________________________________________ 7. Pressure increases as you travel from the crust to the center of the Earth. This is a result of the weight of the rock ...
Sea Floor Spreading
Sea Floor Spreading

... xbfa4 ...
Expedition #7 - Commotion Beneath the Ocean
Expedition #7 - Commotion Beneath the Ocean

... Many of the figures in this worksheet and the online expedition are derived from "This Dynamic Earth" by Jacqueline Kious and Robert Tilling of the U.S. Geological Survey. ...
Lecture 27 April 3, 2006
Lecture 27 April 3, 2006

... What is EarthScope?EarthScope is a bold undertaking to apply modern observational, analytical and telecommunications technologies to investigate the structure and evolution of the North American continent and the physical processes controlling earthquakes and volcanic eruptions.EarthScope will prov ...
Plate Tectonic Outline Notes
Plate Tectonic Outline Notes

... I. ___________________________ – study of the movement of the plates of the Earth’s surface A. Lithosphere – _________________________________________________________ ...
Geology- Module 7
Geology- Module 7

... • Pangaea was the name of the land mass that existed approximately 240 million years ago. • Alfred Wegner first created continental drift theory which stated that the continents drifted apart from this land mass into their present day location. He used plant/animal fossil evidence to help support h ...
Volcanoes Vocabulary
Volcanoes Vocabulary

... An area of deep cracks that forms between two tectonic plates that are pulling away from each ...
Presentation
Presentation

... The Earth's Crust is like the skin of an apple. It is made of solid rock. The crust is only about 3-5 miles (8 kilometers) thick under the oceans and about 25 miles (32 kilometers) thick under the continents The temperatures of the crust vary from air temperature on top to about 1600 degrees F in th ...
#______ Parent Signature: Heading: The Earth`s Changing Surface
#______ Parent Signature: Heading: The Earth`s Changing Surface

... B. silicon, aluminum, calcium, sodium and potassium C. Mostly nickel and some iron D. oxygen, magnesium, iron, aluminum, and calcium ...
Earth Science Lecture - Quiz 1
Earth Science Lecture - Quiz 1

... b. using mathematics to confuse students c. defending personal ideas d. making observations and repeatedly testing conclusions 13. As of 2010, the current earth human population is approximately: a. 6.5 million c. 10 billion d. 5.6 billion b. 6.5 billion 14. An open system is defined as: a. An excha ...
PLATE TECTONIC THEORY TEST
PLATE TECTONIC THEORY TEST

... 3. Explain why the mantle has the ability to flow (4) ...
Inside the Earth
Inside the Earth

... Inner Core - Solid dense center. It is about 6,378 km beneath the surface. ...
The Earth`s Asthenosphere – Plasticity Lab
The Earth`s Asthenosphere – Plasticity Lab

... 2. In which phase of mater is the cornstarch? ___________________ 3. Which procedure in the activity could represent to the mantle under pressure? ...
Lesson Plan - GeographyPods
Lesson Plan - GeographyPods

... AIM : To understand that the earth is made up of layers To find out what happens on the surface layer OBJECTIVES By the end of the lesson(s) Pupils will know: That the earth is made up of four basic layers Pupils will understand: That the crust is split into sections, each section is called a plate. ...
Understanding the Earth
Understanding the Earth

... around core 3. Crust: thin layer of rocks and minerals that surrounds mantle ...
Chapter 22.1: Earth`s Structure
Chapter 22.1: Earth`s Structure

... 1. Compare how constructive and destructive forces affect Earth’s surface. 2. List the 3 layers of Earth. 3. Which layer has currents of moving rock? 4. Which is the most dense layer? 5. Which layer is made of light rocks like silicates? 6. Which is more dense: Continental or Oceanic ...
Continental Drift
Continental Drift

11/4 Convection Currents
11/4 Convection Currents

... Broken into many land masses called “plates” Continents are a part of these plates plates also include the seafloor ...
14 The History of Life
14 The History of Life

Unit 5 - mrhebert.org
Unit 5 - mrhebert.org

... • The crust is the top layer of the Earth • Below it is the mantle, which is made of rock material (upper part is solid, lower part is partly melted) • The upper mantle and crust are called the lithosphere • Below the mantle is the core • The outer core made up of mainly liquid iron and nickel … the ...
PDF file of Lecture 4a - Earth`s Interior and Tectonics
PDF file of Lecture 4a - Earth`s Interior and Tectonics

Earth`s Interior
Earth`s Interior

... Geologists are not able to travel to the center of Earth because the temperature is too hot and the pressure is too great. Geologists must relay on other evidence to study the Earth’s interior. Geologists study how seismic waves travel through the Earth to identify the layers of the Earth. Seismic w ...
Lecture 2: Dynamic Earth: Plate Tectonics
Lecture 2: Dynamic Earth: Plate Tectonics

... Earth is a dynamic planet The surface of the Earth is constantly changing. Going back a billion years, there were no Grand Canyon, Appalachian Mountains, or Himalayan Mountains. (Thick sedimentary rock accumulated as horizontal layers on an ocean floor are now folded and faulted to from the highest ...
Convection currents
Convection currents

... The Earth is composed of four different layers. -The crust is the layer that you live on, and it is the most widely studied and understood. -The mantle is much hotter and has the ability to flow. -The outer core and inner core are the inner most sections of the earth ...
Translate the text from English into Russian.
Translate the text from English into Russian.

... known on the basis of seismological evidence that the mantle is not in the liquid state. Laboratory experiments have shown, however, that when rock is subjected to the high temperatures and pressures believed to exist in the mantle, it can be deformed and flows very much like a liquid. The upper par ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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