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Document
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... • Chemical composition (atomic weight of the elements that make up the substance) Atomic weight = the number of protons plus neutrons in an element ...
Geologic Time Scale - CVHS Chicklas
Geologic Time Scale - CVHS Chicklas

... • 20,000 years ago climate began to warm. • Modern humans-Homo sapiens evolved as early as 100,000 years ago. 12,000-15,000 humans had migrated around the world. • Mammals, flowering plants and insects dominate ...
Chapter 7 Answers
Chapter 7 Answers

... 1. Scientists think of the Earth’s layers in terms of composition and physical properties. 2. The 3 layers of the Earth from the exterior to the interior of the Earth are the Crust, the Mantle, and the Core. 3. The crust is the thinnest and outermost layer of the Earth which totals less than 1% of t ...
The History of Life
The History of Life

... Relative dating  If the rock layers have ...
Unit 1:
Unit 1:

... 1. What role did density have in forming the layers on the Earth? 2. How do the three main types of rocks differ in the way that they were formed? 3. How do relative and absolute dating differ? 4. How are ice cores used to tell stories of Earth’s past? 5. How are index fossils used to date rocks? 6. ...
Geologic Time Scale
Geologic Time Scale

... • 20,000 years ago climate began to warm. • Modern humans-Homo sapiens evolved as early as 100,000 years ago. 12,000-15,000 humans had migrated around the world. • Mammals, flowering plants and insects dominate ...
PLATE BOUNDARY
PLATE BOUNDARY

... *PLATE BOUNDARIES* (mark where two different plates meet) ...
Introduction to Plate Tectonics via Google Earth
Introduction to Plate Tectonics via Google Earth

... Laurel Goodell February 2013 ...
word doc leoce study guide with answers
word doc leoce study guide with answers

Introduction to Plate Tectonics via Google Earth
Introduction to Plate Tectonics via Google Earth

... Laurel Goodell February 2013 ...
Plate Tectonics
Plate Tectonics

... Fossils, rocks, glaciers, and the bottom of the ocean all revealed a past that did not reflect the current conditions on earth. But what did that mean? Let’s review what scientists found and then look at their conclusion. ...
(composed of the continental crust and oceanic crust).
(composed of the continental crust and oceanic crust).

... Geologists use the term lithosphere to mean an outer Earth zone, or shell, of rigid, brittle rock. It includes not only the crust, but also the cooler, upper part of the mantle that is composed of brittle rock. The rigid, brittle lithosphere rests on top of a soft, plastic underlayer named the asthe ...
Word format - University of Idaho
Word format - University of Idaho

... The father of modern geology, James Hutton, hypothesized that the Earth was much older than had previously been suggested. He promoted a concept called the Principle of Uniformitarianism, which essentially states: A. the present is the key to the past B. the past is the key to the future C. the past ...
Physical Geography
Physical Geography

... When sea plates pull apart leaving a rift, or deep crack. Magma wells up between the two plates to make underwater volcanoes and ridges. ...
Volcano Intro ppt
Volcano Intro ppt

... Earth’s Energy Budget • Solar radiation: 50,000 times greater than all other energy sources; primarily affects the atmosphere and oceans, but can cause changes in the solid earth through momentum transfer from the outer fluid envelope to the interior • Radioactive decay: 238U, 235U, 232Th, 40K, and ...
Changes to Earth`s Surface Chapter 9
Changes to Earth`s Surface Chapter 9

... sediment from the river will be carried onto land. The water will eventually go down but the sediment remains. This is also deposition. ...
Review II for Making a Habitable Earth and Plate Tectonics Units
Review II for Making a Habitable Earth and Plate Tectonics Units

... 7.) The carbon cycle sheet indicates that the reservoir of carbon in the atmosphere is 800 petagrams. Each year the amount of carbon entering the atmospheric carbon domain is, in petagrams, 60 from plant respiration, 60 from microbial respiration and decomposition, 90 from the ocean surface, and 4fr ...
Plate: a rigid slab of solid lithosphere rock that has defined
Plate: a rigid slab of solid lithosphere rock that has defined

... a rigid slab of solid lithosphere rock that has defined boundaries and floats on the denser rocks of the asthenosphere a point on the earth’s surface where strong upward convection currents or plumes of hot magma in the upper mantle push up below the plates of the lithosphere causing volcanic ...
File - Paxson Science
File - Paxson Science

... Instructions: For each of the questions or prompts below, give a complete answer for all parts. Answer on a separate piece of paper! Since we do not have a Cambridge textbook for this course you will need to do a little research to find your answers. Use our textbook’s glossary, internet sources, an ...
Seismology A shaky science
Seismology A shaky science

... A shaky science Students know why and how earthquakes occur and the scales used to measure their intensity and magnitude. State Standard 3d ...
Guided Notes for Forces Within Earth
Guided Notes for Forces Within Earth

... deformation. This type of strain produces permanent deformation, which means that the material is deformed even if the stress is reduced to zero. ...
Layer - cohort6science
Layer - cohort6science

... Notes on the Layers of the Earth: Draw this graph to help with your studying- ...
Name: Date: General Review Study Guide According to Wegener`s
Name: Date: General Review Study Guide According to Wegener`s

... An aftershock can cause damage days or months after a large earthquake. A fold in rock that bends upward into an arch is called an anticline. A large area of flat land elevated high above sea level is called a plateau. The point beneath Earth’s surface where rock breaks under stress and triggers an ...
Notes: The Theory of Plate Tectonics
Notes: The Theory of Plate Tectonics

...  Continental Drift Theory provided answers to some big mysteries. Like…  The apparent ______________ fit of the ____________. This had been noticed since the early days of map-making.  And … The presence of identical ________ on widely __________ continents belonging to organisms that could not h ...
PDF sample - OYR Raiders Ice Hockey
PDF sample - OYR Raiders Ice Hockey

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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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