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Annenberg Learner: Plate Tectonics Web Quest Name: Blk:
Annenberg Learner: Plate Tectonics Web Quest Name: Blk:

... 2) Please read information on PLATE TECTONICS A) Who was Alfred Wegener? B) His theory was based upon what 3 pieces of evidence? C) What were 3 pieces of information that were published in Wegener's book? 3) "Continents On the Move" ~ please use the CHART & BULLET 2 FACTS for each time period noted. ...
Document
Document

... arrows. Which type of stress is being illustrated? ...
Use the following list to match to the statements below: Seismic
Use the following list to match to the statements below: Seismic

... and one is forced beneath another, are known as ________________ plate boundaries. ANS: Convergent 7. Highly active earthquake zones form where tectonic plates slip past one another. This type of tectonic boundary is known as ________________. ANS: Transform 8. Where does the energy that moves tecto ...
Chapter_1_Revised - Earth and Space Science GIS and stuff
Chapter_1_Revised - Earth and Space Science GIS and stuff

... surface absorbs, called insolation, varies with latitude, producing a temperature gradient between the poles and equator. The resulting atmospheric and oceanic circulation produces substantial pole-ward transfer of heat that delivers warm air and water to higher latitudes. Because Earth’s total heat ...
Chapter 2: Rocks of the Midwestern US
Chapter 2: Rocks of the Midwestern US

... Igneous rocks form from the cooling of magma (molten rock underground) or lava (molten rock at the Earth’s surface). When magma cools slowly underground, it has time to produce large crystals that are visible to the naked eye. Rocks that form in this manner, such as granite, are called plutonic. Mol ...
Minerals and Rocks packet
Minerals and Rocks packet

... 14. Has 1 silicon atom surrounded by 4 oxygen atoms. 15. __________ rocks are the result of the weathering process on earth. ...
Lecture 8: Igneous Petrogenesis
Lecture 8: Igneous Petrogenesis

... (MORB) and a plume basalt normalized to primitive mantle. ...
FOSS Earth History, Second Edition Glossary abrasion
FOSS Earth History, Second Edition Glossary abrasion

... erratic a rock that is different from the type of rock found in its current location (SRB) extinct in terms of volcanoes, a volcano that is not expected to erupt again (IG) extremophiles organisms that live in extreme conditions such as acidic, boiling, or freezing (SRB) extrusive outside the earth; ...
ConceptTest compilation
ConceptTest compilation

... The characteristics of four planets are listed below. Which planet is most likely to be classified as Jovian? a. Mainly rocky, volcanism, low gravity. b. Mainly rocky, no volcanism, high gravity. c. Mainly gaseous, volcanism, low gravity. d. Mainly gaseous, no volcanism, high gravity. It takes 24 ho ...
Earth Materials
Earth Materials

... Density Each rnineral has a specific densiW or a small range of densities-for those minerals that vary in mineral composition. Often in mineral studies, density is stated as specific gravity, a value without units. Specific gravity is the density of a mineral compared to the density of water. Specif ...
Unit 6.3 PowerPoint File
Unit 6.3 PowerPoint File

... apart over millions of years • Pangaea the supercontinent that formed 300 million years ago and that began to break up beginning 200 million years ago • Panthalassa the single, large ocean that covered Earth’s surface during the time the supercontinent Pangaea existed ...
Metamorphic Rocks
Metamorphic Rocks

... Composition of the Parent Rock •Composition may remain the same or change during metamorphism depending upon the parent rock’s composition and whether new chemicals are added during the process. ...
Poster NGC 2013 Transitional I-S type characteristics in the Main
Poster NGC 2013 Transitional I-S type characteristics in the Main

... Bentong‒Raub suture zone was previously regarded exclusively as S–type granite. Among the S-type characteristics of the granite are, (a) high initial 87Sr/86Sr isotope ratio > 0.710, (b) low Na2O content, < 3.2% Na2O in rocks with ~ 5% K2O, (c) narrow range of felsic rock (SiO2: 65.95 to 77.4%), (d) ...
Terrestrial planets fractionated synchronously
Terrestrial planets fractionated synchronously

... vigorous than Earth’s but to have almost no horizontal effect at the surface, which instead they deform vertically. Extremely active Venusian plumes have dynamically maintained precisely the same topography for a half-billion years. On Mars, plumes generate long-term volcanism, mostly in one region, ...
Chapter 3. Archean Crustal Provinces
Chapter 3. Archean Crustal Provinces

... Two opposing schools of thought: (1) Uniformitarian - The plate tectonics functions all the time on the Earth; there is no exception for the Precambrian. (2) Non- uniformitarian - The early lithosphere was too warm and too soft to subduct, the “plates” were likely small and thin; they were pushed an ...
America`s Explosive Park
America`s Explosive Park

... Though Yellowstone could erupt again someday, there is no evidence that the caldera is readying for another massive blast, says Smith. That outlook is shared by Jake Lowenstern, the U.S. Geological Survey's lead geologist at the Yellowstone Volcano Observatory. Volcanologists with the U.S. Geologic ...
Plate Tectonics
Plate Tectonics

... Evidences For Plate Tectonics • Earthquakes and Volcanoes • It has been long observed that earthquakes and volcanoes DO NOT occur randomly on Earth’s surface. • Instead, they tend to occur in specific belts. • These belts just happen to be location of the boundaries between the plates. • These boun ...
layers of the earth
layers of the earth

... B. because they are made up of more dense materials than a core. C. because we already used the words core and mantle. D. because they are the thinnest and are on the outside of the earth. E. Other______________________________________________ ...
seismic waves - Gordon State College
seismic waves - Gordon State College

... the roots of the mountain are heavier than the mountain at the surface. mountains sink until the upward buoyant force balances the downward gravitational force. mantle rock is weak beneath the mountain. oceanic crust is thin. ...
Library List - the Helena Mineral Society
Library List - the Helena Mineral Society

... “And There’s Opals Out There” by Ed Waller “The Opal Book” by Frank Leechman (a complete guide to the famous gemstone) “Southwestern Turquoise-The Indians’ Sky Stone” by Lee Hammons – director Arizona Mineral Museum “Turquoise Deposits of Nevada” Nevada Bureau of Mines by Frank R. Morrissey “Blue Go ...
Powerpoint Presentation (large file)
Powerpoint Presentation (large file)

... retrograde direction, with a period of only about 4 Earth days ...
Eastern Klamath Mountains - College of the Siskiyous
Eastern Klamath Mountains - College of the Siskiyous

Grade 4 Earth Science Unit (4.E.2.)
Grade 4 Earth Science Unit (4.E.2.)

... Activating Strategies: (Learners Mentally Active) Background for Teachers: Scientists have good evidence that Earth is very old, approximately four and one-half billion years old. Scientific measurements such as radiometric dating use the natural radioactivity of certain elements found in rocks to h ...
GY 111 Lecture Note Series Intrusive Igneous Rocks
GY 111 Lecture Note Series Intrusive Igneous Rocks

... Press, F. and Siever, R., 1986. Earth. W.H. Freeman, 656p. B) Intrusive igneous rocks that suck I have a fun relationship with all of the faculty in the Department of Earth Sciences. One of my best friends in the department is Dr. David Allison. He studies igneous and metamorphic rocks. I study sedi ...
Document
Document

... about 20 distinct “plates” (~ 100 km thick), or lithosphere which move relative to each other • This motion is what causes earthquakes and makes mountain ranges ...
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Age of the Earth



The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.
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