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STATION 1: EARTH`S INTERIOR 1. Pressure occurs – remain here 2
STATION 1: EARTH`S INTERIOR 1. Pressure occurs – remain here 2

... 1. Water washes away layers – go to MOUNTAINS 2. Sediments form – go to SOIL 3. Ice melts carrying rocks – remain here 4. Floodwater causes silt from river to be deposited on flood plain – go to SOIL 5. Silt washed into ocean – go to OCEAN 6. Sediments under pressure – go to EARTH’S INTERIOR ...
Solutions
Solutions

... The oldest homo sapiens fossils are 195,000 years old. 24 hours = 4.55 billion years, so 195,000 years/4.55 billion years × 24 hours × 60 minutes × 60 seconds= 0.15 seconds. Subtracting this from 24:00:00 gives 23:59:45. 2. How do carbon isotope measurements in rocks provide evidence for the existen ...
New Title - Geneva Area City Schools
New Title - Geneva Area City Schools

Environmental Science Chapter 3 Section 1
Environmental Science Chapter 3 Section 1

... * 4 Parts: geosphere (rock), the atmosphere (air), the hydrosphere (water), and the biosphere (living things) * geosphere (rock) = solid part of the Earth including all rock, as well as the soils and loose rocks on Earth’s surface (12,756 km = 7+ mi) * atmosphere (air) = mixture of gases that makes ...
REGIONAL GEOLOGY AND MINERALIZATION
REGIONAL GEOLOGY AND MINERALIZATION

review packet
review packet

... proportion of these unstable elements gradually decreases over time as they decay into other materials in a predictable way. Scientists use the rate at which such unstable elements decay to determine when the fossils or minerals formed. The technique described above is known as as A. the law of esti ...
Seafloor Spreading - Paramus Public Schools
Seafloor Spreading - Paramus Public Schools

... 2. When hardens adds new ocean floor 3. As spreading occurs, more magma is forced upward and the crust moves away from ridge 4. Crust is destroyed by subduction at trenches ...
The History of the Earth
The History of the Earth

... Melody, Loren, Rosie, Austin, Nicki and Addison learned that there are four layers that make up the earth. We live on the crust. The core is too hot and too deep to get to. ...
Study of oxygen fugacity influence on redox state of iron in
Study of oxygen fugacity influence on redox state of iron in

The Hadean Eon
The Hadean Eon

... • Proto-sun forms from hydrogen gas. • Dust particles condense, begin to clump. • Proto-sun becomes dense enough to begin hydrogen fusion. • Jupiter forms early and grows quickly. • Remaining planets form from leftovers. ...
Plate Tectonics - Awtrey Middle School
Plate Tectonics - Awtrey Middle School

... Evidence that Pangaea existed 1. Continents fit together like puzzle pieces (mountain ranges lined up) 2. Mesosaurus – Reptile fossil found on South America and Africa – It couldn’t swim! 3. Glossopteris – Tropical plant fossil that was found in Antarctica! ...
PT Dir Rdg
PT Dir Rdg

... 2. continental crust b. dense crust made of rock that is rich in iron and magnesium 3. tectonic plates c. blocks of Earth’s shell that ride on a deformable layer of the mantle 4. lithosphere d. solid, plastic layer of the mantle beneath the lithosphere 5. asthenosphere e. low-density crust made of r ...
Earth Science Text Assignments
Earth Science Text Assignments

... 9. What do scientists record and study to learn about the interior from these events? Scientists study these seismic waves and the speed of them reveals the structure of the planet. 10. What characteristics of these events, specifically, do they rely on? Scientists rely on the speed of the waves. 11 ...
File
File

... ________________ 6. Earth’s molten liquid layer found between the inner core and the mantle. ________________ 7. The thin outer layer of Earth that can be compared to an egg shell or an apple skin; this is also where life is found on Earth. ________________8. Largest layer of the Earth’s interior st ...
crust, mantle, outer core, inner core
crust, mantle, outer core, inner core

... Crater ...
File
File

... Metamorphic rocks whose minerals are arranged in layers or bands are called— A. unfoliated B. nonclastic C. clastic D. foliated Heat and pressure can transform igneous rock into metamorphic rock. What processes can transform igneous rock into sedimentary rock? A. heat and pressure B. rifting and sub ...
PHS 111 Test 1 Review Answers Chapters 20-22
PHS 111 Test 1 Review Answers Chapters 20-22

... The crustal surface and the uppermost part of the mantle is called the: asthenosphere; lithosphere; mohorovicic; centrosphere. Earth's core is probably composed of: silicate minerals; aluminum oxides; ...
Teacher`s Guide - Discovery Education
Teacher`s Guide - Discovery Education

4. Seafloor Spreading Notes
4. Seafloor Spreading Notes

... • Earth’s magnetic field has reversed many times since its creation ...
Supporting the theory of Plate tectonics
Supporting the theory of Plate tectonics

oceans
oceans

... expanded into space • Matter clumped and planets formed 5 bya • Early on our planet is a hard rock being bombarded by other planetary bodies and experiencing volcanic eruptions ...
Chapter 5 Fast Changes on Earth
Chapter 5 Fast Changes on Earth

... Twenty of the following questions will appear on the test. Each question will be worth 4 points. In addition, 8 questions, from prior chapter tests, will be on the test. Each of these questions will be worth 1 point. A. Crater D. floods G. mudslide J. Volcano B. Earthquake E. hot spot H. plates C. F ...
Mountain Building
Mountain Building

... – Rocks deeper within the Earth are warm and more ductile. They will tend to fold (bend) ...
Unit 1 Ch. 3 Intro to env Science
Unit 1 Ch. 3 Intro to env Science

... Air Pressure – atmosphere more dense near surface due to gravity ...
Read the following about the layers of the Earth and answer the
Read the following about the layers of the Earth and answer the

... of Earth? If we could travel through the layers of the Earth, what would our trip be like? In order to make this trip, we would need a special vehicle that could travel through both liquid and solid rock and that could withstand intense temperature and pressure changes! The deeper into the center of ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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