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Changing Earth`s Surface
Changing Earth`s Surface

... _________________: A layer of molten iron and nickel that surrounds the inner core of Earth. _________________: The material that forms Earth’s hard surface. _________________: The study of the solid Earth _________________: A rigid layer made up of the uppermost part of the mantle and the crust. __ ...
Earth Interior quest
Earth Interior quest

... 13. Where and what are the convection currents? (p.17) Read this section. 14. How hot is the inner core? 15. What does melting point mean? 16. If the temperature of material is hotter than the melting point what should happen to it? 17. What is the outer core made of? What is the inner core made of? ...
Plate Tectonics
Plate Tectonics

... Plates move ______from each other along _______boundaries Plates ______along a ________boundary Plates _____past each other along _____fault boundaries  These plate movements have produced _____of ...
Lecture presentation - NAU jan.ucc.nau.edu web server
Lecture presentation - NAU jan.ucc.nau.edu web server

... • P waves are always faster than S waves • Wave velocity increases with density and stiffness • Passing from one material to another causes waves to refract (bend) ...
Continental Drift and Sea-Floor Spreading 7.2
Continental Drift and Sea-Floor Spreading 7.2

... 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! ...
Geodynamics
Geodynamics

... Studies of the Earth's Deep Interior (CSEDI). Funding will support basic research on the character and dynamics of the Earth's mantle and core, their influence on the evolution of the Earth as a whole, and on processes operating within the deep interior that affect or are expressed on the Earth's su ...
What are the Layers of the Earth?
What are the Layers of the Earth?

... on the ocean floors. The lithosphere is the outer solid portion of the Earth that includes the crust and the uppermost part of the mantle. The lithosphere has an average depth of 100 km. 2. Lower Mantle and Core : Directly below the lithosphere is the asthenosphere, a region of the mantle with a pla ...
Lecture09
Lecture09

... Consumed CO2 and gave off O2 Photosynthesis ...
- Google Sites
- Google Sites

... 12. Who is responsible for the theory of natural selection, and explain what natural selection is. Charles Darwin. It states that organisms that are best suited to their environment will survive and produce the most offspring, carrying on those “strong” traits. 13. What major event marks the ends of ...
third quarter - New Haven Science
third quarter - New Haven Science

... 1. Earth’s surface features, such as mountains, volcanoes and continents, are the constantlychanging result of dynamic processes and forces at work inside the Earth. 2. Earth is formed of three basic layers, with the densest being the iron and nickel core. The middle layer, the mantle, of the Earth ...
THIRD QUARTER II. UNIT 5: PLATE TECTONICS Time
THIRD QUARTER II. UNIT 5: PLATE TECTONICS Time

... 1. Earth’s surface features, such as mountains, volcanoes and continents, are the constantlychanging result of dynamic processes and forces at work inside the Earth. 2. Earth is formed of three basic layers, with the densest being the iron and nickel core. The middle layer, the mantle, of the Earth ...
Earth`s Interior Reading Packet 1
Earth`s Interior Reading Packet 1

... fE-'a, he rocks, soil, and water you can see on the ffi earths surface make up only a tiny fraction of the &- total mass and volume of the earth' What is the earth like below its surface? What makes up the interior of our planet? At one time, some people thought the earth might be hollow. They imagi ...
File
File

... • From seismic and other geophysical evidence and laboratory experiments, scientists agree with the theory that the plate-driving force is the slow movement of hot, softened mantle that lies below the rigid plates • Below the lithospheric plates, at some depth the mantle is partially molten and can ...
Chapter 21- Planet Earth
Chapter 21- Planet Earth

... the theory that explains how the outer parts of Earth ______________________________, and that explains the relationships between _______________________________, sea-floor spreading, ____________________________, and volcanic activity ...
The Earth February 7 − Why does Earth support life?
The Earth February 7 − Why does Earth support life?

... • Incoming sunlight passes through atmosphere. • Absorbed by ground. • Re-emitted as infra-red radiation. • CO2 gas causes atmosphere to be opaque to infra-red light. • Infrared light is trapped, so heats surface. ...
The Earth`s Interior Structure Reading
The Earth`s Interior Structure Reading

... for the gravitational constant (known from experiments). Because the Earth exerts a certain force on a body (like you) with a certain mass m1 on the Earth’s surface, some 6400 km from its center, the known values can be substituted into the equation and the mass of the Earth (m2) can be calculated. ...
List 1 - arbuthnotbraingame
List 1 - arbuthnotbraingame

... and Mesozoic eras about 250 million years ago, before the component continents were separated into their current configuration.[2] • The name was coined in the scientific discussion of Alfred Wegener's theory of the Continental drift. In his book "The Origin of Continents and Oceans" (Die Entstehung ...
formation of Plate tectonic theory
formation of Plate tectonic theory

... Plate Tectonic theory is one of the eight greatest scientific discoveries of all time. Most recently discovered (first presented in the late 1960’s) Today most geoscientists take plate tectonic theory for granted. To get there was in fact a 100 year scientific journey involving many different scient ...
Accretion and Differentiation of Earth
Accretion and Differentiation of Earth

... of the core relative to the entropy of the same liquid material at melting point & and 1 bar. • Corresponds to about 1000K for present Earth, may have been as much as 2000K for early Earth. • It is diagnostic of core formation process...it ...
Changing Earth
Changing Earth

... methods has been used to produce estimates of the major geological events in the history of the earth. We call this the geological time scale. The time scale is hierarchical, with eons divided into eras, eras divided into periods, and periods divided into ...
Part A: Modeling Shadow Zones The structure of the Earth consists
Part A: Modeling Shadow Zones The structure of the Earth consists

... Surrounding this is the outer core, a 2,000 km thick layer of iron, nickel, and small quantities of other metals. Lower pressure than the inner core means the metal here is fluid. Differences in temperature, pressure and composition within the outer core cause convection currents in the molten metal ...
Chapter 3
Chapter 3

... • Less than 1% of all water on the Earth. • Aquifers - Rock layer that stores and allows the flow of groundwater. • Recharge zone - surface of the land where water enters the aquifer ...
Document
Document

... 13. How do magnetic reversals provide evidence of sea-floor spreading? _______________________________________________________________ _______________________________________________________________ 14. Explain how sea-floor spreading provides a way for continents to move. __________________________ ...
November 2003
November 2003

... The table below provides information collected at seismic stations A, B, and C for the same earthquake. ...
course outline - UTSC - University of Toronto
course outline - UTSC - University of Toronto

... been in operation for at least 3 Ga. It may not be the only way in which planet Earth functions however and there is increasing recognition of so-called vertical tectonics involving giant mantle plumes and the outpouring of enormous volumes of magma at the Earth’s surface. Lithospheric plates are cr ...
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Geobiology

Broadly defined, geobiology is an interdisciplinary field of scientific research that explores interactions between the biosphere and the lithosphere and/or the atmosphere.
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