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Ocean Floor
Ocean Floor

... CONTINENTAL CRUST = THICK AND LEIGTHER ...
Layers of the Earth PowerPoint
Layers of the Earth PowerPoint

... OF SPACE AN OBJECT TAKES UP. If a liquid is heated to a gas, it will take up more space than before. ...
Structure Of The Earth
Structure Of The Earth

... • The lithosphere (geosphere) is the "solid" part of Earth. It has two parts, the crust and the upper mantle • The lithosphere “ sits on the” asthenosphere. • The Earths Plates are the lithosphere. • It is the rocky, solid portion of the crust. Remember that it is made up of mostly Silicon( Si) and ...
Earth Science Glossary - Newcomers High School
Earth Science Glossary - Newcomers High School

... apogee point in an orbit farthest from the Earth. apparent diameter the diameter of an object as it appears to an observer; changes with distance. apparent magnitude how bright a star appears to someone on Earth. arid climates that are extremely dry, with low precipitation and high evapotranspirati ...
The Earth`s Layers Foldable
The Earth`s Layers Foldable

... © Copyright 2004 - 2005.  M. J. Krech. All rights reserved. Reproduction for educational purposes is encouraged. ...
Unit 5 - Structure and Composition of the Earth
Unit 5 - Structure and Composition of the Earth

... History of Plate Tectonics • Plate tectonic theory had its beginnings in 1915 when Alfred Wegener proposed his theory of "_______________." • He was one of the first to realize that the Earth's surface has changed through time, and that continents that are separated now may have been joined togethe ...
Earth System Science: The Big Ideas
Earth System Science: The Big Ideas

... Earth sciences revolves around the causes of these glacial cycles, with the general consensus pointing toward cyclic variations in the planet’s tilt, movement about its axis, and its orbital shape around the sun. These variations lead to changes in the amount of solar radiation that reaches the Eart ...
Document
Document

... Plates Slide • As plates pass by each other, they ...
The Earth`s Layers Foldable
The Earth`s Layers Foldable

... rocks that can flow under pressure. It is thought that when the rocks rise due to the very intense heat and then cool, this means that they sink back to the core and this movement causes the crust to break into sections, or plates. When these move and crash into each other it causes earthquakes and ...
Earth`s Layers Lesson Plan - elementaryscienceteachers
Earth`s Layers Lesson Plan - elementaryscienceteachers

... Model: Show the students a mini Milky Way bar. Ask them what they think a Milky Way bar and the Earth have in common. Ask them if they think that they could make any comparisons between the candy and the Earth. Create a list of comparisons between the Earth and Milky Way Bar that the students offer. ...
6.B Formative Assessment #1
6.B Formative Assessment #1

... Directions: Using the terms in the word bank, answer the following questions. Be sure to use complete sentences and label the drawing. Density  or  dense   ...
The Earth`s Layers From least to most dense
The Earth`s Layers From least to most dense

... Magnetism has been used by sailors to find their way on earth for thousands and thousands of years. Magnetism also influences particles outside the atmosphere of the earth up to more than 60, 000 kilometers (37,000 miles) into space. The outer core is about 2200– 5000 °C (3992- 9032 °F). The density ...
Name: _________________________ Period: ______ Date
Name: _________________________ Period: ______ Date

... 7. Know how to read and answer questions based on the time zone map below. (C22) Which of earth’s motions is the cause of time zones? rotation ...
Topic Six - Science - Miami-Dade County Public Schools
Topic Six - Science - Miami-Dade County Public Schools

... Student BYOD Resource Page ...
CHAPTER 1 - INTRODUCTION TO PHYSICAL GEOLOGY
CHAPTER 1 - INTRODUCTION TO PHYSICAL GEOLOGY

... developed and looks at some of the important figures in the development of geology in Canada. Two key concepts in geology are then briefly examined as these are fundamental to the discipline – plate tectonics and the geological time scale. The discussion then turns to examine the range of work moder ...
Earth`s Layered Structure
Earth`s Layered Structure

... Layers Defined by Physical Properties ...
Rocks and minerals
Rocks and minerals

... hardness (Mohs scale), (how it reflects light) and color, as well as more complicated properties such as streak, fracture, cleavage and density. ...
the earth`s interior
the earth`s interior

... Ever since its formation—some 4.5 billion years ago—the earth has been losing heat. The deeper one goes inside the earth, the greater the temperature becomes. The pressure rises, too. The earth’s outer layer, or crust, is the coolest and least dense of all the layers inside the earth. (You might com ...
N.HW101
N.HW101

... every 40 meters that you descend from that point, the temperature rises 1 Celsius degree. This rapid rise in temperature continues for several tens of kilometers. After that, the temperature increases more slowly, but steadily. Near the top of the crust, temperatures average around 20°C. At the bott ...
Biogeochemical cycles – Geological, Chemical
Biogeochemical cycles – Geological, Chemical

... between the high temperature vents and cold oxygenated sea water. The bacteria thrive on gases produced by the vents such as methane and use these chemicals to produce simple organic molecules to support the local ecosystem in a similar way to plants using photosynthesis. • Wächtershauser has propos ...
Directed Reading
Directed Reading

... ______ 3. rifting ...
Final Review Answers - Academic Computer Center
Final Review Answers - Academic Computer Center

... False, they are hard to overcome because they make sense to the possessor _____ 2. The following statement is a fact: “The Sun will continue as a yellow star for another 10 billion years.” False, this is a projection based on what we have observed/theorized, not a provable statement _____ 3. The til ...
How did plate tectonics emerge on Earth?
How did plate tectonics emerge on Earth?

... than to weaken (10 million years). Changes in mantle convection were therefore slow enough to damage the lithosphere locally, but fast enough to prevent complete healing, thus allowing enough weak zones to accumulate for plates to form. In this model, the Earth's lithosphere accumulates enough damag ...
Curriculum Map and Pacing Guide – Earth Systems
Curriculum Map and Pacing Guide – Earth Systems

... Where I Found This taskstudents will be presented with fossil specimens collected in the state of Georgia, a fossil field guide, and a geologic map of Georgia and will be asked to synthesize the ...
The Terrestrial Planets
The Terrestrial Planets

... • Definition - the daily fluctuation in ocean level. • The magnitude of the fluctuation (height of the tides) can vary from a few centimeters to many meters depending on location and time of year. Average 1 m in the open sea. • An enormous amount of energy is contained in the daily tidal motions of ...
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