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First Hour Exam, Fall, 2016
First Hour Exam, Fall, 2016

... a. a transform boundary c. a convergent boundary b. a shoreline boundary d. a divergent boundary 10. The upper mantle is believed to be composed mostly of a. olivine and pyroxene c. clays and other sheet silicates b. iron and magnesium d. carbonates and oxides 11. The core of the Earth is believed t ...
Jeopardy
Jeopardy

... sidewalk is an example of which type of weathering: Physical or Chemical? ...
Earth Science Reference Tables
Earth Science Reference Tables

... Energy gained during melting . . . . . . . . . . . . . . . . 80 calories/gram Energy released during freezing ...
layers of the earth
layers of the earth

... Homeroom Make sure all science homework is complete Do not walk around! ...
summing-up - Zanichelli online
summing-up - Zanichelli online

... new sedimentary rocks, unconformally on the older ones. Over billions of years, the traces of numerous cycles, similar to that described, can be seen in the rocks in the Earth’s crust. ...
LG: Identify the steps of the Rock Cycle
LG: Identify the steps of the Rock Cycle

... Plate tectonic movement is responsible for the recycling of rock materials. As the earth’s plates slowly move, the rocks that make up the plates are continuously recycled and change from one form to another ...
Rocks
Rocks

... Plate tectonic movement is responsible for the recycling of rock materials. As the earth’s plates slowly move, the rocks that make up the plates are continuously recycled and change from one form to another ...
Desert Area of land with too little rainfall to support much
Desert Area of land with too little rainfall to support much

Lesson 5 - Igneous Rocks .key
Lesson 5 - Igneous Rocks .key

... and a white precipitate means it does. ...
Chapter 9 notes
Chapter 9 notes

... a. The lithosphere is broken into small and large sections called plates. 1. All sections meet at plate boundaries (edge of the plate). b. All of Earth’s plates move slowly (some slower than others) and they might move together, pull apart from each other or move past each other because of gravity a ...
Physical Geology 101*Midterm 1
Physical Geology 101*Midterm 1

... A. compressional, shear, tensional B. tensional, shear, compressional C. tensional, compressional, shear D. shear, compressional, tensional E. shear, tensional, compressional 35. Volcanic glass, i.e. obsidian, is not considered a mineral because it: A. does not have enough silicon or oxygen in its c ...
Earth`s interior
Earth`s interior

... by earthquakes allow scientists to measure the speed in which they travel giving clues to the structure of the planet. ...
6th Grade Science Semester Exam Review The semester exam will
6th Grade Science Semester Exam Review The semester exam will

Geography 12
Geography 12

... _IGNEOUS_________ rock formed from the solidification (cooling) of magma below and above the earth’s surface. This type of rock was changed by great heat and pressure from its original state ___METAMORPHIC_________. The weathering and erosion of the earth’s crust is deposited in layers. The compacti ...
!GLG-101-Chapter 1-Illustrated Vocabulary copyright 2003
!GLG-101-Chapter 1-Illustrated Vocabulary copyright 2003

... *the surface layer of the planet is brittle and broken into large pieces called plates. Convection within the mantle of the planet moves these plates with respect to each other. !rock cycle *a description of physical processes that relate the formation of igneous rocks, sediments, sedimentary rocks, ...
Sedimentary Rocks
Sedimentary Rocks

... b. Sediments are loose materials such as rock fragments, mineral grains and bits of plant and animal remains that have been moved by wind, water, ice or gravity i. ...
The Rock Cycle - Science A 2 Z
The Rock Cycle - Science A 2 Z

... Any rock (igneous, sedimentary, or metamorphic) exposed at the Earth's surface can become a sedimentary rock. The forces of wind, rain, snow, and ice combine to break down or dissolve (weather), and carry away (transport) rocks exposed at the surface. These particles eventually come to rest (deposi ...
Midterm Exam
Midterm Exam

... number of neutrons C. Atoms of most elements can gain or lose electrons from their outer shells to form ions D. The positively charged cation of an element is heavier than the atom of that element, because of the addition of electrons ...
Changing Earth*s Surface
Changing Earth*s Surface

... Lesson 3 Vocabulary ...
EES 202 - Geological processes powerpoint
EES 202 - Geological processes powerpoint

... sea, swamp. ...
study guide - Hull Lessons
study guide - Hull Lessons

... together like pieces of a jigsaw puzzle. The theory that says the earth’s surface is made up of about 20 moving pieces is called plate tectonics. Plate tectonics is the scientific theory that explains how continents move. The earth’s plates move very slowly. Mountains, earthquakes, and volcanoes are ...
Geology of the Kingston Area – 1.1 Billion Years of History
Geology of the Kingston Area – 1.1 Billion Years of History

... Rocks are made up of different kinds of minerals. The types of minerals, and the way that the rock formed, can be used to determine the environment in which the rock formed. ...
Intrusive Igneous Rocks, part 1
Intrusive Igneous Rocks, part 1

... • Volume percent abundance is an important means of rock classification • Total lack of glass - slow cooling allows matter to achieve the lowest energy state, which is as crystalline matter ...
Tonalite, Diorite, Gabbro, Norite and Anorthosite
Tonalite, Diorite, Gabbro, Norite and Anorthosite

... • Volume percent abundance is an important means of rock classification • Total lack of glass - slow cooling allows matter to achieve the lowest energy state, which is as crystalline matter ...
Intrusive Igneous Rocks, part 1
Intrusive Igneous Rocks, part 1

... • Volume percent abundance is an important means of rock classification • Total lack of glass - slow cooling allows matter to achieve the lowest energy state, which is as crystalline matter ...
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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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