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Rock Webquest
Rock Webquest

... Explore the Rock Creations area to complete each section. For thousands, even millions of years, little pieces of our earth have been eroded-- broken down and worn away by __________ and __________. These little bits of our earth are washed downstream where they settle to the bottom of the _________ ...
Rock Cycle and Rock Types
Rock Cycle and Rock Types

... remains of organic matter. • The most important of ...
II. Subduction-related granites: “Andean” I
II. Subduction-related granites: “Andean” I

... 1. Major elements Alkaline, peralkaline (not that the two terms do not have the same values, one refers to a magmatic series, the other to a position in A/CNK vs. A/NK diagrams). Low K/Na, low Mg/Mg+Fe 2. Trace elements Rich in LREE (10-100 times more than I and S types !). Some huge depletions and ...
Normal Faults
Normal Faults

... Magma rises through the Earth’s surface to form volcanic mountains. ...
Rock Formations: How Igneous, Sedimentary, and Metamorphic
Rock Formations: How Igneous, Sedimentary, and Metamorphic

... Magma can result from the melting of existing rocks in the Earth’s mantle or crust. This melting usually occurs when there is an increase in temperature, a decrease in pressure, or a change in composition. Igneous rocks can be either intrusive (forming below the Earth’s surface) or extrusive (formin ...
GEOLOGY EXAM IS ___Weds. 11/28
GEOLOGY EXAM IS ___Weds. 11/28

... _________________ 9. Minerals that form irregular surfaces when they break apart have a property called cleavage. ...
Plate Tectonics
Plate Tectonics

... ◦ Oldest rocks were found closest to the shoreline, youngest nearest the ridge ◦ Therefore: The ridge is producing new oceanic crust while older crust is being pushed toward the shoreline ...
Background Information for Plate Tectonics Rock Formation
Background Information for Plate Tectonics Rock Formation

... water or wind carrying it. These deposits may include shells, bones, leaves, stems, and other remains of living things.  Compaction is the process that presses sediments together. As more and more sediment falls on top, creating new layers, the weight of the layers squeezes the sediments tightly to ...
The evolution of Life in the History of Earth
The evolution of Life in the History of Earth

... Life on a Changing Earth Life is a continuum - from the earliest organisms to the great variety of species that exist today • Geological events change the course of biological evolution • Conversely, life changes the planet that it inhabits ...
The theory of plate tectonics
The theory of plate tectonics

... The Geological Timescale • The earth is 4600 million year • Only the last 570 million years are well documented as this is when life became abundant ...
Questions for the fifth quiz
Questions for the fifth quiz

the Earth`s interior must be much greater than 2.8 g/cm3 for the
the Earth`s interior must be much greater than 2.8 g/cm3 for the

APES Focus/Ch - cynthiaahmed
APES Focus/Ch - cynthiaahmed

... 12. Igneous rocks are those formed directly from magma. They are classified as basaltic or granitic, and by their mode of formation as extensive or intrusive. Explain each of these terms. ...
Seafloor Ages ABC - SERC
Seafloor Ages ABC - SERC

... Seafloor Ages Part 1: Divergent Boundary A divergent boundary in the center of an ocean is shown below with arrows showing the direction the crust is moving. 1) Where is the oldest crust found? A ...
Earth Science Introduction
Earth Science Introduction

... 1 Second = 1 Year • 35 minutes to birth of Christ • 1 hour+ to pyramids • 3 hours to retreat of glaciers from Wisconsin • 12 days = 1 million years • 2 years to extinction of dinosaurs • 14 years to age of Niagara Escarpment • 31 years = 1 billion years ...
While hiking, you find a rock that is soft, fine grained, dark, and
While hiking, you find a rock that is soft, fine grained, dark, and

A Head
A Head

... happen near the oceanic trenches. 11 The Himalaya mountains are growing taller by about 5 mm each year. 12 Surveys of the ocean floor show tat there are very long mountain ridges beneath the oceans. 13 Rock samples have been taken from the ocean floor. These show that the rocks are much younger near ...
rock cycle_pangea - Northside Middle School
rock cycle_pangea - Northside Middle School

... Many forces cause the surface of the Earth to change over time. However, the largest force that changes our planet’s surface is the movement of Earth's outer layer through the process of plate tectonics. This process causes mountains to push higher and oceans to grow wider. ...
ES2 Sea floor spreading Name: Introduction: About 30 years ago
ES2 Sea floor spreading Name: Introduction: About 30 years ago

platetect
platetect

... >>>> Notice that as we travel vertically the amount of quartz in the rock increases, and at the 90% boundary and above the rock has so much quartz the rock becomes a "quartz something", such as a quartz sandstone or quartz conglomerate. >>>> The lower two fields contain rocks that are felspar (red) ...
Classifying rocks
Classifying rocks

...  _______________ is most common (on ocean floor)  Intrusive Rock: forms from magma __________ Earth’s surface  _______________ is the most abundant o Texture: depends on _______________ and shape of mineral crystals  Small crystals: Lava cools _______________  _______________ rock o ___________ ...
Key expressions and vocabulary
Key expressions and vocabulary

... ...
Igneous Rock PPT - Effingham County Schools
Igneous Rock PPT - Effingham County Schools

... Molten rock with lower amounts of silica flows faster than molten rock with higher amounts of silica. ...
Chapter 8 Notes
Chapter 8 Notes

... • Sedimentary Rocks a. form from sediments being compressed by other overlying sediments b. typically uniform in composition c. sink for phosphorus d. fossil record ...
Chapter 9 Notes III. Continental Tectonics I. Great ocean basins
Chapter 9 Notes III. Continental Tectonics I. Great ocean basins

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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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