EES Geology Vocabulary Review Name___________________
... Mantle- the layer of the Earth between the crust and the outer core; this layer makes up most of the volume of the Earth Lithosphere- the rigid crust and outer mantle Asthenosphere- the semisolid (soft, plastic) layer of the mantle Outer Core- the liquid layer of the Earth that surrounds the inner c ...
... Mantle- the layer of the Earth between the crust and the outer core; this layer makes up most of the volume of the Earth Lithosphere- the rigid crust and outer mantle Asthenosphere- the semisolid (soft, plastic) layer of the mantle Outer Core- the liquid layer of the Earth that surrounds the inner c ...
Geography 1
... dots) in the surrounding foothills. The squiggly lines show the rivers that flow from the mountain. In which town will the potential hazard for a lahar be greatest? -The town of Timberland (two rivers meet) followed by Tinytown (proximity). ...
... dots) in the surrounding foothills. The squiggly lines show the rivers that flow from the mountain. In which town will the potential hazard for a lahar be greatest? -The town of Timberland (two rivers meet) followed by Tinytown (proximity). ...
Obj - davis.k12.ut.us
... a) Crust – the Earth’s solid and rocky outer layer, including both land surface (continental crust), and ocean floor (oceanic crust). The crust averages 32 km thick and is composed of O2, Si, Al, Ca, Fe, Na, K, and Mg. b) Mantle – the layer below the crust comprised of the lithosphere (upper mantle) ...
... a) Crust – the Earth’s solid and rocky outer layer, including both land surface (continental crust), and ocean floor (oceanic crust). The crust averages 32 km thick and is composed of O2, Si, Al, Ca, Fe, Na, K, and Mg. b) Mantle – the layer below the crust comprised of the lithosphere (upper mantle) ...
document
... Summation/synthesis of the entire poster or project. No more than five or so sentences at the most. ...
... Summation/synthesis of the entire poster or project. No more than five or so sentences at the most. ...
Mineral
... Tiny bits of rock that can be carried by moving water or wind. The bits get deposited (left) in a new location or build up in layers. ...
... Tiny bits of rock that can be carried by moving water or wind. The bits get deposited (left) in a new location or build up in layers. ...
What is a Rock?
... • These layers are made up of progressively denser material toward the center of the Earth. ...
... • These layers are made up of progressively denser material toward the center of the Earth. ...
6th Grade Earth Science
... • A mineral can also be identified by the ______ shape of its crystals. • _______ Cleavage - minerals show particular patterns when they are broken along flat planes. ...
... • A mineral can also be identified by the ______ shape of its crystals. • _______ Cleavage - minerals show particular patterns when they are broken along flat planes. ...
INTRODUCTION TO TYPES AND CLASSIFICATION OF ROCKS
... rocks. Metamorphic rocks therefore form at great depths, but exposed on the surface due to erosion and epirogenic movements. Each of these three rock types can be further classified in terms of; chemistry, how the form and environment of formation. The distributions of these major rock types are cri ...
... rocks. Metamorphic rocks therefore form at great depths, but exposed on the surface due to erosion and epirogenic movements. Each of these three rock types can be further classified in terms of; chemistry, how the form and environment of formation. The distributions of these major rock types are cri ...
Earth Science Essential Knowledge and Skills
... sedimentation – the process of depositing sediments tides – the periodic rise and fall of water level caused by the gravitational pull of the moon and sun as well as forces of circular motion trench – the deepest feature in the ocean; forms at subduction zones upwelling – the rising of deep water to ...
... sedimentation – the process of depositing sediments tides – the periodic rise and fall of water level caused by the gravitational pull of the moon and sun as well as forces of circular motion trench – the deepest feature in the ocean; forms at subduction zones upwelling – the rising of deep water to ...
The Structure of the Earth*s Interior
... Please read through the PowerPoint to add to your Layers of the Earth foldable any information you do not already have. ...
... Please read through the PowerPoint to add to your Layers of the Earth foldable any information you do not already have. ...
Earth`s Interior Crust Mantle Core
... • Convection in liquid metal outer core. • Convection is coupled to Earth’s ...
... • Convection in liquid metal outer core. • Convection is coupled to Earth’s ...
Landforms
... • Geology- the study of Earth’s physical structures and the processes that have created them • Forces below Earth’s surface are key to shaping landforms • Four important zones in Earth’s Interior – Core-Center: like a nuclear furnace, divided into inner(solid) and outer core (dense liquid metal) – M ...
... • Geology- the study of Earth’s physical structures and the processes that have created them • Forces below Earth’s surface are key to shaping landforms • Four important zones in Earth’s Interior – Core-Center: like a nuclear furnace, divided into inner(solid) and outer core (dense liquid metal) – M ...
EarthLayersPlateTectonicsPP
... • As Earth cooled, crust formed as its upper layer solidified. • These early crust pieces returned to the mantle carrying water which when recycled produced a less dense, granitic crust. • Differentiation: Layering of the Eearth as it cooled due to differences in density, (iron sank) while Earth wa ...
... • As Earth cooled, crust formed as its upper layer solidified. • These early crust pieces returned to the mantle carrying water which when recycled produced a less dense, granitic crust. • Differentiation: Layering of the Eearth as it cooled due to differences in density, (iron sank) while Earth wa ...
Layers of the Earth Study Guide
... 1. The first layer of the earth is called the crust. 2. It is the layer of the Earth where we live. 3. It is the outer most (outside) layer of the Earth. 4. It is a solid and is up to 100 kilometers thick. 5. It is the coolest in temperature of all the ...
... 1. The first layer of the earth is called the crust. 2. It is the layer of the Earth where we live. 3. It is the outer most (outside) layer of the Earth. 4. It is a solid and is up to 100 kilometers thick. 5. It is the coolest in temperature of all the ...
Outer Core - Wikispaces
... are not plate boundaries have little or no seismic or volcanic activity form when a continent rifts apart creating a new ocean basin between the fragments. ...
... are not plate boundaries have little or no seismic or volcanic activity form when a continent rifts apart creating a new ocean basin between the fragments. ...
KEY Earth`s Interiors Lab Sheet Student Name(s): Use the labeled
... crust of the Earth is the same temperature as the air. So, it might be as hot as 35 °C in the desert and below freezing in Antarctica. If you dig down, the temperature goes up. The crust is very thin, just 5-70 km. ...
... crust of the Earth is the same temperature as the air. So, it might be as hot as 35 °C in the desert and below freezing in Antarctica. If you dig down, the temperature goes up. The crust is very thin, just 5-70 km. ...
Chapter 8 Plate Tectonics With Video
... 4. Climatic patterns shown by rock layers: Some rock types only form in certain climates, for example coal, which forms in warm, very wet (rainy) environments. If coal is found in a place that is not warm and rainy, then either the climate has changed or the rock has moved. ...
... 4. Climatic patterns shown by rock layers: Some rock types only form in certain climates, for example coal, which forms in warm, very wet (rainy) environments. If coal is found in a place that is not warm and rainy, then either the climate has changed or the rock has moved. ...