word doc leoce study guide with answers
... organism are found on continents that are far away from each other. Some fossil deposits form patterns that can be connected like a puzzle. ...
... organism are found on continents that are far away from each other. Some fossil deposits form patterns that can be connected like a puzzle. ...
EPSC-201_2015final-E..
... In the largest stars the cycle of nuclear fuel depletion, renewed collapse, core temperature rise, and ignition of a less flammable nuclear fuel is repeated several times, but as the mass number increases, each merger leads to a smaller loss of mass and to the corresponding production of heat. Final ...
... In the largest stars the cycle of nuclear fuel depletion, renewed collapse, core temperature rise, and ignition of a less flammable nuclear fuel is repeated several times, but as the mass number increases, each merger leads to a smaller loss of mass and to the corresponding production of heat. Final ...
PHSC 4013 Course Outline—Fall 2008
... internal structure and a definite chemical composition. o Rock = any solid mass of mineral or mineral-like matter that occurs naturally as part of the planet. o These are materials found on the surface of the Earth, but as one goes deeper, the mean density of these properties increases A brief overv ...
... internal structure and a definite chemical composition. o Rock = any solid mass of mineral or mineral-like matter that occurs naturally as part of the planet. o These are materials found on the surface of the Earth, but as one goes deeper, the mean density of these properties increases A brief overv ...
THE INNER PLANETS
... dense and have rocky surfaces. The inner planets are often called “terrestrial planets,” from the Latin word “terra” which means “Earth.” ...
... dense and have rocky surfaces. The inner planets are often called “terrestrial planets,” from the Latin word “terra” which means “Earth.” ...
Mid Term Review Sample Questions
... Mid – Term Exam Review For Earth Science 1. What causes tectonic plates to move? _____________________________ 2. Where do volcanoes and earthquakes occur relative to plate boundaries? ______________________ 3. What probably caused the dinosaurs to go extinct? _____________________ 4. What is the co ...
... Mid – Term Exam Review For Earth Science 1. What causes tectonic plates to move? _____________________________ 2. Where do volcanoes and earthquakes occur relative to plate boundaries? ______________________ 3. What probably caused the dinosaurs to go extinct? _____________________ 4. What is the co ...
The Appalachian Story sheet
... 1. The province of Newfoundland can be separated into ________ distinct geological zones. 2. Rocks on the western side of NFLD near Dover are ____________ million years old. These rocks are predominantly _____________________ (type of rock). 3. In the fault zone, rocks are sheared and deformed by in ...
... 1. The province of Newfoundland can be separated into ________ distinct geological zones. 2. Rocks on the western side of NFLD near Dover are ____________ million years old. These rocks are predominantly _____________________ (type of rock). 3. In the fault zone, rocks are sheared and deformed by in ...
controls (practical/laboratory) work, abstract
... agencies, e.g. in the folding of strata or the nearby intrusion of igneous rocks C-is the solid mineral material forming part of the surface of the earth and other similar planets, exposed on the surface or underlying the soil or oceans D-is a coarse-grained metamorphic rock which consists of layers ...
... agencies, e.g. in the folding of strata or the nearby intrusion of igneous rocks C-is the solid mineral material forming part of the surface of the earth and other similar planets, exposed on the surface or underlying the soil or oceans D-is a coarse-grained metamorphic rock which consists of layers ...
E.S. SOL Facts
... cool very slowly. The texture if intrusive rocks include coarse or large mineral grains. Examples of intrusive rocks include granite. 34. Felsic colored rocks are light colored, while mafic rocks are dark colored. Ultramafic rocks may contain olivine and augite and are very dark in color. 35. Metamo ...
... cool very slowly. The texture if intrusive rocks include coarse or large mineral grains. Examples of intrusive rocks include granite. 34. Felsic colored rocks are light colored, while mafic rocks are dark colored. Ultramafic rocks may contain olivine and augite and are very dark in color. 35. Metamo ...
SEDIMENTARY ROCKS
... plants) transported and laid down by running water, wind or ice. Generally silicate minerals. 2. Chemical and biochemical sediments -chemical precipitation of dissolved components of rocks at the ...
... plants) transported and laid down by running water, wind or ice. Generally silicate minerals. 2. Chemical and biochemical sediments -chemical precipitation of dissolved components of rocks at the ...
1 Eons, Eras, Periods and Epochs Dating by radioactive isotopes
... 4. Disk of matter (many elements) around sun 5. Disk slowly accretes into clumps (planetesimals) that also contain heavier elements 6. planetesimals → planetoids → planets and satellites Hubble Space Telescope view of a new solar system 1500 l-y away in the Orion Nebula ...
... 4. Disk of matter (many elements) around sun 5. Disk slowly accretes into clumps (planetesimals) that also contain heavier elements 6. planetesimals → planetoids → planets and satellites Hubble Space Telescope view of a new solar system 1500 l-y away in the Orion Nebula ...
Metamorphic Rocks - Washingtonville Central School District
... Intense Heat and/or Pressure, Yo! ...
... Intense Heat and/or Pressure, Yo! ...
Metamorphic Rocks
... Collisions between Earth’s plates push rock down toward the heat of Earth’s 1. ___________________. ➡ As the rock is buried deeper in the crust, 2. ___________________ also increases on the rock. ➡ The rock is squeezed so tightly that the 3. ___________________ of the rock change, creating metamorph ...
... Collisions between Earth’s plates push rock down toward the heat of Earth’s 1. ___________________. ➡ As the rock is buried deeper in the crust, 2. ___________________ also increases on the rock. ➡ The rock is squeezed so tightly that the 3. ___________________ of the rock change, creating metamorph ...
Sedimentary Rocks - McGraw Hill Higher Education
... Sand forms sandstone Silt & clay form shale or siltstone Organic materials form limestone or coal ...
... Sand forms sandstone Silt & clay form shale or siltstone Organic materials form limestone or coal ...
Overview of the Big Questions in Physical Geology
... subcontinent of India into Asia, to produce the Himalayas and the Tibetan Plateau. What is a rock? What is a mineral?A rock can be made of one or more minerals. An example of a singlemineral rock would be rock salt, or halite (the mineral). Most rocks are made of groups of minerals (igneous and meta ...
... subcontinent of India into Asia, to produce the Himalayas and the Tibetan Plateau. What is a rock? What is a mineral?A rock can be made of one or more minerals. An example of a singlemineral rock would be rock salt, or halite (the mineral). Most rocks are made of groups of minerals (igneous and meta ...
STUDY GUIDE FOR MID-TERM EXAM KEY In which type of rock are
... 33. Students want to identify a rock in a nearby field. Which property would be most useful in identifying the unknown rock?___Mineral content___________ 34. Rocks formed by the cementing of weathered materials are called _sedimentary_ rocks. 35. Draw and correctly label a rock cycle. A igneous ro ...
... 33. Students want to identify a rock in a nearby field. Which property would be most useful in identifying the unknown rock?___Mineral content___________ 34. Rocks formed by the cementing of weathered materials are called _sedimentary_ rocks. 35. Draw and correctly label a rock cycle. A igneous ro ...
Metamorphic Rocks
... • Regional Metamorphic Rocks – these rocks form over millions of years and many thousands of meters of sediments accumulated in the ocean basins. The overlying weight causes the sediments to lithify and eventually metamorphose. • Example shale metamorphoses into slate ...
... • Regional Metamorphic Rocks – these rocks form over millions of years and many thousands of meters of sediments accumulated in the ocean basins. The overlying weight causes the sediments to lithify and eventually metamorphose. • Example shale metamorphoses into slate ...
SUMMARY KEY TERMS APPLYING THE CONCEPTS
... is a tetrahedral structure that combines with positive metallic ions or with other tetrahedral units to form chains, sheets, or an interlocking framework. The ferromagnesian silicates are tetrahedral structures combined with ions of iron, magnesium, calcium, and other elements. The ferromagnesian si ...
... is a tetrahedral structure that combines with positive metallic ions or with other tetrahedral units to form chains, sheets, or an interlocking framework. The ferromagnesian silicates are tetrahedral structures combined with ions of iron, magnesium, calcium, and other elements. The ferromagnesian si ...
Physics 127 Descriptive Astronomy Homework #12 Key (Chapter 6
... 6-6. If Mercury is the closest planet to the Sun and has such a high average surface temperature, how is it possible that ice might exist on its surface? Because Mercury’s rotational axis is almost perfectly perpendicular to its orbital plane, no sunshine ever falls on the floors of craters near its ...
... 6-6. If Mercury is the closest planet to the Sun and has such a high average surface temperature, how is it possible that ice might exist on its surface? Because Mercury’s rotational axis is almost perfectly perpendicular to its orbital plane, no sunshine ever falls on the floors of craters near its ...
Practice Test-1 - Florida International University
... 20. The first minerals to crystallize out of a magma is likely to be more A) felsic, B) mafic, C) of the same composition as the magna D) can be any of these 21. The mineral plagioclase is an example of a ________ silicate. A) framework single chain C) sheet D) ring ...
... 20. The first minerals to crystallize out of a magma is likely to be more A) felsic, B) mafic, C) of the same composition as the magna D) can be any of these 21. The mineral plagioclase is an example of a ________ silicate. A) framework single chain C) sheet D) ring ...
Metamorphic Rock Metamorphic rocks have been changed over
... Metamorphic rocks can be formed by pressure deep under the Earth's surface, from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates. Uplift and erosion help bring metamorphic rock to the Earth's surface. Examples of metamorphic rocks include anthracite, qua ...
... Metamorphic rocks can be formed by pressure deep under the Earth's surface, from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates. Uplift and erosion help bring metamorphic rock to the Earth's surface. Examples of metamorphic rocks include anthracite, qua ...
Planet Earth - Topic 2 (ANSWERS)
... 1. Scientists have grouped rocks into three major families they are igneous, sedimentary and metamorphic rocks. Each can be identified by its appearance. *Type I - Igneous rock forms when hot magma or lava cools and solidifies. 3. Magma is melted rock found below the Earth’s crust, where temperature ...
... 1. Scientists have grouped rocks into three major families they are igneous, sedimentary and metamorphic rocks. Each can be identified by its appearance. *Type I - Igneous rock forms when hot magma or lava cools and solidifies. 3. Magma is melted rock found below the Earth’s crust, where temperature ...
Metamorphic rocks
... • Unlike what you may have heard, it’s not just “heat and pressure” applied to existing rocks • Also, not due to partial melting of rocks • What it is: “the solid-state reaction of minerals within the rock to produce new minerals and thus new rocks” ...
... • Unlike what you may have heard, it’s not just “heat and pressure” applied to existing rocks • Also, not due to partial melting of rocks • What it is: “the solid-state reaction of minerals within the rock to produce new minerals and thus new rocks” ...
Rocks Powerpoint Notes
... mantle that slowly change rocks from one kind to another Once a rock is formed, does it stay the same rock forever?_____________ Rocks are continually changed by many ___________________, such as weathering, _______________, compaction, ________________________, melting, and cooling Rocks can ______ ...
... mantle that slowly change rocks from one kind to another Once a rock is formed, does it stay the same rock forever?_____________ Rocks are continually changed by many ___________________, such as weathering, _______________, compaction, ________________________, melting, and cooling Rocks can ______ ...
magma
... a. Formed from another rock by heat and pressure. b. Usually form beneath the earth’s crust (which means they often heat up and become magma again—it’s a cycle—the Rock Cycle!) c. Fact: Both igneous and sedimentary rocks can change into metamorphic rocks. d. Characteristics: These rocks are usually ...
... a. Formed from another rock by heat and pressure. b. Usually form beneath the earth’s crust (which means they often heat up and become magma again—it’s a cycle—the Rock Cycle!) c. Fact: Both igneous and sedimentary rocks can change into metamorphic rocks. d. Characteristics: These rocks are usually ...
layer of the atmosphere in which weather occurs and we have direct
... oceanic crust: crust that is made mostly of basaltic rock and is very dense continental crust: crust that is made mostly of granitic rock and is less dense than the other type of crust hot spots: places where molten material rises from the asthenosphere and reaches the lithosphere seafloor spreading ...
... oceanic crust: crust that is made mostly of basaltic rock and is very dense continental crust: crust that is made mostly of granitic rock and is less dense than the other type of crust hot spots: places where molten material rises from the asthenosphere and reaches the lithosphere seafloor spreading ...
Composition of Mars
The composition of Mars covers the branch of the geology of Mars that describes the make-up of the planet Mars.