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Marano- Geology
Question | Answer |
---|---|
geology | study of Earth |
minerals | solid, inorganic (nonliving), pure substances that make up the Earth |
minerals | made of only one type of matter, building blocks of rocks |
Physical traits to identify minerals | color, luster, streak, hardness, cleavage, density |
Is the color of a mineral the best indicator for identification? | No, because impurities or weathering may change color |
Luster | the way that light reflects on a surface |
metallic luster | shiny surface |
nonmetallic luster | glassy, greasy, oily, waxy, earthy, dull |
streak | color of powder left when a mineral is rubbed against a hard rough surface |
streak plate | unglazed porcelain |
Hardness | mineral's resistance to being scratched |
What scale is hardness based on? | Moh's scale (1 to 10) |
What is the softest mineral on Moh's scale? | talc=1 |
What is the hardest mineral on Moh's scale? | diamond=10 |
Mineral's tendency to break in a specific crystal pattern along areas of weakness? | cleavage |
Mineral's tendency to break in no particular pattern | fracture |
density | amount of matter in a certain amount of space, how packed something is |
formula for density | density = mass/volume |
label for density | g/cm3 |
specific gravity | comparison of mineral's density to water's density (1 gm/cm3) |
hydrochloric acid causes _______ on some minerals such as calcite | bubbling |
Halite tastes like _____ | salt |
Which mineral is magnetic? | magnetite |
flame color | when minerals are burned they may glow a specific color |
Glows green | copper |
Which minerals will glow (fluorescence)? | calcite and fluorite |
Rocks made up of one or more _______. | minerals |
Differences in rocks are based on the _____ of the rock. | origin (how it was made) |
Texture of rocks | sizes, shapes and positions of the grain it is made up of |
Three types of rocks | Igneous, sedimentary, and metamorphic |
Igneous rocks | Latin for fire, made of cooled molten matter |
Lava | when matter is above ground |
magma | when matter is in the ground |
As matter cools, it forms _______. | Crystals |
The faster the matter cools, the (smaller, bigger) the crystals. | smaller |
Extrusive (volcanic) igneous rocks | form outside of the volcano and have small crystals |
Intrusive (plutonic) igneous rocks | form inside of volcano from magma and have large crystals |
Sedimentary rocks | made from sediments |
sediments | solid fragments (pieces) of material that have been moved by air, water, ice and clumped together |
lithification | when loose sediments become rock |
examples of lithification | cementation and compaction |
Compaction | loose sediments swished together |
Cementation | loose sediments glued together |
Sedimentary rock | forms at or near the Earth's surface at normal temperature and pressure |
Sedimentary rock | may contain fossils |
Sedimentary rock | forms in layers (beds, strata) |
The ______ is the last layer formed and will be the youngest | top |
Clastic (fragmental) sedimentary rock | made up of pieces of sediment named by the size of sediment |
Crystalline /chemical sedimentary rock | left behind when water evaporates |
Metamorphic rock | From the Greek "meta" means change, "morph" means form |
Metamorphic rock | rocks that are changed by heat and pressure |
Metamorphic rock | characteristics: may look completely different than parent rock |
Metamorphic rock will become harder and denser because _____ | the depth of the Earth or the movement of the plates on the Earth has squished the rock |
Metamorphic rock looks (the same or different) than parent rock. | different |
Metamorphic rock- characteristics include _______ texture | crystal |
foliation | when the layers appear to align much like the pages in a book because of the pressure |
nonfoliated | no regular pattern of layers |
Types of metamorphism are ______ and ______ | contact and regional |
Contact metamorphism | rock that is in contact with magma |
Regional metamorphism | enormous pressure for either being very deep within the Earth or when large pieces of Earth's crust collide |
Weathering | the breaking apart of rocks, minerals, or any object into smaller pieces |
erosion | the movement of weathered pieces |
Relative dating | determining whether an object or event is younger or older than other objects of events |
Super position | principle that states that younger rocks lie above older rocks when the rock is undisturbed |
fault | a break in the Earth's crust along which blocks of the crust slid past each other |
intrusion | molten rocks from the Earth's interior that squeezes into existing rock and cools |
folding | when rock layers bend and buckle form Earth's internal forces |
tilting | when internal forces in the Earth slant rock layers without folding them |
Main layers of the Earth | crust, mantle, inner and outer core |
hydrosphere | water layer of the Earth |
atmosphere | gaseous layers of the Earth |
lithosphere | the upper/solid portion of the Earth, made of crust and top of mantle, divided into pieces called tectonic plates |
asthenosphere | soft, gooey layer of the mantle that the plates float along |
mesosphere | bottom layer of the mantle |
tectonic plates | pieces of the lithosphere that move around on top of the asthenosphere |
earthquakes | occur when tetonic plates rub or smash into each other |
seismology | the study of earthquakes |
epicenter | the point of the Earth's surface directly above an earthquake's starting point |
focus | the point inside the Earth where an earthquake begins |
Richter scale | measures the strength of the earthquake |
San Andreas fault | location in California where many earthquakes occur |
volcano | a mountain that forms when molten rock is forced to the Earth's surface |
Ring of Fire | plate boundaries surrounding the Pacific ocean where many volcanoes exist |