Geology 101 Knapp 1 – Flashcards
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Scientific Method
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A general procedure by which scientists propose and test hypothesis that explain some aspect of how the physical universe works. 1) collecting data 2) formulating a hypothesis 3) testing the hypothesis 4) stating conclusions
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hypothesis
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A testable prediction, often implied by a theory
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geologic record
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the information preserved in rock that have formed throughout time
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principle of uniformitarianism
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Earth processes occurring today are similar to those that occurred in the past.
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topography
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the general configuration of varying heights that gives shape to Earth's surface, which is measured with respect to sea level.
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seismic waves
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A ground vibration produced by an earthquake.
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Core
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mostly iron and nickel
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Mantle
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The region that forms the main bulk of Earth, between the crust and core, containing rocks of intermediate density, mostly compounds of oxygen with magnesium, Iron, and Silicon.
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Crust
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composed of low-density silicates, rich in aluminum and potassium
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Inner Core
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solid metallic sphere suspended within liquid outer core
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Outer Core
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liquid sphere surrounding solid inner core
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Earth system
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understanding Earth as an interaction of many systems (spheres)
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geosystems
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specialized subsystems that produce specific types of behaviors, such as climate change or mountain building.
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climate
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Describes an area's average weather over a long period of time. Also includes measures of how variable the weather has been.
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Lithosphere
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A rigid layer made up of the uppermost part of the mantle and the crust. One of four spheres into which scientists divide Earth.
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Asthenosphere
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Highly deformable (plastic/weak/ductile) upper mantle below lithosphere. Allows plates to move.
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Plate Tectonics
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The theory that explains how large pieces of the lithosphere, called plates, move and change shape.
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magnetic field
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The energy field created by the spinning of the inner and outer cores.
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geodynamo
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Geosystem phenomenon in which the iron-rich fluid is electrically charged, thus generating a magnetic field similar to an electromagnet.
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fossils
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traces of organisms preserved in the geologic record.
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continental drift
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large-scale movement of continents
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Pangea
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Wgener's supposed "super continent", before continental drift.
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seafloor spreading
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The process that creates new sea floor as plates move away from each other at the mid-ocean ridges. (Hess' theory)
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divergent boundaries
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plates move apart and new lithosphere is created (plate area increases) Ex: Mid-Ocean Ridges, African Great Rift boundaries
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convergent boundaries
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plates come together and one plate is recycled into the mantle (plate area decreases)
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transform faults
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plates slide horizontally past each other (plate area does not change).
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mid-ocean ridge
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undersea mountain chain that exhibits earth-quakes, volcanism, and rifting, all caused by the (stretching) forces of mantle CONVECTION that are pulling the two plates apart.
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O
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Oxygen (Mantle,
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Mg
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Magnesium (Mantle,
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Al
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Aluminum
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Fe
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Iron (Mantle, Core
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Si
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Silicon (Mantle,
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Ni
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Nickel (Core,
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spreading centers
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the seafloor spreads as magma wells up into the rifts to form new oceanic crust.
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Magma
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molten rock BELOW Earth's surface
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Lava
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Molten rock ABOVE Earth's surface
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Transform, Divergent, Convergent
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The three types of plate boundaries.
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Ocean-Ocean
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Convergent boundary (subduction zone) where one plate goes up, and the other goes down underneath. Water from subducted plate causes melting and generates volcanoes at surface. Ex: Japan
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Ocean-continent
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Convergent boundary (subduction zone) where continental crust overrides oceanic plate because it is lighter/less dense). Continent's edge is uplifted into a mountain chain parallel to deep sea trench. Also earthquakes and volcanoes. Ex: Andes
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Continent-continent
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Convergent boundary where both continents remain afloat, and the crust crumbles, creating high mountains and wide plateaus. Ex: Himalaya
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Transform Plate Boundary
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lithosphere is neither created, nor destroyed during the horizontal displacement between adjacent plates. Slide past each other.
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Subduction
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One plate going under another plate.
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Mantle Convection
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Drives plate-tectonics.
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reversed
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Oceanic crust that records negative magnetic anomalies formed when Earth's magnetic field was ______ from what it is today.
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isochrons
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On a map of oceanic crust, boundaries between normally and reversely magnetized oceanic crust are called ________.
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Minerals
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naturally occurring inorganic Characteristic Chemical Composition Distinct Physical Properties crystalline structure Ex: diamond, Gypsum, rock salt. COAL IS NOT A MINERAL (because it's organic)
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Element
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A pure substance that is made up of only one kind of atom, that cannot be separated by ordinary processes.
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Na
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Sodium
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Ca
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Calcium
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K
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Potassium
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Atom
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Smallest possible unit of an element.
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electrons
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# of ______ = # of protons
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Isotopes
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Atoms of the same element with different numbers of NEUTRONS.
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Ions
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When an atom loses or gains an ELECTRON to or from another atom.
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cations
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Positively charged Ions (LOSS of an electron)
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anion
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Negatively charged Ion (GAIN of an electron)
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Chemical bonds
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atoms of elements that make up compounds and are held together by -electrical forces of attraction between electrons and protons-.
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Ionic bonding
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attraction of opposite charges. Simplest and MOST COMMON chemical bond.
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Covalent bonding
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sharing of electrons in outer shells. Involves elements that don't readily form ions, forms stronger and more stable bond. Ex: Diamond = Carbon with covalent bonds
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Metallic bonding
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sharing of an electron CLOUD around several nuclei.
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Hardness, cleavage, fracture, luster, color, streak, density, crystal habit,
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Identify minerals according to:
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Hardness
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Resistance to scratching. Talc is softest, Diamond is hardest.
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cleavage
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Tendency to break along even planes. Best _____(s) have Ionic Bonds.
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Fracture
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Tendency to break along uneven, irregular planes.
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Luster
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The way a mineral reflects light.
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Color
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The first thing you notice, not always accurate.
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Streak
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The color of the powder left behind on a streak plate.
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Crystal habit
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Shape that the mineral takes on.
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10
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Sodium as an atomic # of 11, how many electrons will the sodium ion Na+ have?
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Ionic
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Cleavage in minerals is controlled by the ______ arrangement of atoms.
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Rocks
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Naturally occurring aggregates/combinations of one or more minerals. Ex: marble, granite, sandstone
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Mineralogy
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The study of relative proportions of constituent minerals and their properties. (ends with logy) Can be used to describe a rock.
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Texture
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Describes the sizes and shapes of its mineral crystals and the way they are assembled. Can be used to describe a rock.
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Solid, liquid, or gas
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All matter exists as either:
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Temperature and Pressure
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Increases with depth.
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Composition
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combination of elements.
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Igneous
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Type of rock that is cooled from MAGMA. Ex: Granite
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Sedimentary
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Type of rock that is the result of processes (weathering) ONLY on the SURFACE of Earth. Ex: Sandstone
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Metamorphic
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Rock formed under high temperatures and pressures in the DEEP crust. Recrystallization in SOLID state (does not melt). Ex: Gneiss
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Any rock type
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___ ____ ____ can be turned into any other type (igneous, sedimentary, metamorphic) via the rock cycle.
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Pressure, water content, rock composition
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Factors affecting melting of minerals: 1) P_________: when increased, melting point is raised. 2) W_____ C_______: When increased, lowers melting point. 3) R____ C___________: Felsic minerals melt at lower temperatures than Mafic minerals.
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Felsic
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Rich in Silicon (Si).
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Mafic
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Rich in Iron (Fe) and Magnesium (Mg). Ex: magnesium-ferric
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Intrusive rocks
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Rocks cooled inside the Earth. Often have larger crystals, cooled slowly.
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Extrusive rocks
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Rocks cooled on the surface of the Earth. Often have smaller crystals, cooled quickly.
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Plutons
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Large igneous bodies that form at depth in the Earth's crust.
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Intermediate
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Andesite is an example of an ___________ igneous rock.
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Utramafic
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Has the lowest silica content.
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Basalt
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Mafic lava that runs onto the surface, makes up most of the Hawaiian Islands.
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Clastic Sediments
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Accumulations of solid rock fragments produced by weathering of pre-existing rocks.
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Chemical sediments
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Accumulations of substances precipitated from ionic species in water.
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Biochemical sediments
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same as chemical, but with involvement of biologic organisms.
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Subsidence
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Sedimentary basins are formed by _______ (process), which includes: - compaction - cementation - diagenesis -recrystallization
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Compaction
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Removal of pore space and pore fluid (physical). A process that squeezes sediments together to form sedimentary rocks.
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Cementation
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Precipitation of new minerals between grains. (chemical). The process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock.
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Diagenesis
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All the processes that convert sediment into rock at low temperature and pressure (compaction and cementation).
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Recrystallization
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Change of mineral form due to chemical reactions in rocks during metamorphism (no melting involved)