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modern estimate of age of earth |
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organize earths history into blocks of time based on history & evolution of life on earth |
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radio active elements decay at known rates |
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largest subdivision on geologic time scale |
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4.65 billion-542 million years ago |
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subdivision of eon named on dominent life forms boundaries mass extinction |
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phanerozoic eon has how many eras and what are they |
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paleozoic mesozoic cenozoic |
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"recent life" 65-0(present) MYA |
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cenozoic era has what 2 periods |
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tertiary period has what to epochs |
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smallest division of matter |
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positively charged particle, mass = 1Amu |
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negatively charged particle that orbit nucleus, no mass = 0 |
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1 type of atom, defined by number of protons in nucleus |
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# of protons + # of neutrons |
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same number of protons, different number of neutrons |
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2 or more elements combined together ex. H20 |
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oxygen, silica,aluminum, iron, calcium, sodium, potassium, magnesium, other |
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70% of earth made of these 2 elements |
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elements or compounds that are the building blocks of rocks |
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1. naturally occuring 2. inorganic-not created by biological process 3. solid 4. crystalline structure-atoms arranged in 3-D frame work 5. set chemical formula ex. NaCL |
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physical properties of a mineral |
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crystal form, luster, streak, color, hardness, cleavage, fracture, and other properties - ex. specific gravity, ratio of weight to volume, reaction with acid, magnetic, taste, flouroscene/phosphorescense |
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crystal form (physical property of mineral) |
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shape crystal grows in reflection of internal crystalline structure |
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luster (physical property of mineral) |
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the way mineral interacts with light metallic- look like metal non metallic-all other lusters ex. glassy,earthy,silky,resinous,pearly |
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streak (physical property of mineral) |
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color of mineral in powder form rub on ceramic plate nonmetallic make light metallic make dark |
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color (physical property of mineral) |
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unreliable physical property (transparent/translucent minerals) trace elements better for opaque or metallic minerals |
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hardness (physical property of mineral) |
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resistence of mineral to abrasion mohs scale-compare mineral 1. talc 2. gypsum 3. calcite 4. flolorite 5. apatite 6. ortoclase(feldspar) 7. qaurtz 8. topaz 9. corundum 10. diamond |
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cleavage (physical property of mineral) |
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minerals break along lines of weakness in crystalline structure # of surfaces, angle relationship |
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fracture (physical property of mineral) |
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distinct/other forms when broken conchoidal-glass break |
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other properties (physical property of mineral) |
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specific gravity ratio of weight to volume reaction with acid magnetic taste flourescene/phosphorescense |
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one or more minerals or mineral like substance |
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forms by the cooling of molten rock (lava or magma) |
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felsic composition >65% silica, high in K & Na ex. qaurtz, k-feldspar, & micas |
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45-55% silica high Fe,Mg,& Ca ex. olovine,amphiboles,plagioclase feldspar |
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two types of igneous rock |
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cooled beneath earths surface large crystals granite-felsic gabbro-mafic diorite-intermediate |
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cool at earths surface small crystals rhyolite-felsic basalt-mafic andesite-intermediate obsidian-glass pumice-woven glass Tuff-rock made of volcanic ash and pyroclastics |
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rocks that form at earths surface result from water,wind,ice & gravity&biological |
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made of fragments of rocks |
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grain size of clastic rocks |
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>2mm gravel-breccia or conglomerate .625-2mm sand-sandstone .0004-.0625mm=silt-siltstone <.0004= clay-mud shale |
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rocks that form by the precipitation of minerals by biologic entities or precipition out of water |
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altered by heat and pressure |
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creates a new mineral, new texture shale->slate->schist->gneiss ^ in order of higher heat and pressure |
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break down of rock by physical or chemical means |
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breakdown of rock by mechanical means break into smaller peices without altering chemical composition of rock |
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mechanical break down of rock caused by formation of ice crystals |
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breakdown of rocks by chemical reactions change composition of rock water always involved |
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a reaction with oxygen in the presence of water |
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reduces grain size create new minerals |
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thin layer that is a mixture of mineral and organic matter that can support living plants complex mix of liquids,gases,organic material,minerals,&organisms |
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parent material, climate, topography organisms, and time |
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parent material (soil forming factor) |
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rock regolith or sediment that the soil is developed in |
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permeability (soil forming factor) |
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how connected are the pore space |
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temperature (soil forming factor) |
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control availability of liquid H20 control speed of biological & chemical reaction |
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precipitation (soil forming factor) |
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amount & type provides H20 for biological & chemical processes |
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topography (soil forming factor) |
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shape of land surface affects drainage of soils rate of erosion |
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organisms(soil forming factor) |
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vegetation micro-organisms animals physical weathering adds organic material |
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time (soil forming factor) |
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increase in thickness develope properties & structure through time |
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color humus content texture structure chemical properties mineral composition |
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layers within soils that are differentiated by their physical and chemical properties |
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description of thickness& horizons present |
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physical properties dominated by organic material |
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"top soil" mineral horizon high concentration of organic material |
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leached of carbonates,iron&aluminum oxides, and clay |
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where material from above accumulates |
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loose, unconsolidated parent material |
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classify based on observable soil characteristics |
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earth has layers that differ in density heaviest elements are in the center |
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most dense elements are located here |
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liquid convection currents |
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thick layer 82% of earth by volume |
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Asthenosphere small amount of molten rock/melt
lithosphere rigid solid |
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oceanic crust mafic composition |
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felsic composition thickest |
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earth's crust is broken into plates that move relative to one another |
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plates moving away from each other new crust formed |
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convergent plate boundary |
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2 plates move towards eachother |
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2 plates have unequal densities denser plate pushed under less dense plate create chains of volcanoes |
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continent to continent collision |
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plates have same density neither can be pushed under and destroyed build mountain chains |
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plates move past one another no volcanoes are earthquakes |
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plum of heat from deep in earth "burns" through crust creating volcanoes |
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where can volcanoes be found |
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mid ocean ridges, rift valleys,subduction zones, hotspots |
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low viscosity high temp ropey appearance |
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high viscosity low temp jagged and crumbly appearance |
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Aa, Pahoehoe->basaltic-mafic=45-55% silica Aa->Andesitic-intermediate=55-65% silica Aa->rhyolitic-felsic=>65%silica |
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solids ejected during an eruption |
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volcano explosivity index |
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volume of material ejected, height of plum, and furation& frequency of eruptions |
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0-1 mostly lava gentle eruption |
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gentle mostly gas & pyroclastics weekly basis |
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steam, pyroclastics, & gas viscous lava after yearly-decade |
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4-6 pyroclastics plume 10-25 km century |
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large,broad gently sloping volcano |
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flat lying layers pf basalt, from plateous |
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steepsided composed of alternating layers of pyroclastics and lava |
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depression caused by the collapse or partial collapse of a volcano |
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mass or plug of lava right on vent |
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small steep sided colcano pyroclastics lava flows,break and exit at base |
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lava flows, ashfall, pyroclastic flow, lahar, large release of gasses,tsunami |
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cracks in the earth along which movement occurs |
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release of energy from fault rupture or movement |
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actual location in earths crust where the rock ruptured |
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location on earths surface directly above the focus |
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energy from earthquake radiates out in all directions |
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compressional wave rock movement is parallel to the wave movement |
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shear waves rock movement is perpendicular to wave movement |
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travel along earths surface |
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device used to measure seismic waves |
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energy released during an earthquake |
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amplitude(height of the largest peak recorded |
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1 step on scale = 10x the amplitude, 32x the energy |
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length of fault rupture, depth, strength of rock, and length of movement |
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destructiveness of an earthquake as perceptible moving, shaking, and damage to human structure |
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destructiveness of human structres and on eye witness accounts of ground movement |
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ground shaking and displacement, liquefecation(while earth is shaking satured sediments near surface turn fluid, landslides, and tsunamis, fires,floods, spread of disease |
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(while earth is shaking satured sediments near surface turn fluid |
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channelized flow of water on earths surface |
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runoff, discharge from groundwater |
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area of land that contributes water to a stream network |
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a topographically high are that seperates drainage basins |
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arrangement of streams in a drainage basin controlled by the type of structures or rock under the stream |
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volume of water flowing through a givenlocation or cross section of a stream per unit time |
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elevation of water surface above a known elevation |
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level of water to the channel |
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channel is completely filled with water |
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water spills out to surrounding area |
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changes in stream vs time |
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sediment moving in stream |
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transported in contact with bottom of stream pushed or rolled jumping |
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transported in water silts and clays |
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floating along surface organic stuff |
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size of largest particle a stream can transport |
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total volume of sediment it can transport |
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where water is transported |
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water in pore spaceof soil or rock |
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body of saturated rock or sediment that is capable of yeilding significant quantities of water |
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body of saturated rock or sediment that is not capable of yeilding signifacant water |
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landscape that is shaped by the solution of bedrock |
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karst landforms on surface |
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sink hole, polje, disappearing or sinking streams,springs, tower karst |
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sinkholes merge together to form valleys |
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disappearing or sinking streams |
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surface streams enter sink and continue underground |
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groundwater system discharges into the surface system |
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steepsided limestone hill/towers |
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subsurface karst landforms |
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form from ceiling downwards |
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stalagmite & stalactite grow together |
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curved or curly stalactites ribbons, curtains, drapes |
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mountain that have been sculpted by glaciers |
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set of cirques downside of mountain |
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series of tarns linked together by short streams |
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steepsided flat, bottemed valley formd by glacier |
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u shaped valley that has been flooded by sea |
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u shaped valley of a tributary glacier meets the main u shaped valley of trunk glacier |
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pyramid shaped mountain peak formed by the erosion of several cirques |
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knife like ridge between two cirques or 2 u shaped valleys |
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ridges of sediment, built by ice at the edge of the glacier |
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rolling hills & depressions |
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formed along sides of glaciers between the ice & the valley wall |
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moraine that forms between two lobes of an ice sheet |
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streamlined hills formed under ice sheet |
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sinuous ridge formed undr the ice sheet |
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hills formed by inversion of topography |
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closed depression formed by the inversion of topography |
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outwash deposits extending from front of ice sheet |
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features that are formed from cold (ice) |
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driven by prevailing winds |
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driven by density differences |
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sediment currents that sweep down continental slopes onto sea floor |
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wind pushes on surface of water |
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water molecule movement in water |
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depth to which water is distributed |
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wave fronts intersect the shor at an angle |
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weak current that moves parrallel to the shore |
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sediment moving parallel to the shore with the longshore current |
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longshore current escapes seaward |
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mass of water pushed infort of a storm |
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cyclic fluctuation of sealevel caused by the gravitational pull of moon & sun on oceans |
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where wave energy decreases and longshore currents slow |
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ridges that mark high extent wave action |
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extention or buildup of beach by longshore current across an inlet |
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build up of sediment behind a breakwater or obstacle |
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long low islands of sediment that run parallel to shore |
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stream that enters ocean/ lake |
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sediment being carried by wave |
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pillar of rock that sticks out of ocean |
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mass of ice and snow that flows under its own weight |
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processes that removed mass from glacier melting, carving, sublimation |
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leaves cirque and flows down valley, form into networks |
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glacier that enters the ocean |
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when glacier extends outside the confines of valley, they spread or fan out |
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large ice masses on landscape less that 50,000 km^2 |
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deposited directly from glacial ice |
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sediment deposited by glacial meltwater |
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shore parallel structures |
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absorb and reflect wave energy |
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shore perpendicular structure |
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disrupt the longshore current |
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a pair of groins that protect an inlet or navigation to a harbor |
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artificially add/supply sand to the beach to creat a positive budget/ balance |
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