* first civilization to practice 1st form of physical geography * interested in earth’s size, shape, and geography * first to give it a name and declare it a science
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geography
* devoted to studying lands, features, inhabitants, and phenomenon of earth * Eratosthenes * how things differ/interconnected from place to place
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human geography
study of communities, cultures, economies, interactions by studying their relations with space and place
* data collection and eliminating explanations * theories developed through method, review, uncertainty
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scientific method importance
* develop ideas * natural world is predictable and constant * data can prove/disprove hypothesis/multihypotheses * new information expands ideas
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things to remember about scientific method
* science doesn’t prove anything * a theory isn’t a guess or a hunch * there will always be research that needs to be done * scientific acceptance is based on evidence * there will always be controvery
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truth and reality
* scientific method * agreed upon definitions in science
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belief
idea that is not confirmed by science
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principle
* ideas based on scientific rules and laws * fundamental truths, foundation for other studies * scientists use these when making predictions
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fact
confirmed many times, but it could still be wrong
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law
description of how something is happening, but doesn’t explain whyt
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theory
explanation of some aspect of the natural world through well-substantiated facts, tested hypotheses, and laws
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theories of universe’s demise
the Big Crunch, the big freeze, the big rip, the big suck, the big bouncet
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the Big Crunch
universe stops expanding, gravity takes dark matter and space gets smaller
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the big rip
the universe keeps expanding until everything binding the universe rips and we all float away
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the big freeze
everything floats away until earth is alone and the earth freezes
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the big suck
a giant black hole sucks the earth, alternate universe inside
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the big bounce
the world ends when it crunches, but everything restarts
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formation of universe
1. solar nebula contracts 2. as solar nebula shrinks, motion causes it to flatten 3. nebula is disk of matter w/ concentration near center 4. formation of profusion, solid particles condense as nebula cools, increase to planetesimals
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planetesimals
building blocks of planets
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solar system
* sun isn’t the exact, mathematical center * 8 plants * 4 jovian 4 terrestial * open system * earth is 3rd from the sun
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solar system origins
* 4.5-5 billion years ago (4.72 billion) * started as nebula, contracted into protostar, then turned into our sun
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earth systems
interactions between environmental sphereso
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closed system
isolated from outside influence
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open system
energy and matter and exchanged across systems
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interconnected systems
systems influence other systems (glacier systems)e
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equilibrium
inputs and outputs in balance
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feedback loops
outputs feedbacks as inputs reinforcing change
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positive feedback loop
change within system that continues in one direction
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negative feedback loop
inhibits system from changing
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theories of universe origins
* big bang * creation * intelligent design (a religious) * steady state * black hole * multiverse
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geologic time scale
* vast periods of time over which geological processes occur * life represents a tenth of a second of an entire year
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primary
volcanic
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secondary
hardened sedimentary
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territory and quaternary
surface soils
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units of time
eons, eras, periods, epochs
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eons
* longest unit * Phanerozoic and precambrian
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phanerozoic
* time of visible life * 541 million years ago
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precambrian
* 88% of earth’s history * cenozoic, mesozoic, Paleozoic
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three major eras
cenozoic, mesozoic, paleozoicc
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cenozoic
age of recent life
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mesozoic
age of middle life
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paleozoic
age of ancient life
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units
eons, eras, periods, epochs
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radiometric dating
measuring decay of radioactive elements in some rocks
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absolute age
exact number of years since layers formed or geologic event took placere
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native age
relative dating doesn’t equal absolute agepr
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principle of original horizontality
sediments accumulate in flat, horizontal layer
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principle of superposition
oldest is the bottom layer and vice versa
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principle of cross cutting relationships
if fault or igneous intrusion cuts through, cross cutting occurred after layer formed
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unconformities
interruption in rock record
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anthropocene
current epoch of geologic time
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crust
outermost shell of earth
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oceanic crust
ocean, denser rocks
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continental crust
* significantly thicker * large land masses * preserved longer * low density * oldest crust doesn’t equal earth’s age
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mohorovic discontinuity
narrow zone of change in mineral composition in crust