geography lecture midterm

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greeks and geography
* 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
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physical geography
natural environment
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spatial science
physical and social science
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four spheres of earth
atmosphere, geographic/lithosphere, biosphere, hydrosphere
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atmosphere
gassesge
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geographic/lithosphere
land
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biosphere
life
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hydrosphere
water
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cyrosphere
ice
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global environmental change
natural and man made changesg
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globalization
interconnected world
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pattison
stated that modern geography is defined by four academic traditions
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four academic traditions
* spatial tradition
* area studies/regional
* man-land tradition
* earth science tradition
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spatial tradition
studying geographic phenomena in terms of spatial perspective
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area studies/regional
gleam a place in order to describe, differentiate, and define from other areas
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man land tradition
studying relationship between humans and the land
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earth science tradition
focus on how the planet’s location in the solar system impacts seasons and how spheres impact human lives on earth
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holistic nature of geography
* integrates a variety of subject matter
* integration makes geography holistic
* can be a strength and weakness
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j lewis robinson
stated that Pattinson’s model lacked a unifying focus
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five themes of geography
location, place, region, movement, human environment interaction
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absolute location
exact location
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relative location
next door, nearby, etc
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place
characterized by everything in it (physical or human characteristics)
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region
characterized by certain similar characteristics (political borders, physical characteristics)
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movement
how people, products, information, and ideas and spread from place to place
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human environment interaction
relationship between humans and the environment
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formal regions
government designated boundaries or defined by similar characteristics (chinatown, the corn belt, etc)
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functional regions
regions based on their functions (newspaper delivery area)
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vernacular regions
based on people’s perceptions (the south, the Middle East, etc)
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systems theory
study of collections of interacting objects as it applies in natural and cultural application
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relating to our environment
adapt, depend, and modify
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adapt
alter our needs to accommodate to the land
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depend
we use the land
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modify
we change the land
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importance of geography
* fundamental skill
* ties together diverse sciences
* understand conflict in world
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first geographers
* 4,000 years ago


* main purpose → to map landscape and human settlements
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aristotle
showed that the earth was a sphere using lunar eclipses
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lunar eclipse
earth’s shadow covers the moon
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eratosthenes
measured the circumference of earth
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earth’s circumference
40,233 km (25,000 miles)
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scientific method
a cylindrical model/process
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steps of the scientific method
* observe phenomena
* hypothesis
* create experiment
* make predictions
* conduct experiment
* conclusions
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geography and science
* 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
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mantle
composed of high density rock, largest layer
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upper mantle
* thin, rigid
* lithosphere
* asthenosphere
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lithosphere
uppermost, combo of crust and upper rigid mantle