ESSENTIALS of GEOGRAPHY. Physical Geography (Geog. 300) Prof. Hugh Howard American River College

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ESSENTIALS of GEOGRAPHY Physical Geography (Geog. 300) Prof. Hugh Howard American River College

GEOGRAPHY

GEOGRAPHY Earth description, or study of Earth Describes the natural environment and human interaction with it Spatial science, having to do with physical space Deals with spatial distributions and spatial relationships of Earth features and phenomena

GEOGRAPHY Ancient Greeks didn t invent geography, but they formalized it as a field of study Organized all knowledge into Geography and Cosmography Eratosthenes coined the term geography in the 3 rd century BCE He was the first person to calculate the circumference of Earth (using geometry) Geographic library at Alexandria

GEOGRAPHY Geography has two major subfields Physical Weather, climate, geology, hydrology, soils, etc. The emphasis of this course Human Cultural, economic, political

Major Subfields of Geography

GEOGRAPHY Synthesizes other fields of study Geology, hydrology, meteorology, etc. Geography acts to bring specialized fields together to find relationships between them

THE SCIENTIFIC METHOD

SCIENTIFIC METHOD Method for investigating phenomena and acquiring new knowledge A hypothesis is formed A proposed explanation for something Is formed by making a general statement from specific observations Mt. Shasta is a volcano. It is made of lava. Therefore, all volcanoes are made of lava.

SCIENTIFIC METHOD Hypotheses are based on inductive reasoning Generalizing from specific observations Allows for the conclusion to be false Mt. Shasta is a volcano. It is very large. Therefore, all volcanoes are very large. Hypotheses can be supported or rejected on a case-by-case basis

SCIENTIFIC METHOD Hypotheses are tested using deductive reasoning Reasoning from a general statement to a logical conclusion Mt. Shasta is a volcano. It is formed from lava. Therefore, all volcanoes are formed from lava. The hypothesis is accepted Experiments performed on all known volcanoes show that they are all made of lava.

SCIENTIFIC METHOD Hypotheses are tested using deductive reasoning Reasoning from a general statement to a logical conclusion Mt. Shasta is a volcano. It is very large. Therefore, all volcanoes are very large. The hypothesis is rejected Experiments performed on all known volcanoes show that they vary in size.

The Scientific Method A Theory Is a well-substantiated explanation acquired through the scientific method, and repeatedly confirmed through observation and experimentation. There is a very high probability that it is true.

SYSTEMS and MODELS

SYSTEM Set of related objects or events Useful in identifying relationships and interactions between components Used by geographers to organize information Open System Allows exchange of energy and matter (a tree)

Open System

Earth SYSTEM Is an open system all components interact

Earth SYSTEM Is a closed system in the context of space Allows exchange of energy only (really?)

MODEL Simplified, idealized representation of reality Maps and globes as models Physical or computer Allow us to see the most prominent, or important aspects of a system

Models of Earth

EARTH as a SYSTEM: The FOUR SPHERES

Atmosphere The FOUR SPHERES Extends up 300 miles Uneven solar heating keep it in constant motion, causing weather Lithosphere The rock layer Earth s outer shell, including the continents and ocean floors

The FOUR SPHERES Hydrosphere All water on and in the lithosphere Oceans constitute the largest component: 71% of Earth s surface Biosphere Life Layer - all living things We ll focus less on the biosphere than on the first three spheres

REGIONAL SUB-SYSTEMS: All four spheres can be studied within a particular geographic region Earth s Four Spheres

The SPHERICAL EARTH

SHAPE of EARTH Ancient Greeks believed that Earth was a sphere Ships disappeared over the horizon Lunar eclipses provided clues They believed the sphere to be a perfect form, appropriate for Earth Earth is not a perfect sphere It is spherical

The Spherical Earth

Half of a sphere HEMISPHERES Earth can be divided in many ways Northern and Southern Defined by the equator 70% of land is in the northern 90% of the human population is in the northern

HEMISPHERES Eastern and Western Defined by humans, rather than by physical principles International Meridian Conference, 1884, Washington, D.C. The Prime Meridian (0 degrees longitude) passes through Greenwich, England

The Four Hemispheres

Land and Water HEMISPHERES Land hemisphere centered on Africa Water centered on the Pacific The Water Hemisphere

CONTINENTS and OCEANS

CONTINENTS Continents Large, continuous, discrete masses of land Six continents Africa, Antarctica, Australia, N. America, S. America, Eurasia Europe is not a continent, but part of Eurasia It can be considered a sub-continent, or cultural region

Oceans OCEANS Large bodies of saline water Five oceans Arctic, Atlantic, Indian, Pacific, Southern Further subdivisions are made N. Atlantic and S. Atlantic, etc. Really only one global ocean

Continents and Oceans

AFRICA The mother continent for humans Second largest ( 20% of land area) Center of land hemisphere Straddles equator Plateau continent Much is over 3,000 ft, but large mountain ranges are uncommon

Africa

ANTARCTICA Home to the South Pole Second smallest ( 9% of land area) Surrounded by the Southern Ocean World s largest ice sheet Population 1,000-4,000 Scientists and support workers

Antarctica

AUSTRALIA Smallest ( 6% of land area) Great Dividing Range Lowest and flattest continent Highest point is only 7,316 ft Interior is almost completely uninhabited

Australia

Australia 2% of total population lives in yellow area

NORTH AMERICA Home! 17% of land area Great Mountain Ranges Rocky Mountains, Sierra Nevada, Cascade, Appalachians Great Plains Mississippi/Missouri Rivers and basins

North America

SOUTH AMERICA Last continent to be settled by humans 12% of land area Andes Earth s longest mountain range Amazon Earth s longest river Angel Falls Earth s highest waterfall

South America

EURASIA Largest ( 36% of land area) Himalaya Earth s tallest mountain range Almost 5.5 miles high, >29,000ft Alps Europe s greatest mountain range Densely populated river plains Ganges, Yellow, Yangzi

Eurasia

THE GEOGRAPHIC GRID

The GEOGRAPHIC GRID System for locating places on Earth Meridians Lines that stretch from north to south pole Prime Meridian passes through Greenwich Parallels Circles that intersect meridians at right angles, but are parallel to themselves Equator is a parallel

Meridians

Parallels

DEGREES Ancient Babylonians divided the circle into 360 equal parts Degrees! This system was applied to meridians and parallels Allows us to describe any location on Earth

DEGREES Degrees are too coarse to allow precise descriptions of location, so refinements were made Degrees, Minutes, and Seconds Angles, not units of time 60 (minutes) in 1 (degree) 60 (seconds) in 1 (minute) 3,600 (seconds) in 1 (degree)

LONGITUDE A measurement, in degrees, E or W of the Prime Meridian (Greenwich) 0-180 East or West One degree of longitude is 69 mi (111 km) at the equator and 0 mi at the poles. Sacramento: 121 28 W

Longitude

LATITUDE A measurement, in degrees, north or south of the equator (a parallel) 0-90 North or South One degree of latitude is 69 mi (111 km) anywhere on Earth Latitude: ladder, or lattice Sacramento: 38 33 N

Latitude

Latitudinal Zones

GLOBAL TIME

TIME and the GRID Earth completes one rotation every day, or every 24 hours Because Earth is composed of 360 degrees of longitude One hour of time corresponds with 15 degrees of longitude (360 /24 hours = 15 /hour)

TIME and the GRID Standard Meridians divide Earth into one hour zones The sun moves 15 in the sky every hour

SOLAR NOON Time when the sun reaches its highest point above a particular place on Earth Actual noon (differs from clock noon) Different for every longitude Earlier for Sacramento than for San Francisco But our clocks tell us that noon is at the same time in both places

TIME ZONES Regions 15 wide that share a common Standard Time Solar noon of the center of each zone is used throughout the zone Simplifies time scheduling Zones are actually irregular due to political and natural boundaries

Time Zones International Date Line: If traveling westward, you advance to the next day. If traveling eastward, you repeat the same day.

DAYLIGHT SAVING TIME The advancement of local times by one hour in spring and summer Gains more daylight in the evenings Designed to reduce energy consumption after dark (artificial lighting used to be a primary energy drain) Second Sunday in March First Sunday in November (8 months)

Daylight Saving Time

MAPS and MAP PROJECTIONS

MAPS Reduced, simplified version of geographic reality Allow us to communicate geographic information Predate written language Maps represent the spherical Earth on a flat surface, or plane

Maps

MAP PROJECTION The arrangement of Earth s spherical surface on a plane Projections can be classified according to geometric properties Planar Cylindrical Conic

Planar Map Projection

Cylindrical Map Projection

Conic Map Projection

MAP PROJECTION The projection process always distorts the continents and oceans Orange peel example The map maker can choose a specific type of projection that will be appropriate for a particular map Equal Area Conformal

MAP PROJECTION Equal Area Projection Retains the property of area Areas are shown at their correct sizes in relation to other areas (shape is distorted) Conformal Projection Retains the property of shape Shapes of areas and lines are correct (area is distorted)

Equal Area Map Projection (Eckert IV)

Equal Area Map Projection (Sinusoidal)

Conformal Map Projection (Mercator)

Conformal Map Projection (Lambert)

MAP SCALE

MAP SCALE A ratio (fraction) of map distance over Earth distance The representative fraction M a p d i s t a n c e E a r t h d i s t a n c e 1 24, 000 o r 1 : 2 4, 0 0 0 Unitless: any unit of measure can be inserted

MAP SCALE THE REPRESENTATIVE FRACTION (R.F.) 1:5,000,000 1:5,000,000 (larger scale) 1:20,000,000 1:20,000,000 (smaller scale) O R E G O N Smaller Area Greater Detail Greater Detail Larger Area Lesser Detail Larger Area Lesser Detail

GEOGRAPHIC TECHNOLOGIES

GEOGRAPHIC TECHNOLOGIES Technologies that allow us to examine and analyze geography Global Positioning System (GPS) Remote Sensing Geographic Information Systems (GIS) Computer-based fields that offer career paths

Global Positioning System (GPS)

Remote Sensing

Geographic Information Systems (GIS)

Geographic Information Systems (GIS)

Geographic Information Systems (GIS)

Geographic Information Systems (GIS)

Geographic Information Systems (GIS)

ESSENTIALS of GEOGRAPHY Physical Geography (Geog. 300) Prof. Hugh Howard American River College