Title: Chapter 2 Physical Geography: A Living Planet
1Chapter 2Physical Geography A Living Planet
2CONTINENTAL DRIFT THEORY
- Originally suggested by Francis Bacon in 1620
- Presented theory in 1912 by Alfred Wegner of
Germany - Theory states that all continents were once a
super continent that divided and slowly drifted
apart
3Where are we?
- 93,000,000 miles from the Sun
- 3rd Planet in from the Sun
- 24,900 miles in circumference and 7900 miles in
diameter - Only planet in Milky Way solar system that can
sustain human life
4THE MILKY WAY
- Our Solar system consist of the sun
- 8 planets
- 1 dwarf planet (Pluto)
- Other celestial bodies that orbit the sun
- Comets gt spheres covered with ice and dust that
leave trails of vapor as they race through space - Asteroids gt large chunks of rocky material found
in space - By size Pluto (dwarf), Mercury, Mars, Venus,
Earth, Neptune, Uranus, Saturn, Jupiter
5Section 1 The Earth Inside and Out
- 1. The earth is the only living planet
- Continents
- landmasses above water on earth
6- 2. The earth consists of
- plates
- that float
7- 3. The theory of continental drift explains the
formation of continents
8Inside the Earth
- Core
- center of the earth (inner core- liquid iron
and nickel outer core solid iron and nickel) - Mantle
- several layers surrounding the core
- Crust
- thin layer of rock at the earths surface
9Biosphere
- The part of the earth where plants and animals
live (atmosphere, lithosphere and hydrosphere)
10On and Above the Earth
- Atmosphere
- layer of gases surrounding the earth (contains
oxygen, protects the earth from radiation and
space debris, and provides a medium for weather
and climate
11Lithosphere
- Solid rock portion of the earth (includes crust
and uppermost mantle, ocean floor, etc.)
12Hydrosphere
- Made up of water elements of the earth (oceans,
seas, rivers, lakes and water in the atmosphere)
13Section 2 Bodies of Water and Landforms
- Human Perspective
- The earth is unlike any other observable planet
in our solar system. It is a living planet. - Where there is water there is LIFE.
14Section 2 Bodies of Water and Landforms
The ocean is interconnected and covers over 70
of the earth. Divided into 4 main parts.
Pacific (largest), Atlantic, Arctic and Indian
15Ocean Movements
- Currents- like rivers flowing through the ocean
- Waves- swells produced by winds
- Tides - regular rises and falls of the ocean
created by the gravitational pull of the moon or
the sun
16MOTION OF THE OCEAN
- The ocean distributes heat.
- Winds blow over the ocean and are either heated
or cooled by the water, moderating the
temperature of the air over the land.
17Hydrologic (water) Cycle
- The water on earth is continuously circulated
between the atmosphere, the oceans, and the earth
18LAKES, RIVERS, STREAMS
- Lakes hold more than 95 of all fresh water on
earth. - Rivers and streams
- move water to or from
- larger bodies of water.
19LAKES, RIVERS, STREAMS
- Saltwater lakes are created when creeks rivers
carry salts - into a lake, and there is no outlet to carry the
salt away. - Largest Caspian Sea (West Asia)
20- Drainage Basin -
- Area drained by a major river and its tributaries
21Ground Water water held in the pores of
rocks Water Table the rim level at which rocks
are saturated
22Oceanic Landforms (topography)
- The ocean floor and the continents have a
continental shelf and slope - The ocean floor is similar to the land above
water.
23continental shelf
24Continental Shelf
- Earths surface from the edge of a continent to
the deep part of the ocean
25Continental Landforms
- Naturally formed features on the surface of the
earth are landforms
26Topography Relief
- Relief refers to the difference in elevation of a
landform from lowest to highest point - Mountains, hills, plains, canyons
- The combination of the surface shape and
composition of the landforms and their
distribution in a region gt topography - Topographic Maps show the landforms with their
vertical dimensions and their relationship to
other landforms.
27Section 3 Internal Forces Shaping the Earth
- The earths crust consists of number of tectonic
plates - tectonic plates - enormous moving pieces of the
earths lithosphere - Spreading subduction collision sliding past
each other in a shearing motion
28- Movement
- of the plates
- produces
- earthquakes
- and volcanoes
- Fault fracture in the earths crust where
plates move past each other
29Types of boundary movements
- Divergent plates move apart, spreading
horizontally (i.e. Saudi Arabia Egypt making
Red sea wider)
30Types of boundary movements
- Convergent Plates collide, causing either one
plate to dive under the other or the edges of
both plates to crumple (i.e. South Asia forming
the Himalayas)
31Types of boundary movements
- Transform plates slide past each other (i.e.
San Andreas Fault in California)
32Volcanoes crack in the earths surface where
magma and gases pour outBenefits gt fertile soil
energy
Lava magma that has reached the earths surface
33- Earthquake Violent movement of the earth as the
plates grind or slip past each other at a fault - 95 around Pacific Rim (Ring of Fire)
- Along plate boundaries
- Seismograph
- measures the size of the waves created by and
earthquake - Largest Earthquake measuredgt Kermadec Island, 8.9
34Epicenter
- Point directly above the focus of an earthquake
on the earths surface - Richter Scale
- uses information collected by seismographs to
determine the strength of an earthquake
35DAMAGE
- Landslides
- Fires
- Collapsed Buildings
- Tsunami (speeds up to 450 mph and waves 100 feet
tall)
36Tsunami
- A giant wave in the ocean caused by an
underground earthquake
37The Ring of Fire
- The most active volcano and earthquake zone on
earth
38(No Transcript)
39Hot Spots
- Volcanoes that are far from the margins of the
tectonic plates are located on Hot Spots. - Hot springs geysers are other features that
indicate areas where the crust is thin.
40External Forces Shaping the Earth
- Human Perspective
- In Egypt, a seasonal dry wind is called Khamsin
(50) for the number of days the season occurs.
These wind-driven sandstorms cause serious
problem for the people of the region.
41External Forces Shaping the Earth
- Weathering and erosion alter the surface of the
earth - Weathering physical and chemical processes that
change the characteristics of rock on or near the
earths surface
42- Sediment Small pieces of rock created by
weathering (mud, sand or silt) - Mechanical Weathering
- processes that break rock into smaller pieces
(doesnt change the composition of rock, but the
size) - Example road construction
- 4 causes gt human activity,
- plants, frost, ice crystal in
- cracks of rocks
43- Chemical Weathering
- occurs when rock is changed into a new substance
as a result of interaction between elements in
the air or water and minerals - (example iron rusting)
44Erosion
- Occurs when weathered material is moved by the
action of wind, water, ice and gravity
45Water Erosion
- The motion picks up loose material and moves it
downstream - Delta
- sediment is deposited in a fan-like landform when
a river enters an ocean
46Wind erosion
- Wind speeds have to reach 11 mph before fine
sediments can be moved. - Depending on the types of wind, different types
of landforms can be formed - Loess, sand dunes, rock structures.
47wind erosion
Loess windblown silt and clay sediment that
produces very fertile soil
48Glacial Erosion
- Glacier - a large, long-lasting mass of ice that
moves because of gravity - (Form in mountainous regions)
- Glaciation
- changing of landforms by slowly moving glaciers
- Moraine
- rocks left behind from a glacier that form a
ridge or hill
49BUILDING SOIL
- HUMUS -
- Organic material in the soil.
- Esker gt snakelike ridge
- Created by melted ice
50- Kettle gt depression in the ground created by
blocks of trapped ice in the sediment that melts.
They can fill with water to form lakes.
51- Weathering and erosion help form soil. Soil
consist of a loose mixture of weathered rock,
organic matter, air, and water that supports
plant growth - Factors that determine
- soil fertility
- Parent Material
- Relief
- Organisms
- Climate
- Time
52- The variety and the climates in which they are
found determine the types of vegetation that
can grow in a location. Agricultural activities,
such as farming, ranching, and herding, depend on
this complex relationship.