the physical world chapter 2. our solar system earth is part of a larger physical system that...
TRANSCRIPT
The Physical World
Chapter 2
Our Solar SystemEarth is part of a larger physical system
that contains other planets, moons and stars.
The PlanetsPlanets – largest objects in the solar systemDwarf planets – small round bodies that
orbit the sun, but have not cleared the area around their orbits of other orbiting bodies.
Terrestrial Planets – have solid, rocky crusts. Ex. Mars, Earth, Venus, Mercury.
Gas Giant Planets – More gaseous and less dense planets. Ex. Jupiter, Saturn, Uranus and Neptune
Asteroids, Comets and MeteoroidsAsteroids – small, irregularly shaped,
planet-like objectsComets – made mostly of icy dust particles
an frozen gases, look like bright balls with long, feathery tails.
Meteoroids – chunks of space debris, chunks of rock and iron.
Getting to Know EarthEarth’s surface is a complex mix of
landforms and water systems
Water, land and AirHydrosphere – surface of the earth made
up of water, about 70 percentLithosphere – the earths crust, about 30
percent of the earths surfaceAtmosphere – layer of gases extending
above the planets surface.Biosphere – the part of the earth that
supports life, on or close to the earths surface or in the atmosphere.
LandformsLandforms – natural features of the earth’s
surface. Continental Shelf – underwater extension of
the coast. Continental shelves slope out from land.
Continental Slope – sharp drop off to the ocean floor
Earth’s Heights and DepthsHighest Point – Mount Everest – 29,028 ftLowest Point – Mariana Trench – 35,827 ft
below sea level
2. Forces of ChangeThe Earth’s internal and external structure,
including the tectonic plates, is responsible for the creation of the continents, oceans and mountain ranges.
A Layered PlanetCore – hot, solid center of EarthMantle – thick layer of hot dense rock,
middle layer of earthCrust – rocky shell forming the Earth’s
surface
Plate MovementContinental Drift – theory that the
continents were once joined and then slowly drifted apart
Pangaea – SupercontinentPlate Tectonics – scientists theorize that
plates moving slowly around the globe have produced Earth’s largest features
Magma – molten rock
Internal Forces of ChangePlate Tectonics is responsible for folding,
lifting, bending and breaking parts of the Earth’s surface.
Colliding and Spreading PlatesMountains are formed in areas where giant
continental plates collide. Subduction – heavier sea plate dives
beneath the lighter continental plate. Accretion – as sea plate slides under
continental plate, debris buildup causes continents to grow outward.
Spreading – sea plates pull apart.
Folds and FaultsFolds – bends in layers of rock.Faults – cracks in earths surface.Faulting – occurs when earth cannot be
bent any further, crust cracks and breaks into huge blocks.
EarthquakesEarthquakes are sudden, violent
movements of tectonic plates along a fault line.
Volcanic EruptionsVolcanoes are mountains formed by lava or
by magma that breaks through the Earth’s crust.
External Forces of ChangeExternal forces such as weathering and
erosion also shape the surface of the Earth.
WeatheringWeathering – breaks down rocksErosion – wears away the Earths surface
Glacial ErosionGlaciers – large bodies of ice that move
across the Earth’s surface.Glacial movement changes the landscape.Moraines – large piles of rocks and debris
left behind by glaciersSheet glaciers – flag, broad sheets of ice.
Ex. Greenland and Antarctica. Mountain glaciers – located in high
mountain valleys where the climate is cold.
Water ErosionWater erosion begins when spring water
and rainwater flow downhill in streams, cutting into the land and wearing away the soil and rock.
Oceans also cause erosion by pounding the coastlines with their waves.
3. Earth’s Water
The Water CycleThe water cycle is the name given to the
regular movement of water. Earth’s water is constantly moving, from the
oceans, to the air, to the land and back to the oceans.
Evaporation – changing of liquid water into vapor.
Condensation – when warm air cools, it cannot retain all of its water vapor, so the excess water vapor changes into liquid water.
Precipitation – rain, snow or sleet
Bodies of Salt WaterSalt water covers much of the earth’s
surface.
OceansAbout 97 percent of Earth’s water is ocean
waterThis water is salt waterToo salty for drinking, farmingDesalination – turning ocean water into
freshwater
Bodies of FreshwaterAlthough there is a small amount of
freshwater on Earth, it is necessary to sustain life.
Lakes, Streams and RiversOnly about 3 percent of Earth’s water is
freshwaterLakes, Streams and Rivers contain less
than 1 percent of Earth’s waterGroundwater – freshwater that lies beneath
the Earth’s surface, comes form rain and melted snow that filter through the soil and from water that seeps into the ground from lakes and rivers.
Aquifer – underground porous rock layer often saturated by very slow flows of water