Staar review earth and space systems
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STAAR REVIEW Earth and Space Systems. Changes in the Earth Over Time. Weathering- the process of rocks being broken down into smaller pieces. Mechanical Rocks break into smaller pieces by physical means – Water, ice, wind, gravity, organisms & changing temperatures. Chemical

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STAAR REVIEW Earth and Space Systems

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Staar review earth and space systems

STAAR REVIEWEarth and Space Systems


Changes in the earth over time

Changes in the Earth Over Time

Weathering- the process of rocks being broken down into smaller pieces.


Two types of weathering

Mechanical

Rocks break into smaller pieces by physical means –

Water, ice, wind, gravity, organisms & changing temperatures

Chemical

Rocks break into smaller pieces by chemical reactions – Air, water, acid & salts react with minerals in rocks to form new substances

Two Types of Weathering


Erosion

Erosion

Destructive

  • The movement of particles from one location to another is erosion

  • Weathered particles of rock are transported by gravity, living organisms, water, glaciers & wind.


Deposition

Constructive

Deposition

  • The settling (depositing) of eroded particles as sediments wherever they are transported by wind or water.


Rock cycle

Rock Cycle


Staar review earth and space systems

Sedimentary

Igneous

Metamorphic


Plate tectonics

Plate Tectonics

Plate tectonics explains the movement of large sections of Earth’s crust called tectonic plates. The force behind tectonic plate movement is thought to be currents of magma flowing in Earth’s mantle.


Plate boundaries

Plate Boundaries

Tectonic plates slowly collide against one another along plate boundaries. Sections of the plates may break off and be pushed down, up, or to the side. Mountain ranges, ocean trenches, earthquakes & volcanic activity are all common along plate boundaries.

Pacific Plate is the largest


Staar review earth and space systems

San Andreas fault


Staar review earth and space systems

All the land that drains into a specific body of water.

Groundwater and surface water both contribute to the water in a watershed.

Surface water becomes groundwater by soaking into the sand and soil or by traveling through cracks in rock.


Groundwater vs surface water

Groundwater vs Surface Water

  • Groundwater: water that fills the cracks and spaces in underground soil and rock layers such as aquifers. More freshwater is found here than on the surface.

  • Surface Water: water found on the surface such as rivers, lakes, oceans.

  • Watershed: the land area that supplies water to a river system

How do these to systems feed into each other?


Two important ways that oceans affect climate on land

  • Land heats up faster than water because land has a lower specific heat than water does. This causes the air over land to heat faster than the air over water. The warm air rises, starting a convection current that pulls air toward land from the ocean. This keeps air over the land from getting too hot and brings moist ocean air inland.

  • Warm air holds more water vapor than cold air does. When warm, moist air is cooled, clouds form and can produce precipitation. This warm air can be cooled by rising into the colder upper atmosphere, by moving over cold ocean or lakes, or by mixing with colder air. (Ex. Front boundary- the edge where cool, dry air meets warm, moist air. Often causes stormy weather)

Two Important Ways that Oceans Affect Climate on Land


Nitrogen cycle

Nitrogen Cycle

Nitrogen changes back & forth from nitrogen gas to the nitrogen compounds used by plants & animals.

Nitrogen is passed from plants to other organisms through food webs in the ecosystem. Once plants & animals use the nitrogen it returns to the atmosphere as a gas, completing the cycle.

Some fertilizers contain nitrogen compounds because plants need nitrogen to grow. Though there is plenty of nitrogen gas in the atmosphere, plants can’t use this form. In nature nitrogen can be changed from a gas to a form that plants can use by lightning or by soil bacteria and fungi in a process called nitrogen fixation.


Problems with too much nitrogen in the environment

Problems with too much Nitrogen in the Environment


Carbon cycle

Carbon Cycle


Effects of carbon on environment

Effects of Carbon on Environment

One of the biggest ways humans affect the carbon cycle is by burning fossil fuels.

Burning fossil fuels transforms carbon into carbon dioxide.

Higher levels of carbon dioxide cause the atmosphere to hold more heat energy. This may be the cause of warmer temperatures measured in recent years on Earth. (Called “The Greenhouse Effect”)

This could affect the climate in many places. The kinds of plants and animals in these climates may change if the warming continues.


Staar review earth and space systems

Without the carbon and nitrogen cycles, there would be no life on earth!


Catastrophic events affect the earth

Catastrophic Events Affect the Earth

Earthquakes

Floods

Meteorite crater

Volcanoes


Ways humans affect the earth

Ways Humans Affect the Earth

  • Two common forms of pollution:

  • Gases released into the atmosphere

  • Chemicals that are carried by water into a watershed


Humans can cause extinctions

Humans Can Cause Extinctions

  • Human can change:

  • The quality of the air, water & soil we use

  • Ecosystems by removing plants & animals & by introducing new species, such as invasive plants & pets

    • Invasive species don’t naturally live in the ecosystem where they are introduced.

    • Invasive species compete with/or drive out native species (species that live naturally in an ecosystem)

FIRE ANTS- invasive species- accidentally introduced to North America from South America. They have few predators in NA & aggressively attack & kill many kinds of native plants & animals. They have upset the balance of ecosystems in many southern states.


Renewable

Renewable


Non renewable

Non renewable

Fossil Fuels

Natural Gas

Oil

Coal


Inexhaustible

Inexhaustible


Eclipses

Eclipses


Solar eclipse

Solar eclipse

When the moon is aligned so that its shadow falls on Earth’s surface, the sun’s light is blocked from reaching part of the Earth. Called solar eclipse because it’s the sun that is being blocked from our view.


Lunar eclipse

Lunar Eclipse

A lunar eclipse occurs when Earth blocks sunlight from reaching the moon. This puts the moon in Earth’s shadow.


4 main phases of the moon

4 Main Phases of the Moon


Moon phase diagram

Moon Phase Diagram


Moon s revolution rotation

Moon’s Revolution & Rotation


Seasons

Have you ever noticed that the sun travels lower across the sky in winter than in summer? This is because Earth is tilted on its axis at a 23.5oangle.

Seasons

During winter part of Earth tilts away from the sun. This causes the sun’s rays to strike that part of Earth at a lower angle than in the summer.


Seasons remember it s the tilt of the earth that causes the seasons

Seasons- Remember it’s theTILT of the Earth that causes the seasons


Winter solstice shortest day of the year

Winter Solstice- shortest day of the year

Days are shorter & nights are longer during winter. This occurs in December in the Northern Hemisphere & in June in the Southern Hemisphere.

Each hemisphere receives less sunlight & therefore less heat energy during the winter. This is why temperatures are colder during winter.


Summer solstice longest day of the year

Summer Solstice- longest day of the year

This occurs in June in the Northern Hemisphere and in December in the Southern Hemisphere.

Earth’s revolution around the sun causes part of the Earth to tilt toward the sun at different times of the year. This causes that part of the Earth to receive more sunlight at a more direct angle. This is why days are longer and nights are shorter.


Equinox

Equinox

Equinox- means “Equal Night”

Daytime lasts exactly as long as nighttime on the first day of autumn – the Autumnal Equinox (about September 21) and the first day of spring - the Vernal Equinox (about March 21).


8 planets

8 Planets


The sun gravity

The Sun & Gravity


The sun is a star

The Sun is a Star

Our sun is a medium-size yellow star.

In the sun, hydrogen undergoes nuclear fusion, a process that releases vast amounts of energy. During fusion hydrogen atoms join to form helium atoms.

Hydrogen fusion is the source of light, heat, and other radiation from the sun.


Comets

Comets

Comets are made of various solids (like dirt & dust) and ice crystals. When their orbits take them close to the sun, dust and ice heat up to produce a “tail” behind the comet. Larger comets may even become visible without the aid of a telescope.


Asteroids

Asteroids

Asteroids are rocky and usually follow regular orbits around the sun.

Asteroid belt- the area between Mars and Jupiter that contains many asteroids orbiting the sun.


Nebulae

Nebulae

Nebulae are huge clouds of dust and gas. Some scientists think that our solar system was formed from nebula.


Staar review earth and space systems

Spiral

Galaxies are groups of millions or billions of stars.

The galaxy we live in is the Milky Way galaxy and has over 100 billion stars. It would take 100,000 light years to travel across it!

Irregular

Elliptical


Staar review earth and space systems

300,000,000 meters per second is the same as 300,000 kilometers per second.

That’s theSpeed of Light!


H r diagram

H-R Diagram

In the Hertzsprung-Russell diagram each star is represented by a dot. Stars are plotted by their luminosity (brightness) and surface temperature.


Hertzsprung russell diagram

Hertzsprung-Russell Diagram

http://www.dustbunny.com/afk/stars/lifecycle/hrdiagram.gif


Objects in the sky

Objects in the Sky


Objects in the sky1

Objects in the Sky


Objects in the sky2

Objects in the Sky


Objects in the sky3

Objects in the Sky


Objects in the sky4

Objects in the Sky


Phases of the moon

Phases of the Moon

  • New Moon

  • Waxing Crescent

  • First Quarter

  • Waxing Gibbous

  • Full Moon

  • Waning Gibbous

  • Third Quarter

  • Waning Crescent


Igneous rock

Igneous Rock

  • Formed when magma cools

    • Inside the Earth

      • Can be heated under pressure

        • Becomes metamorphic rock

      • Can be melted again to form new magma

    • Above the ground

      • Can be weathered and eroded

        • Becomes sedimentary rock


Sedimentary rock

Sedimentary Rock

  • Formed when sediments compact & cement into layers

    • Inside the Earth

      • Can be heated under pressure to form metamorphic rock

    • Above the ground

      • Can be weathered again to form more new sediment


Metamorphic rock

Metamorphic Rock

  • Formed when rock changes under heat & pressure

    • Inside the Earth

      • May melt to form magma

    • Above the ground

      • May weather & erode to form sediment


Staar review earth and space systems

http://www.cet.edu/ete/modules/msese/earthsysflr/rock.html


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