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statue Grand Canyon Sand Pile What do These 3 Things Have in Common??

Weathering

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Page 1: Weathering

statue Grand Canyon

Sand Pile

What do These 3 Things Have in

Common??

Page 2: Weathering

They have all been

subjected to the process of

WEATHERING

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Page 4: Weathering

WEATHERING: is

THE CHEMICAL AND PHYSICAL PROCESS THAT CHANGES ROCK

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For weathering to occur the rocks must be

exposed to:

WATER (hydrosphere) AIR (atmosphere)

ACTION OF HUMANS & OTHER LIVING ORGANISMS

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Evidence of Weathering:

the end product of the weathering of rock is

SEDIMENT

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Sediment Name Diameter range(cm) Boulder Cobble

Pebble Sand Silt (colloid-suspended) Clay (colloid-suspended)

Sediments are classified by size: use the reference tables

page 6 to complete the chart

Dissolved particles (ions) Not visible

25.6 or larger 6.4-25.5

0.2-6.3 0.006-0.1 0.0004-0.005

Less than 0.0004

Examples:salt,calcite

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PHYSICAL WEATHERING:

ROCKS ARE BROKEN INTO SMALLER PIECES WITHOUT CHANGING THE CHEMICAL NATURE OF THE ROCK

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Explain how water and wind can can cause

physical weathering

in the following ways:

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The alternate freezing and thawing of

water

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WATER EXPANDS WHEN IT FREEZES

This is called…….

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Ice Wedging or Frost Action

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a weathered sidewalk

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Half Dome in Yosemite California

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*ABRASION

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RUNNING WATER AND

WIND CAN RUB OR WEAR DOWN ROCKS

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RUNNING WATER AND WIND CAN CAUSE ROCKS TO RUB AGAINST EACH OTHER AND WEAR THEM DOWN

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* BIOLOGIC ACTIVITY

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My sidewalk being lifted by the tree roots!!

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PLANT ROOTS EXPOSES NEW SURFACES TO WEATHERING

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*Humans can influence the rate of weathering by the use of powerful

equipment

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If you increase the surface area you will ___________ the

rate of weathering increase

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Surface area

rate of

weathering

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CHEMICAL WEATHERING:

Rocks are broken and the chemical composition is also ___________ CHANGED

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• OXIDATION OCCURS WHEN __________ FROM AIR COMBINES WITH ___________ TO FORM OXIDES

OXYGEN

MINERALS

RUST

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This was washed up on a beach!!

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A rusty gate……

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• CARBONATION

OCCURS WHEN __________ CONTAINING

__________ ACID

DISSOLVES MINERALS

WATER

CARBONIC

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EX.

LIMESTONE CAVES

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* POLLUTANTS can speed up the rate of

chemical weathering OXIDES OF SULFER AND NITROGEN MAKE RAINWATER UNNATURALLY ACIDIC

ACID RAIN

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• HYDRATION OCCURS WHEN _______ SUCH AS MICA AND FELDSPAR ABSORB ________ AND WEAKEN AND FORM ________

MINERALS

WATER CLAY

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If: temperature = 5 precipitation = 100

Moderate physical and

chemical weathering

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temperature = 20 precipitation = 100

Faster rate of chemical weathering

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If: temperature = -10 precipitation = 50

Faster physical

weathering

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CLIMATIC EFFECTS ON WEATHERING:

PHYSICAL WEATHERING DOMINATES IN

COLD, MOIST

CLIMATES

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CLIMATIC EFFECTS ON WEATHERING:

CHEMICAL WEATHERING DOMINATES IN

WARM, MOIST

CLIMATES

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IN GENERAL WHEN THERE IS MORE

THERE IS MORE WEATHERING

MOISTURE

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CLEOPATRA’S NEEDLE Central

Park

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RATE OF WEATHERING ALSO

DEPENDS ON:

MINERAL COMPOSITION ROCK RESISTANCE

(HARDNESS)

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SHALE SANDSTONE

SHALE SANDSTONE LIMESTONE

SHALE DOLOSTONE WHICH ROCK

IS THE MOST

RESISTANT TO

WEATHERING?

WATER

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SHALE SANDSTONE

SHALE SANDSTONE LIMESTONE

SHALE DOLOSTONE WHICH ROCK

IS THE MOST

RESISTANT TO

WEATHERING?

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SHALE SANDSTONE

SHALE SANDSTONE LIMESTONE

SHALE WHICH ROCK

IS THE LEAST

RESISTANT TO

WEATHERING?

DOLOSTONE

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SHALE SANDSTONE

SHALE SANDSTONE LIMESTONE

SHALE WHICH ROCK

IS THE LEAST

RESISTANT TO

WEATHERING?

DOLOSTONE

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SOIL FORMATION: SOIL IS THE

COMBINATION OF:

ROCK PARTICLES MINERALS ORGANIC MATTER

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THE END RESULT OF

WEATHERING AND BIOLOGIC ACTIVITY IS:

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Adding to a compost pile

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SOIL FORMATION:

Breakdown of rock

Addition of organic material ( from decomposition )

(biological activity)

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A B

C

Soil Horizons

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SOIL HORIZONS (LAYERS) A (TOP SOIL) rich in organic material B little organic material

rich in minerals leeched from horizon A

C partly weathered broken up bedrock sits on top of solid bedrock

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The two types of sediment (soil) are:

Transported Residual

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TRANSPORTED SOILS:

CARRIED FROM LOCATION OF PARENT ROCK

MOST OF NEW YORK SOIL IS TRANSPORTED

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3 WAYS THAT SOIL CAN DIFFER IN VARIOUS

LOCATIONS:

SOIL ASSOCIATIONS (CHARACTERISTICS

1. 2. 3.

COMPOSITION

MOISTURE ORGANIC MATERIAL

(MINERALS)

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HOW CAN WE IMPROVE THE SOIL’S ABILITY TO SUSTAIN LIFE?

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Terrace planting

Page 66: Weathering

Wind breaks like trees Planted

To Stop

Wind erosion