Residual/Transported Soils, Erosion, and Erosion History.

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Residual/Transported Soils, Erosion, and Erosion

History

Parent Material Classified as either

residual or transported

Residual- soils that formed in their present location from the bedrock beneath

Bedrock- The sold rock beneath the soil

Example: Sandstone

Sandstone soils form from sandstone bedrock producing dry coarse soil. (mountain ridges)

Example: Limestone Limestone soils come

from limestone bedrock producing soil good for farming. (Lancaster)

Transported Soils Soils that have been moved from their original

location

Glacial Till Rocks and soils moved by glaciers

Aeolian Soil moved by wind

Colluvial Fallen rocks and soil along cliffs and

slopes

Alluvial Soil moved by water (flooded stream banks)

Please Answer these questions in your notebooks quietly as I come around to

check HW. What is a soil horizon? EXPLAIN how the soil horizons form, including any

processes that facilitate the process. What is weathering and what are some of the ways in which

rock weathers? How are forest soil horizons different from grassland soil

horizons (at least 2 ways) Why does this difference exist? Why is it so devastating to cut down rainforests? What is erosion and how is it different from weathering? What do you know about the history of erosion in the United

States?

Before the bell… Grab 2 articles Take out your Erosion Notes (you got them

Friday on back of Soil Horizon Questions) Answer these questions?

What are the 2 types of weathering? Give 3 examples of each What is erosion? What can cause erosion (list 3 things at least)

What is Erosion? The movement of

soil by wind or water to some new location.

Naturally a slow process but speeds up quickly when it is exposed.

Billions of tons of exposed topsoil are lost each year to erosion

Erosion History: Early SettlersHow do you believe farmers increased

erosion? Plows- The invention

of the plow greatly increased the amount of erosion by exposing large areas of farmland

Monocultures- Early colonists would grow one crop (monoculture) in the same place every year until the nutrients were used up and then they would move on leaving exposed soil behind.

Erosion History: Early Settlers

Colonists moved west to the great plains where the soil was rich in organic matter.

Why is this area so good for farming?

Erosion History: Early 1900’s Farmland

increased rapidly and by the 1930’s giant dust clouds of soil blew across the county due to dry exposed soil. (dust bowl)

Trailer Dust Bowl Movie

We Messed Up… Now What?

The government created the Soil Conservation Service (SCS) (now the NRCS) within the Dept. of Agriculture to conserve the nation’s soils.

The NRCS maps and surveys soil to plan methods of soil conservation.

http://soils.usda.gov/

Erosion History: Late 1900’s Modern technology

has allowed the U.S. to increase its production allowing it to produce more food than needed.

In the 70’s the U.S. started growing grains for other countries adding to the erosion problem (dust storms in CA.)

Erosion History: Today

Many conservation practices are still ignored when using large machinery because many practices are more difficult to do on a large scale.

Besides farming, highway construction, building construction, overgrazing and some logging activities all increase the rate of erosion

Types of Erosion: Rill Occurs on gentle slopes of exposed soil.

Water creates small channels a few inches deep. It may turn into gully erosion on steeper slopes.

Types of Erosion: Gully Occurs on steep slopes. Fast moving

water cuts deep ditches into the soil that can change the landscape.

Types of Erosion: Sheet Gradual removal

of topsoil by wind or water.

Occurs in thin layers on very gentle to non-sloping exposed soils.

It can be seen by blowing dust and muddy water.

Types of Erosion: Mass

Large movements of soil due to gravity.

Several Types: Landslide Mudslide Rockfall Creep

Landslide

Mudslide

Rockfall

Creep