Soil part of the regolith that supports the growth of plants.

Slides:



Advertisements
Similar presentations
Weathering, Soil, and Mass Movements
Advertisements

5.2 Soil.
Earth’s Resources Chapter Fifteen: Soil and Fresh Water Resources 15.1 Soil 15.2 Water Resources.
DO Now: You find a sedimentary rock that has one graded bed. Describe how you know which layer of the graded bed is formed last?
Agenda: Notes Hand in Parent Quiz! Next class will be review! Homework: Read and take notes on 5.3 pg STUDY FOR TEST 3/1-3/2. Matter Review, Chap.
Processes that break down rock.  Rock is broken apart but not changed chemically.
Weathering and Soil. Types of Weathering Chemical Weathering: a rock being changed into 1 or more new compounds Oxidation- turns the rock into a rusty.
Section 3: Soil Preview Key Ideas Soil Soil Characteristics
Soils.
Weathering, Soil, and Mass Movement
An important product of Weathering.
Weathering, Soil, and Mass Movements
CHAPTER 5.2 Soil. CHARACTERISTICS OF SOIL Soil is what is made from weathering and covers most land surfaces. Soil is what is made from weathering and.
Earth’s Changing Surface
SOIL DEVELOPMENT AND EROSION. Soil Soil is a combination of mineral and organic mater, water, and air Soil is a combination of mineral and organic mater,
Weathering, Soil, and Mass Movements
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
5.2 Soil. Soil -Product of weathering -one of our most important resources *Regolith- layer of rock and mineral fragments that nearly everywhere covers.
Soils & Soil Formation-The Results of Weathering
Characteristics of Soil 5.2 Soil  Soil is part of the regolith that supports the growth of plants. Regolith is the layer of rock and mineral fragments.
Soil Section 5.2.
Soil. Regolith: Rock and mineral fragments that cover the Earth from weathering.
Weathering, Soil, and Mass Movements Chapter 5. Mechanical Weathering physical forces break rock into smaller and smaller pieces.
Weathering, Soil, and Erosion
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
The Ground Beneath Our Feet
Soil.
Soil: One of Our Natural Resources
Soil: One of Our Natural Resources
The Nature of Soil Essential Question:
Soil.
Ch. 5- Weathering and Erosion
The Nature of Soil Essential Question:
Chapter 12: Weathering & Erosion
Ch. 7 Sec. 3 Formation of Soil.
Soil Formation Soil is an important natural resource
Soils.
3.2 - Soils Discuss why soil is an important resource.
Soils.
Weathering and Erosion
Chapter 5 Weathering, Soil, and Mass Movements
Chapter 14: Weathering & Erosion.
Soil An interface in the Earth system, a boundary between different systems (biosphere, lithosphere, atmosphere). Soil is a combination of mineral matter,
The Ground Beneath Our Feet
Weathering and Soil Chapter 7.
SOIL - NOTES.
The Nature of Soil Essential Question:
Soil.
All About Soil.
Soil.
Read First Grab a folder and sit in a spot labeled FREE.
Soil Regolith – layer of rock and mineral fragments produced by weathering Soil – part of regolith that supports plant growth.
Weathering, Soil, and Mass Movements
Soil Brainpop Weathering Brainpop
SOIL.
Do First Actions: Get Ch.6 packet stamped
5.2: Soil regolith: layer of rock and mineral fragments created from weathering soil: part of regolith that can support plant life.
Soil Section 5.2.
Soil
Chapter Soils.
WEATHERING AND SOIL Weathering - breaking down of rocks Types
Soil.
Soil.
Chapter Soils.
Do First Actions: Get Ch.5-6 packet due Identify the below features:
Soil.
Weathering and Erosion
Soils.
SOIL.
Presentation transcript:

Soil part of the regolith that supports the growth of plants. Regolith: layer of rock and mineral fragments that covers Earth’s land surface. 1

How is Soil Formed? By rock being eroded away. 2

Characteristics of Soil Soil Composition Soil has four major components A. Mineral matter (broken-down rock) B. Humus (decayed remains of organisms) C. Water D. Air 3

Characteristics of Soil Texture refers to the proportions of different particle sizes. A. Sand (large size) B. Silt – feels like flour C. Clay (small size) D. Loam (a mixture of all three sizes) is best suited for plant life. 4

Characteristics of Soil 5

Time, Climate, Organisms and Slope The longer a soil has been forming, the thicker it becomes. Climate Greatest effect on soil formation Organisms Furnish organic matter to soil Slope Steep slopes often have poorly developed soils. 6

Soil Types Location Contents Pedalfer Pedocal Laterite under forest vegetation iron oxides and aluminum-rich clays in the B horizon Pedocal drier grasslands Calcium carbonate Laterite Hot, wet, tropical climates Intense chemical weathering to the top layers of soil 7