 Weathering is the breakdown and alteration of earth-forming materials by low pressure, temperature, water, air, and biological organisms.

Slides:



Advertisements
Similar presentations
The breakdown of rocks into smaller particles.
Advertisements

DENUDATION: Erosion and Weathering
 Rocks are continually recycled on the Earth’s surface and in Earth’s interior, on a geological time scale.  Rock is often exposed to an environment.
Weathering MechanicalandChemical. What Caused This?
Mechanical and Chemical. _ jpg
DENUDATION: Weathering and Erosion Introduction DENUDATION refers to the wearing down and stripping and leveling of the earths surface. DENUDATION refers.
Weathering Processes Formation of Soils By Diana L. Duckworth Rustburg High School Campbell County, VA.
Weathering, Erosion & Deposition
Topic 4: Weathering, Erosion and Deposition
The Process of Weathering Rocks. Weathering The breaking down of rock into smaller pieces that remain next to each other. Weathering forms sediments.
Weathering:  The natural process by which atmosphere and environmental forces, such as wind, rain, and temperature changes, disintegrate and decompose.
Weathering
The Art of Breaking things… Weathering and Soil. Weathering ► Weathering is the physical breakdown (disintegration) and chemical alteration (decomposition)
AP Environmental Science Trotter ROCKSMINERALS  Heterozygous  Can be organic or non- organic  Follow the rock cycle  Three types: sedimentary,
WEATHERING & EROSION.
Unit 1 Lesson 2 Weathering
The Process of Weathering Rocks
Weathering,Soil and Glacial Movement
Weathering. ing.
Weathering,Soil and Glacial Movement Ch. 14,15. What Physical Properties Affect Rocks Near the Surface? There are many processes that break rocks apart.
World Geography Unit 1: Physical Geography Land and Water Forms. Physical and Chemical Weathering.
Weathering and Soils Practice Test. QUESTION: What kind of weathering is represented by the following picture?
Weathering. What is Weathering? The physical, chemical, and biological processes that break down rocks and minerals, turning large particles into smaller.
Mechanical and Chemical. _ jpg
Weathering MechanicalandChemical. What Caused This?
Weathering Weathering is the physical breakdown and chemical alteration of rocks and minerals. Weathering happens on or near the surface. Weathering is.
JOURNAL #1 List two things you know about any of the following topics:
Weathering of Rocks. Why we see weathering 1.Most minerals are not stable at the Earth’s surface 2.The Earth wants to be flat – lowest energy state Topography.
Chapters 7 - Erosion & Weathering Lecture notes. Erosion- removal and transport of weathered materials.
Chapter Weathering and Soil. What is weathering? Weathering is process of breaking down and changing of rock at or near Earth’s surface. The two.
Weathering and Soil Formation
Learning Outcomes: 1.To be able to understand the terms Weathering and Erosion 2.To be able to understand and describe the different types of weathering.
What is Weathering?. Weathering The breaking down of rock into smaller pieces that remain next to each other. Weathering forms sediments. There are two.
Unit 1 Lesson 2 Weathering
Unit 1 Lesson 2 Weathering
Weathering, Erosion, and Deposition
Mechanical and Chemical
Find and photograph 6 examples
The Shape of the Earths Surface
The Process of Weathering Rocks
Weathering.
SOIL.
Weathering.
The Process of Weathering Rocks
Chapter 7 Section 1 Notes.
1. What are the two main types of weathering?
DENUDATION: Erosion and Weathering
Weathering and Erosion
Erosion and Weathering
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Mechanical and Chemical
Mechanical and Chemical
DENUDATION: Erosion and Weathering
1. What are the two main types of weathering?
Weathering and Erosion
Unit 1 Lesson 2 Weathering
Mechanical and Chemical
DENUDATION: Erosion and Weathering
Weathering.
Weathering and Erosion
Mechanical and Chemical
Weathering Unit 4: Lesson 2
Weathering.
Unit 1 Lesson 2 Weathering
Mechanical and Chemical
Mechanical and Chemical
Unit 1 Lesson 2 Weathering
Three Basic Definitions
Presentation transcript:

 Weathering is the breakdown and alteration of earth-forming materials by low pressure, temperature, water, air, and biological organisms.

 Weathering happens quicker on newly exposed rock because the minerals have not met their equilibrium state with their environment.

 Weathering surface are changed in color, texture, composition, firmness or form, with little or no transportation of the altered material

 Weathering is responsible for soil formation, nutrients used by marine organisms, fossil fuels and sedimentary ore deposits.

 Erosion is the transportation and removal of material produced by weathering.

 Erosion is caused by wind, water, currents, glaciers, humans, and animals.

 This type of weathering involves breaking down rocks into progressively smaller pieces.  It increases the surface area exposed to the elements to increase the rate of chemical weathering.

1. Pressure or Stress Release (Unloading) ◦ The removal of surface material by water, glacial erosion or human activities that could cause the minerals in the rock to spread further apart to create large voids.

2. Frost Action ◦ The changes in pressure caused by the cycle of freezing and thawing of water in colder climates in joints and crevasses may cause the rocks to fracture.

3. Salt Weathering ◦ The salt penetrates the rock’s surface and embeds itself in the pores and small cavities in the rock. ◦ The salt change size by either absorbing water or when the temperature changes.

4. Heating and Cooling (Exfoliation) ◦ Rock is also a poor conductor of heat so the surface may be hot, but the interior might be cold. This difference in temperature may can the rock to break apart.

 Minerals in a rock undergo changes that make them more stable under their current environmental and biological conditions.

1. Water ◦ Water serves as a medium for any chemical reaction to occur between a rock’s environment and it’s minerals. Flowing water prevents the chemical reaction to reach a state of equilibrium, thus allows it to continue indefinitely.

2. Chemical Reactions ◦ the reaction between the ions in the water and the minerals. This decomposes igneous rock. Hydrolysis Ion Exchange

Oxidation Carbonation

 The type of weathering that is the result of biochemical or biophysical processes associated with living matter.

 Worms increase a surface’s exposure to air and water.

 Bacteria break down chemicals and minerals and produce harmful by-products.

 Algae, lichen and fungus colonize rock surfaces reducing their contact with water and air and create ions that react chemically with the surface.

 P. 161 #1-4  P. 166 #1-4