Slides:



Advertisements
Similar presentations
Weathering I. Definitions: the process by which rocks and minerals break down at or near the Earth’s surface Weathering: Produces soil, releases the minerals.
Advertisements

Erosion What are the agents of erosion? Erosion acts through weathering, the force of gravity, and through the movement of streams, groundwater, glaciers,
Weathering.
Geology 12 Presents Sedimentary Rocks Weathering and Erosion.
Aim: How does the shape of Earth’s surface change?
Weathering, Erosion & Deposition
5.1 Weathering.
Weathering, Erosion, and Deposition
Ch 5 – Weathering & Erosion
Weathering.
Weathering and Erosion Weathering means the process of breaking down rocks and other substances at Earth’s surface.
Weathering and erosion. What is Weathering? Weathering is the breaking down of rocks and other materials on the earth’s surface Weathering is the breaking.
Weathering.
LEARNING OBJECTIVES: Summarize the difference between mechanical and chemical weathering. Identify the factors that affect the rate of weathering.
12.1 Weathering Key Idea: Over time, the rocks are broken down by mechanical and chemical weathering.
Weathering must happen before erosion can take place!
Weathering and Erosion
Key Terms: weathering, mechanical weathering, chemical weathering, sediment, erosion, deposition, compaction, cementation.
UNIT SEVEN: Earth’s Water  Chapter 21 Water and Solutions  Chapter 22 Water Systems  Chapter 23 How Water Shapes the Land.
Weathering and soil formation – section 2-1 Rocks and Weathering
Weathering and Erosion. Weathering is the breaking down of rocks and other materials on the Earth’s surface.
Unit 2 Lesson 1 Weathering Copyright © Houghton Mifflin Harcourt Publishing Company 1.
Constructive and Destructive Forces
WEATHERING EROSION WEATHERING and the BREAKDOWN of ROCKS The process by which rocks and minerals break down at or near the surface of the Earth. The.
Weathering Topic 9 Regents Earth Science. Weathering  The break down of rock material as a result of chemical and/or physical action.
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.
Chapter 7- Weathering, Erosion and Soil
WEATHERING Big Rocks Into Small Rocks. 2 Types – Physical/Mechanical & Chemical   Physical/Mechanical Weathering – The physical breakdown of rocks into.
WEATHERING.
Chapters 7 - Erosion & Weathering Lecture notes. Erosion- removal and transport of weathered materials.
Gradational Processes
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 The natural breaking down of rocks and other materials on the Earth’s surface. A slow continuous process that affects all substances exposed.
Weathering and Erosion
Weathering How are the earth’s surfaces changed?.
Mechanical (Physical) Weathering What causes it? What happens? What do the effects look like? What causes it? What happens? What do the effects look like?
Mechanical Weathering MackenzieKevinMattSamMarissaVeronica.
Weathering & Erosion.
WEATHERING Breaking down of rock in Earth’s surface.
WEATHERING and SOIL Does The Earth’s Surface Change Slowly OR Quickly?
Weathering and Erosion
Weathering - the break down of rocks on the Earth’s surface.
Chemical and/or Physical breakdown of rock Physical Weathering (mechanical) breakdown of rock into smaller pieces –Does not involve a chemical change.
Weathering.  Earth’s surface is always changing. There are internal processes like mountain building and volcanic activity.  There are also external.
Weathering, Soils, & Erosion. #1 Weathering is the break up of rock due to exposure to processes that occur at the Earth’s surface. Weathering is the.
Weathering.
Lab: What effect does increased surface area on weathering?
Weathering and Erosion
Do Now: While watching the following clip answer the following:
Weathering, Erosion, and Soil
Weathering Notes.
Weathering and Erosion
Chapter Weathering, Erosion, and Soil
Ch 10: Weathering and Soil Formation.
Weathering, Erosion, and Soil
Weathering Notes.
Weathering and Erosion
Ch 5 – Weathering & Erosion
Weathering and Erosion
Weathering Notes.
Weathering Chemical and Physical & Erosion.
Weathering and Erosion
What causes Weathering?
Weathering. Weathering Weathering is the physical and chemical breaking down of rock material into smaller fragments due to exposure to processes that.
Ch 5 – Weathering & Erosion
Weathering and Erosion
Weathering and Erosion
Weathering Notes.
Weathering and Erosion
Presentation transcript:

What is a sinkhole? Sinkholes are depressions or holes in the land surface that occur throughout west central Florida. They can be shallow or deep, small or large, but all are a result of the dissolving of the underlying limestone.

earth_science/terc/content/visuali zations/es1103/es1103page01.cf m?chapter_no=visualization

Erosion Erosion is the process by which the surface of the Earth gets worn down. ence/terc/content/visualizations/es1205/es 1205page01.cfm?chapter_no=visualizatio nhttp:// ence/terc/content/visualizations/es1205/es 1205page01.cfm?chapter_no=visualizatio n

Weathering Mechanical and Chemical

Factors that influence weathering 1. Composition Some materials are harder than others (quartz) Some materials are more resistant to weathering (calcite) 2. Structure Fractured and fine grained rock weathers faster 3. Topography Severe temperatures expose fresh material 4. Climate Moisture and heat accelerates weathering

Why is weathering important? It produces sedimentary rocks and soil Mineral resources – ore deposits

MechanicalWeathering Mechanical Weathering

Mechanical Weathering Physical forces break rock into smaller and smaller pieces without changing mineral composition.

Six types of Mechanical weathering 1. Frost Wedging 2. Unloading or exfoliation 3. Thermal Expansion or exfoliation 4. Salt formation 5. Biological Activity 6. Abrasion

1. Frost Wedging Freezing and thawing of water in cracks Ice expands by 9% This occurs in mountainous regions and colder areas Talus: material produced by frost wedging at the base of a mountains forming a talus slope

/leveson/core/topics/weathering/processes /frost/frost_rollover.htmlhttp://academic.brooklyn.cuny.edu/geology /leveson/core/topics/weathering/processes /frost/frost_rollover.html

Talus slope from mechanical weathering

2. Unloading or exfoliation Pressure of overlying rock is removed by weathering Like the peeling of an onion This occurs because there is a reduction in pressure There is usually slab-like layers or loose sheets of rock Can be removed by erosion or ice sheets

3. Thermal Expansion Rock is a poor conductor of heat so the outside expands more than the inside This occurs in the desert – temperatures can vary by 30 degrees. This can causes exfoliation

Called: Exfoliation domes

4. Salt-crystal growth Salt crystal growth called haloclasty Water in rock openings is saline, the water evaporates and it leaves behind salt crystals which when heated expand and exert pressure on the rock. Causes granular disintigration This is common along the coast or the sides of the road in places where they salt the road

honeycomb weathering

5. Biological Activity Roots growing into the cracks and joints in rocks Earthworms and termites making tunnels People building roads, cultivating the land, exposing rocks to other types of weathering

6. Abrasion Abrasion refers to the breaking and grinding away of solid rock by collisions with moving particles. Abrasion takes place in many environments: fast-moving streams, beaches subject to storm waves, desert environments with high winds and beneath glaciers that are loaded with fragments of rock.

Just plain old gravity can be a factor of mechanical weathering like seen in these pictures…

howell/goodies/elearning/modul e07swf.swf

ence/terc/content/visualizations/es1201/es 1201page01.cfm?chapter_no=visualizatio nhttp:// ence/terc/content/visualizations/es1201/es 1201page01.cfm?chapter_no=visualizatio n