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Prepared by: Rana Faizan Saleem BS-Applied Geology Institute of Geology, Universty of The Punjab. Weathering. Is to explain you about: What is Weathering? Agents of Weathering Types of Weathering Types of Mechanical Weathering Types of Chemical Weathering
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Prepared by: RanaFaizanSaleem BS-Applied Geology Institute of Geology, Universty of The Punjab Weathering
Is to explain you about: • What is Weathering? • Agents of Weathering • Types of Weathering • Types of Mechanical Weathering • Types of Chemical Weathering • Factors that Effects rate of Weathering Aim of This Presentation
Weathering is the Physical and Chemical breakdown of pre-existing rocks into small particles , called sediments. Weathering
Water • Wind • Ice • Gravity Agents of Weathering
There are following types of Weathering: • Mechanical Weathering • Chemical Weathering Types of Weathering
The Physical breakdown of rocks into sediments, but their Chemical composition does not change. Mechanical Weathering
Frost Wedging • Salt Wedging • Exfoliation • Frost Heaving • Organic Activity • Abrasion Types of Mechanical Weathering
When water peels into the cracks of rocks, it freezes and causes the rock to crack. Frost Wedging
This occurs when rain water fills cracks in rocks; then water evaporate and with the passage of time salt crystals grow into cracks and expands,finally break the rocks. Salt Wedging
When a rock has heat exerted upon it, along with pressure, it separates into layers. It is also called Onion Skin Weathering because rock layers separate like onion layers. Exfoliation
Upward or Vertical movement of soil due to freezing of water in soil. Frost Heaving
Organic weathering is the breakdown of rocks by plants or animal action or by chemicals formed from plants and animals. Organic Activity
Abrasion occurs when rocks rub against each other and become rounded. Abrasion
The process by which rocks break down into sediments and their chemical composition will also changed. Chemical Weathering
Hydrolysis • Oxidation • Carbonation • Hydration • Reduction • Acid Rain • Plant Acid Types of Chemical Weathering
When rocks sit in water for extended periods of time they begin to break down and have a clay-like texture. 2KAlSi3O8+ 2H+ + H2O → Al2Si2O5(OH)4 +2K +4SiO2 (Orthoclase)(Kaolinite) Hydrolysis
When oxygen reacts with iron in rocks, they rust, and change the compositon. • 4FeO (Ferrous oxide) + O2 2Fe2O3 (Ferric oxide) • 4Fe3O4 (Magnetite) + O2 6Fe2O3 (Hematite) • 2Fe2O3 (Hematite) + 3H2O 2Fe2O3 .3H2O (Limonite) Oxidation
The carbon dioxide dissolved in water forms carbonic acid that reacts with many common minerals.e.g Limestone and Calcite. • CO2 + H2O H2CO3 carbonic acid • H2CO3 + CaCO3Ca++ + 2HCO3- (bicarbonate ions) Carbonation
The process of removal of oxygen and is the reverse of oxidation is called Reduction. i. 2Fe2O3 4FeO + O2 (Hematite) ( Ferrous oxide) Reduction
Chemical combination of water molecules with a particular substance or mineral leading to a change in structure. • Al2O3 + 3HOH Al2O3 .3H2O (Bauxite) (Hyd. aluminium Oxide) • CaSO4 + 2H2O CaSO4 .2H2O (Anhydrite)(Gypsum) Hydration
Water in the atmosphere absorbs sulfur oxides and nitrogen oxides and forms Sulfuric Acid and Nitric Acid which falls in the form of rain on earth called Acid Rain. • It changs the composition of minerals and rocks. Acid Rain
Plant Acid- When plants decay they release acids that react with the minerals in rocks. Plant Acid
Climate • Rock Composition • Surface Area Factors that affecting rate of Weathering
Weathering occurs fastest in hot, wet climates. It occurs very slowly in hot, dry climates. Without temperature changes, ice wedging cannot occur. In very cold, dry areas, there is little weathering. Climate
Some minerals resist weathering. Quartz is a mineral that weathers slowly. Rocks made up of minerals such as feldspar, calcite, and iron, weather more quickly. Rock Composition
The more surface area a rock has, the more quickly it will weather. • When a block is cut into smaller pieces, it has more surface area. So, therefore, the smaller pieces of a rock will weather faster than a large block of rock Surface Area