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NAME - KCSE Online
NAME - KCSE Online

... (d) - It is expensive. - It is time consuming. - It is tiresome. - It is limited only to direct sources / primary sources. - It is only suitable to the sighted people. (any 3x1 = 3mks) 8. (a) (i) Weathering – is the breaking down and decomposition of solid rocks on the earth through physical and ch ...
Rock Cycle Questions and Short Story
Rock Cycle Questions and Short Story

... 8. Coal lies buried deep below the continental crust and is squeezed by great pressure from the rocks above and turns into diamond. 9. Water and wind weather and erode a mountain into little tiny pieces which are carried by rivers to a huge ocean. The pieces fall to the bottom of the ocean and are b ...
Constructive vs. Destructive project
Constructive vs. Destructive project

... before the forces, after the forces and in the future.(Making sure to use science vocabulary) Be sure to Explain in words why the changes occurred and the forces that were causing the changes. Model the Before, After and Future Earths formations due the forces. (Brochure, Model, Drawing, Diorama, et ...
SOL_5.7_Earth
SOL_5.7_Earth

... Earth is changed by weathering and erosion on the surface and by heat and pressure below the surface. Weathering is the breaking down of rocks and other materials into smaller particles. Air, water, and temperature changes cause rocks to break into smaller pieces resulting in physical change. Disso ...
The Rock Cycle - WordPress.com
The Rock Cycle - WordPress.com

... metamorphic rock slate by heat and pressure. Granite and Basalt They are both igneous rocks. Granite makes up most of the continental crust and basalt makes up oceanic crust. Obsidian and Pumice They are both igneous rocks formed by the quick cooling of lava. Obsidian is from lava that flowed and pu ...
Making Soil - How Does Soil Form?
Making Soil - How Does Soil Form?

... 1. Have learners identify the components of soil. 2. To represent mechanical weathering, the learners can crush rocks and sand with the hammer as parent material for the mineral portion of the soil. Keep the rocks and particles inside the cloth bag to prevent injuries from flying pieces. Explain the ...
When are soils most likely to erode?
When are soils most likely to erode?

... b. To keep the workers cool c. To help new plants grow when they are planted d. It looks better when it is wet. ...
When are soils most likely to erode?
When are soils most likely to erode?

... b. To keep the workers cool c. To help new plants grow when they are planted d. It looks better when it is wet. ...
Rocks, Minerals, and Soil
Rocks, Minerals, and Soil

... b. To keep the workers cool c. To help new plants grow when they are planted d. It looks better when it is wet. ...
The Rock Cycle
The Rock Cycle

... Evaporite is a name for a water-soluble mineral sediment that result from the evaporation from an aqueous solution and has been concentrated by evaporation. ...
Our Changing Earth
Our Changing Earth

... Landforms are always changing. They change when their rocks are broken. Weathering is the process that breaks rocks in Earth’s crust into smaller pieces. It is caused by water, ice, temperature changes, chemicals, and living things. Chemical weathering happens when chemicals cause rocks to change in ...
rocksmineralsjeopard[1] - fourthgradeteam2012-2013
rocksmineralsjeopard[1] - fourthgradeteam2012-2013

... Rocks are changed from one type into another by a never ending process called ...
Chapter 2 Minerals and Rocks
Chapter 2 Minerals and Rocks

... Crystal Structure and Solid  Have flat sides called faces ...
Sedimentary rock
Sedimentary rock

... •Cleavage is a mineral's tendency to break along smooth, flat surfaces. {Often causes a mineral to break into characteristic shapes}. ...
Chapter 7: Weathering & Soil
Chapter 7: Weathering & Soil

...  Changes the chemical composition of the rock  Naturally occurring acids, such as carbonic acid, react with calcite in limestone  The acid weathers away the limestone to form caves  Kaolinite clay is created when acids react with feldspar in granite  Clay is an end product in weathering ...
kirinyaga central district joint examination - 2013
kirinyaga central district joint examination - 2013

... Differentiate between rockslide and soil creep. - Rock slide involves movement of large masses of rocks soil creep involves movement of soil / fine materials. 2mks - Rock slide occurs on a very steep slope. Soil creep on a gentle slope.  2mks - Rock slide fast speed. Soil creep has a very slow s ...
Summary Sheets - The South Wolds Academy
Summary Sheets - The South Wolds Academy

... Porous? ...
Formation of Earth Materials
Formation of Earth Materials

... shaping landforms and weather. In grades 4-5 students learn how Earth materials change and how they can be used for various purposes. They learn that Earth materials include solid rocks and soil, water, and gases of the atmosphere. People use many of these materials as resources to meet their needs. ...
An ore is a rock rich in valuable minerals
An ore is a rock rich in valuable minerals

... removed from the Earth’s crust. Workers use machines to dig out the ore. ...
Weathering Subsystem..
Weathering Subsystem..

... The corestones get smaller and rounded as time goes by. (Credit: Chlaus Lotscher/Peter Arnold Inc.) ...
Weathering and Soils
Weathering and Soils

... Weathering particularly important for nutrient elements that have no gaseous form. ...
Geology Unit Review - Bennatti
Geology Unit Review - Bennatti

... How do you find lag time? What is the purpose of finding lag time? (How is this information used?) ...
geology review
geology review

... When water slows down it drops what it Is carrying. This is called B A ...
Date 7th Grade Science – Test Review 2.3 Vocabulary Review Word
Date 7th Grade Science – Test Review 2.3 Vocabulary Review Word

... support and link organisms together in a geographical region. 4. If the biodiversity of an ecosystem is greater, then the sustainability will be greater allowing that ecosystem to withstand environmental stress. 5. The biodiversity of an ecosystem depends on limiting factors,(both abiotic and biotic ...
Review Sheet for Exam 1
Review Sheet for Exam 1

... (i.e., atomic mass, atomic number, etc.)  What the four types of chemical bonds are  What silicate minerals are & what they are primarily composed of  The seven physical properties of minerals  Moh’s Hardness Scale  How minerals form Chapter 3 — Igneous Rocks  What the difference is b/w magma ...
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Weathering



Weathering is the breaking down of rocks, soil and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters. Weathering occurs in situ, roughly translated to: ""with no movement"" , and thus should not be confused with erosion, which involves the movement of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity and then being transported and deposited in other locations.Two important classifications of weathering processes exist – physical and chemical weathering; each sometimes involves a biological component. Mechanical or physical weathering involves the breakdown of rocks and soils through direct contact with atmospheric conditions, such as heat, water, ice and pressure. The second classification, chemical weathering, involves the direct effect of atmospheric chemicals or biologically produced chemicals also known as biological weathering in the breakdown of rocks, soils and minerals. While physical weathering is accentuated in very cold or very dry environments, chemical reactions are most intense where the climate is wet and hot. However, both types of weathering occur together, and each tends to accelerate the other. For example, physical abrasion (rubbing together) decreases the size of particles and therefore increases their surface area, making them more susceptible to rapid chemical reactions. The various agents act in concert to convert primary minerals (feldspars and micas) to secondary minerals (clays and carbonates) and release plant nutrient elements in soluble forms.The materials left over after the rock breaks down combined with organic material creates soil. The mineral content of the soil is determined by the parent material, thus a soil derived from a single rock type can often be deficient in one or more minerals for good fertility, while a soil weathered from a mix of rock types (as in glacial, aeolian or alluvial sediments) often makes more fertile soil. In addition, many of Earth's landforms and landscapes are the result of weathering processes combined with erosion and re-deposition.
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