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WEATHERING AND SEDIMENTARY ROCKS
WEATHERING AND SEDIMENTARY ROCKS

... mineral in sandstones is always quartz. Further subdivide sandstones based on other minerals present. Quartz sandstone is 99% quartz. Arkose contains both quartz and feldspar. Graywacke is a garbage sandstone with quartz, feldspar, mica and rock fragments. Often has a significant fine-grained compon ...
1. Origin of Soils and Rocks (Das, Chapter 2) - Icivil-Hu
1. Origin of Soils and Rocks (Das, Chapter 2) - Icivil-Hu

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Name #______ date ______ Chapter 2
Name #______ date ______ Chapter 2

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A. WEATHERING • Weathering is the BREAKUP OF ROCK mainly
A. WEATHERING • Weathering is the BREAKUP OF ROCK mainly

... Sedimentary rocks differ in their resistance to weathering depending on the CEMENTS holding their particles together. When these break up, their quartz fragments remain as boulders, pebbles, and sands. Quartzites, well-cemented sandstones and conglomerates (with silica cement) are among the longest ...
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Name Period ______ Date ______ Homework : Read chapter 7 and

... that the particles came from Organic materials, (Humus) waste products of ______________, ___________ and other living organisms broken down by decomposers such as ...
Weathering and Soil (p. 166-182)
Weathering and Soil (p. 166-182)

... The horizons are (from the top down): ____________________________. The O horizon is mostly decaying organic matter, called __________________. The A horizon is a mix of organic matter and minerals, like clay. The O and A horizons together are called _________________. The E horizon is not always pr ...
Word format
Word format

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Soils - sabresocials.com
Soils - sabresocials.com

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Rocks, Weathering and Erosion
Rocks, Weathering and Erosion

... Sedimentary Rocks are formed by the settling out of solid particles from air, water or glacial ice into layers called sediments The sediments are composed of rock particles, the remains of plants or animals or a combination of the two The sediments are cemented and compressed in a process called lit ...
Benchmark 3 Science Study Guide S6E5 A
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Chap. 8 Weathering & Soil Formation

...  Weathering is the process that breaks down rock & other substances at Earth’s surface.  Heat, cold, water, ice, oxygen, carbon dioxide, freezing, & thawing all contribute to weathering.  Erosion is the removal of rock particles by wind, water, ice, or gravity.  Weathering & erosion work togethe ...
External Forces Shaping the Earth
External Forces Shaping the Earth

... External forces, such as weathering and erosion, also alter landscapes and in some instances create the soil that is needed for plant life over many years or centuries. Weathering: refers to physical and chemical processes that change the characteristics of rock on or near the earth’s surface. Sedim ...
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3D ROCKS AND SOILS

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Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE

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... 55. A ___________________________________ is a ridge of sand underneath the water's surface that is built up by the action of waves and currents. 56. Trees and shrubs may eventually grown on a ___________________________________ or a long, narrow land formation that forms parallel to a coast. 57. A ...
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Rocks and Weathering
Rocks and Weathering

... __________________- the grinding away of rock by rock particles carried by water, ice, wind, or gravity ...
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Weathering

... The Fe2O3 produced by these reactions is relatively insoluble, and precipitates to form hematite, which is red in colour. This gives rise to the characteristic reddish or rust-like colours on the weathered surfaces of Fe-rich rocks (e.g. basalts). Note that oxidation of Fe in a silicate will take pl ...
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soil and weathering
soil and weathering

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Laterite



Laterite is a soil and rock type rich in iron and aluminium, and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and long-lasting weathering of the underlying parent rock. Tropical weathering (laterization) is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Cancer and Capricorn.Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to calls for the term to be abandoned altogether. At least a few researchers specializing in regolith development have considered that hopeless confusion has evolved around the name. There is no likelihood, however, that the name will ever be abandoned; for material that looks highly similar to the Indian laterite occurs abundantly worldwide, and it is reasonable to call such material laterite.Historically, laterite was cut into brick-like shapes and used in monument-building. After 1000 CE, construction at Angkor Wat and other southeast Asian sites changed to rectangular temple enclosures made of laterite, brick and stone. Since the mid-1970s, some trial sections of bituminous-surfaced, low-volume roads have used laterite in place of stone as a base course. Thick laterite layers are porous and slightly permeable, so the layers can function as aquifers in rural areas. Locally available laterites have been used in an acid solution, followed by precipitation to remove phosphorus and heavy metals at sewage-treatment facilities.Laterites are a source of aluminium ore; the ore exists largely in clay minerals and the hydroxides, gibbsite, boehmite, and diaspore, which resembles the composition of bauxite. In Northern Ireland they once provided a major source of iron and aluminium ores. Laterite ores also were the early major source of nickel.
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