Sedimentary Rocks

Sedimentary rocks are classified based on the origin of the sediments, divided into three groups: Detrital Rocks, formed by the compaction and cementation of fragments of other rocks, such as ballast, sand and clay; Chemiogenic Rocks, originated by the precipitation of substances dissolved in water, such as limestone and rock salt; and Biogenic Rocks, which have biological origin, accumulating remains of living beings or products of their activity, such as coal and conquiferous limestone. Each group represents a distinct training process.
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Explore more about Minerals can be identified through simple tests that evaluate characteristics such as color, brightness, trace, hardness, cleavage and reaction with acids. Color, although observable, is of little use in identification, as a mineral can have different colors. The shine can be metallic or non-metallic, depending on the light reflection. The trace refers to the color of the powder left by the mineral when it scratches a surface. Hardness, measured by the Mohs scale, indicates resistance to scratching, with harder minerals scratching softer ones. Cleavage, a mineral exhibits cleavage when it breaks, under the action of a force, along well-defined plane surfaces. Reaction with acids refers to the ability of some minerals to react with acids, producing effervescence. For example, calcite reacts with acid, releasing bubbles of carbon dioxide...

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Explore more about Mineral Wealth and Management Challenges
Known for its reddish color and high concentration of minerals, it plays a significant role in tropical and subtropical regions, especially in areas of intense agricultural and mining activity. Formed over thousands of years by weathering processes in hot and humid climates.
Features
Composition: Rich in iron and aluminum oxides, which gives it its characteristic reddish color. In some cases, it may contain valuable minerals such as bauxite.
Texture: Predominantly clayey, but with the presence of hard aggregates when exposed to air.
Porosity: Has low water retention capacity due to compaction.
Color: Shades that vary from red, brown and yellow, depending on the proportion of metallic oxides.
Properties:
High Resistance to Erosion: When compacted, it forms a hard crust on the surface, making surface erosion difficult.
Limited Fertility: Despite the presence of minerals, it is poor in organic matter and essential nutrients, requiring correction for agricultural use.
Moderate Permeability: Natural compaction can make water infiltration difficult.
Durability: Hardened laterite form, used in construction and as a paving material...

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Known for its reddish color and high concentration of minerals, it plays a significant role in tropical and subtropical regions, especially in areas of intense agricultural and mining activity. Formed over thousands of years by weathering processes in hot and humid climates.
Features
Composition: Rich in iron and aluminum oxides, ..know more

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