WEATHERING AND SOIL FORMATION Flashcards

(36 cards)

1
Q

Serves as building blocks of rocks

A

Minerals

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2
Q

A naturally occurring inorganic substance with more or less definite chemical composition and specific physical properties

A

Minerals

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3
Q

study of minerals and their properties.

A

Mineralogy

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4
Q

Persist in the soil in their original state due to high resistance to decomposition. They are chief sources of sand and silt fractions of soils

A

Primary Minerals

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5
Q

Arise from the chemical breakdown of the least resistant primary minerals. Contributes the clay fraction to the soil.

A

Secondary Minerals

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6
Q

a predominantly parent material of this substance is expected to give rise to sandy soils; does not contribute to soil fertility because of its main composition of SiO2.

A

Quartz

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7
Q

contributes Potassium (K) upon weathering

A

Orthoclase

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8
Q

Contributes Sodium (Na) upon weathering

A

Sodium-plagioclase

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9
Q

Contributes Calcium (Ca) upon weathering

A

Calcium-plagioclase

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10
Q

It is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as component of limestone

A

Calcite

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11
Q

an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally CaMg(CO3)2.

A

Dolomite

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12
Q

isa soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula CaSO4·2H2O. It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywall.

A

Gypsum

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13
Q

a sedimentary rock composed principally of calcite or the double carbonate of calcium and magnesium (dolomite). It is commonly composed of tiny fossils, shell fragments and other fossilized debris.

A

Limestone

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14
Q

isan iron ore consisting of a mixture of hydrated iron(III) oxide-hydroxides in varying composition.

A

Limonite

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15
Q

heavy and relatively hard oxide mineral, ferric oxide (Fe2O3), that constitutes the most important iron ore because of its high iron content (70%) and its abundance.

A

Hematite

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16
Q

is one of the mineral forms of aluminium hydroxide.

17
Q

isa layered silicate clay mineral which forms from the chemical weathering of feldspar or other aluminum silicate minerals.(1:1 non expanding clay)

18
Q

ahydrousphyllosilicatemineralwhich undergoes significant expansion when heated. (2:1 limited expanding clays)

19
Q

Illite type clays are formed from weathering of K and Al rich rocks under high pH conditions.(2:1 non expanding clay)

20
Q

is the main constituent of bentonite, derived by weathering of volcanic ash. (2:1 expanding clay)

A

Montmorillonite

21
Q

study of rocks

22
Q

A natural substance composed of solid crystals of different minerals that have been fused together. Aggregates of minerals

23
Q

Original rocks formed from the solidification of magma at temperature 900oC to 1600oC within or outside the earth’s crust.

A

IGNEOUS ROCKS

24
Q

2 Modes of Rock Formation

A

Extrusive and Intrusive Formation

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# Mode of Rock Formation * Magma is ejected out of the earth’s crust through volcanic eruption and solidifies on the surface. * Abrupt cooling of magma and less time for crystal growth. * The rock formed is fine-grained
Extrusive Formation
26
# Mode of Rock Formation * Magma solidifies within the earth’s surface. * Slow cooling of magma due to high temperature and more time for crystal growth. * The rock formed is coarse-grained
Intrusive Formation
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Formed from other existing rocks through process of remelting and recrystalization under very high temperature and pressure.
METAMORPHIC ROCKS
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Formed from other existing rocks through fragmentation, transport and recementation.
SEDIMENTARY ROCKS
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Examples of Igneous Rocks
* Granite * Diorite * Gabbro * Basalt * Obsidian
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Examples of Metamorphic Rock
* Gneiss * Schist * Quartzite * Slate * Marble
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Examples of Sedimentary Rocks
* Limestone * Dolomite * Sandstone * Shale
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It is the breaking down or deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gases, and biological organisms.
Weathering
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# Types of Weathering Breaking up of rocks and minerals into smaller pieces without any drastic alteration of their chemical composition
Physical Weathering
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# Types of Weathering Change in the chemical structure and composition of rocks and minerals which results into simpler products.
CHEMICAL WEATHERING
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Factors of Soil Formation
1. Climate 2. Living Organism 3. Relief or Topographt 4. Parent Material 5. Time
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