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EESC 111 Test 2
Sedimentary/Metamorphic Rocks
Question | Answer |
---|---|
Chemical weathering processes | Dissolution, oxidation, hydrolysis, carbonation, hydration |
Controls of weathering rates | Erosion, climate, parent material, vegetation, topography, time |
A combination of mineral and organic matter, water, and air | Soil |
Rock and mineral fragments produced by weathering | Regolith |
What makes a soil profile? | Horizons |
Horizons are | Vertical differences in soil |
What are the types of soil profiles? | O horizon, A horizon, E horizon, B horizon, C horizon |
O horizon is | Organic matter |
A horizon is | Organic and mineral matter |
Topsoil is made up of | O horizon and A horizon |
E horizon is | Little organic matter |
The E horizon is the zone of | Eluviation and leaching |
B horizon is | Zone of accumulation |
C horizon is | Partially altered parent material |
The "true soil" (solum) is made up of | O, A, E, and B horizons |
What are the 3 generic soil types? | Pedalfer, pedocal, and laterite |
Accumulation of iron oxides and Al-rich clays in the B horizon, best developed under forest vegetation | Pedalfer |
High accumulations of calcium carbonate, associated with dry grasslands and brush vegetation | Pedocal |
Hot and wet tropical climates, intense chemical weather | Laterite |
Sediments and sedimentary rocks cover approximately _ percent of the | 75 |
Sediments and sedimentary rocks compromise about _ percent (by volume) of Earth's outer 10 miles | 5 |
Sedimentary rocks show evidence of | Past environments |
Sedimentary rocks are an important resource of | Coal, oil, and other fossil fuels, groundwater resources |
Sedimentary rocks are products of | Mechanical and chemical weathering |
What are the 3 types of sedimentary rocks | Detrital, chemical, and organic |
Form from sediments that have been weathered and transported | Detrital |
Chief constituents of detrital rocks | Clay minerals, quartz, feldspars, and micas. |
_ is used to distinguish among the various types of detrital rocks | Particle size |
Clay-sized particles that form from the gradual settling of sediments in quiet, nonturbulent environments. It has fissility, crumbles easily and tends to form gentle slopes, and is the most abundant sedimentary rocks. | Shale |
Sand-sized particles that form in a variety of environments. It is the second-most abundant sedimentary rock, and quartz is the most abundant mineral. | Sandstone |
The particles in sandstone vary and are classified by | Their sorting and shape |
Transformed plant matter in ancient swamps | Coal |
Examples of coal | Estuaries, lagoons, low-lying coastal plains or delta environment |
How is coal classified? | Based on carbon content. calorific value on combustion, and sulfur content |
What is considered low sulfur content in coal? | <1% |
What is considered medium sulfur content in coal? | 1-3% |
What is considered high sulfur content in coal? | <3% |
When sediments are siliceous, the surface water temperature is | Cool |
When sediments are calcareous, the surface water temperature is | Warm |
Main locations siliceous sediments are found | Sea floor beneath cool surface water in high latitudes, upwelling areas, high latitude lakes |
Main locations calcareous sediments are found | Sea floor beneath warm surface water in low latitudes, coastal zones, tropical lakes |
Chemical sedimentary rocks form from _ material that was once in _ form. | Precipitated, solution |
Precipitation of material occurs by | Inorganic processes (such as evaporation) and organic processes from (water-dwelling organisms form biochemical sedimentary rocks) |
Types of hydrogenous sediments | Manganese nodules, phosphates, carbonates, metal sulfides, evaporite salts |
Cosmogenous sediment is composed of | Material derived from outer space |
Two main types of cosmogenous sediments are | Microscopic space dust and macroscopic meteor debris |