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Water shortages affect at least one-third of the world s population, with regional shortages being an issue Aquifers are large underground rock formations that store water in reservoirs Recharge zones allow water to enter aquifers Water withdrawal refers to the total amount of water taken, while consumption refers to water lost to direct use, evaporation, and ground seepage Runoff is made up of rainfall or snowmelt that has not had time to evaporate, transpire, or move into groundwater locations
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Global Water Resources and Use 81
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The geographical region from which a stream gets water is called a drainage basin or watershed Evaporation is water to vapor; condensation is the reverse, vapor to liquid (water) Nearly all (97%) of the Earth s total water is contained in its oceans Soil or rock is saturated when no water or other substance can fill the open spaces Aquifers that form a water table that separates the unsaturated and saturated zones are called unconfined aquifers since they flow right into the saturated zone Oscillating sprinkler systems lose a lot of water to evaporation and are not particularly efficient The Gulf Stream current is about 800 times the volume of the Amazon, the world s largest river Water table levels fall during times of low rainfall and high evapotranspiration Aquifer recharge zones, either at the surface or below ground, supply water to an aquifer and/or most of the watershed or drainage basin Porous media aquifers are made up of combined individual particles such as sand or gravel where groundwater is stored or moves between individual grains The boundary between two watersheds is called a divide Scientific concern about increasingly impacted oceans compelled more than 1,600 marine scientists to sign the 1998 Troubled Waters statement to raise public awareness
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CHAPTER
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IN THIS CHAPTER Summary: The Earth is made up of a core, mantle, and crust affected by volcanic, climatic, water, and weathering processes The rock cycle describes the creation, destruction, and metamorphosis of rocks and minerals Soil conservation maintains soil richness and crop vitality by protecting against erosion and desertification
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KEY IDEA
Sedimentary, igneous, metamorphic, rock cycle, stratigraphy, lithology, magma, tectonic, geothermal gradient, weathering, dissolution, hydrolysis, runoff, tillage, soil horizon, topography, desertification
Stratigraphic Classification
Unlike newly erupted volcanic rock, sedimentary rock strata or layers provide snapshots of regional climates and geological events throughout history By studying different rock layers, geologists find windows into climate conditions during specific time periods
Rock Stratigraphy
The study of rock, stratigraphy, is a grouping exercise Figure 81 shows a cross section of the ancient (pre-Cambrian) and more recent (Paleozoic) sedimentary rock layers in the United States Grand Canyon Layers can be thin, thick, rocky, or smooth, but all have a place in the geological stack and time The Grand Canyon is a good example of sedimentary rock layers above metamorphic and ancient rock
82
Soil and Soil Dynamics 83
GRAND CANYON Paleozoic sedimentary rock
Colorado river
Pre-cambrian sedimentary rock
Plutonic rock (granite) Metamorphic rock
The Grand Canyon is a colorful stratigraphic record of sedimentary rock
KEY IDEA
An individual band with its own specific characteristics and position is called a rock stratigraphic unit or rock unit Rock units stacked vertically add up to a formation, which geologists can describe and map as part of the geological record Formations are collections of many rock units grouped into a section with the same physical properties Formations can be seen in places where strata layers are exposed Igneous and metamorphic rock layers also have specific formations When studying sedimentary rock strata, it is important to remember huge stretches of time have led to layer upon layer of solidified rock Thousands and millions of years piled atom upon atom, crystal upon crystal, building each layer Lithology is the visual study of a rock s physical characteristics using a handheld magnifying glass or a low-power microscope Different rock formations can be matched by their physical characteristics such as Grain size and shape Grain orientation Mineral content Sedimentary structures Color Weathering The three main rock types are sedimentary, igneous, and metamorphic
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