earth science, 13e
DESCRIPTION
Earth Science, 13e. Tarbuck & Lutgens. Running Water and Groundwater Earth Science, 13e Chapter 5. Stanley C. Hatfield Southwestern Illinois College. - PowerPoint PPT PresentationTRANSCRIPT
Earth Science, 13eTarbuck & Lutgens
Running Water and GroundwaterEarth Science, 13eChapter 5
Stanley C. Hatfield Southwestern Illinois College
Li River, China’s Guilin District Note karst topography, in which groundwater has dissolved large volumes of limestone (more later).
Earth as a system: the hydrologic cycle •Illustrates the circulation of Earth’s water
supply •Processes involved in the cycle
▫Precipitation▫Evaporation▫Infiltration▫Runoff▫Transpiration
The hydrologic cycle
Running water •Drainage basin
▫Land area that contributes water to a river system
▫A divide separates drainage basins
Drainage basins and divides
Drainage basins and divides exist for all streams, regardless of size.
River systems are divided into 3 zones.
Running water •Streamflow
▫Factors that determine velocity
Gradient, or slope Channel characteristics
Shape Size Roughness
Discharge – volume of water flowing in the stream (generally expresses as cubic feet per second)
Gradient (slope)•Parts of lower Mississippi: 10 cm/km•Mountain streams: 40 m/km•Steeper gradient has more energy,
more velocity
Discharge•Measured in m3 or ft3 per second•Changes over time due to amount of
precipitation in drainage basin
Measuring stream velocity1 kph – 30 kph
Straight – highest at center
Curved– highest at outer bank
Running water •Upstream-downstream changes
▫Profile Cross-sectional view of a stream From head (source) to mouth
Profile is a smooth curve Gradient decreases from the head to the mouth
Factors that increase downstream Velocity Discharge
Running water •Upstream-downstream changes
▫Profile Factors that increase downstream
Channel size Factors that decrease downstream
Gradient, or slope Channel roughness
Longitudinal profile of a stream
Stream Properties – Headwaters to Mouth
Running water •The work of streams
▫Erosion▫Transportation
Transported material is called the stream’s load Dissolved load Suspended load Bed load
Running water •The work of streams
▫Transportation Load is related to a stream’s
Competence – maximum particle size Capacity – maximum load Capacity is related to discharge
Running water •The work of streams
▫Transportation Deposition
Caused by a decrease in velocity Competence is reduced Sediment begins to drop out
Stream sediments Known as alluvium Well-sorted deposits
Running water •The work of streams
▫Transportation Features produced by deposition
Deltas – exist in ocean or lakes Natural levees – form parallel to the stream
channel Area behind the levees may contain back
swamps or yazoo tributaries
Formation of natural levees by repeated flooding
Running water •Base level
▫Lowest point a stream can erode to ▫Two general types
Ultimate – sea level Temporary, or local
▫Changing causes readjustment of the stream – deposition or erosion
Adjustment of base level to changing conditions
Running water •Stream valleys
▫Valley sides are shaped by Weathering Overland flow Mass wasting
▫Characteristics of narrow valleys V-shaped Downcutting toward base level
Running water •Stream valleys
▫Characteristics of narrow valleys Features often include
Rapids Waterfalls
▫Characteristics of wide valleys Stream is near base level
Downward erosion is less dominant Stream energy is directed from side to side
V-shaped valley of the Yellowstone River
Continued erosion and deposition widens the valley
Characteristics of a wide stream valley
Running water •Stream valleys
▫Characteristics of wide valleys Floodplain Features often include
Meanders Cutoffs Oxbow lakes
A meander loop on the Colorado River
Running water •Drainage patterns
▫Networks of streams that from distinctive patterns
▫Types of drainage patterns Dendritic Radial Rectangular Trellis
Drainage patterns
Running water •Floods and flood control
▫Floods are the most common geologic hazard
▫Causes of floods Weather Human interference with the stream system
Running water •Floods and flood control
▫Engineering efforts Artificial levees Flood-control dams Channelization
▫Nonstructural approach through sound floodplain management
Satellite view of the Missouri River flowing into the Mississippi River near St. Louis
Same satellite view during flooding in 1993
Water beneath the surface (groundwater) •Largest freshwater reservoir for humans •Geological roles
▫As an erosional agent, dissolving by groundwater produces Sinkholes Caverns
▫An equalizer of stream flow
Water beneath the surface (groundwater) •Distribution and movement of
groundwater ▫Distribution of groundwater
Belt of soil moisture Zone of aeration
Unsaturated zone Pore spaces in the material are filled mainly
with air
Water beneath the surface (groundwater) •Distribution and movement of
groundwater ▫Distribution of groundwater
Zone of saturation All pore spaces in the material are filled with
water Water within the pores is groundwater
Water table – the upper limit of the zone of saturation
Features associated with subsurface water
Water beneath the surface (groundwater) •Distribution and movement of
groundwater ▫Distribution of groundwater
Porosity Percentage of pore spaces Determines storage of groundwater
Permeability Ability to transmit water through connected
pore spaces Aquitard – an impermeable layer of material Aquifer – a permeable layer of material
Water beneath the surface (groundwater) •Features associated with groundwater
▫Springs Hot springs
Water is 6–9° C (10–15° F) warmer than the mean air temperature of the locality
Heated by cooling of igneous rock Geysers
Intermittent hot springs Water turns to steam and erupts
Old Faithful geyser in Yellowstone National Park
Water beneath the surface (groundwater) •Features associated with groundwater
▫Wells Pumping can cause a drawdown (lowering) of
the water table Pumping can form a cone of depression in the
water table▫Artesian wells
Water in the well rises higher than the initial groundwater level
Formation of a cone of depression in the water table
Artesian systems
Water beneath the surface (groundwater) •Environmental problems associated with
groundwater ▫Treating it as a nonrenewable resource ▫Land subsidence caused by its withdrawal ▫Contamination
Water beneath the surface (groundwater) •Geologic work of groundwater
▫Groundwater is often mildly acidic Contains weak carbonic acid Dissolves calcite in limestone
▫Caverns Formed by dissolving rock beneath Earth’s
surface Formed in the zone of saturation
Water beneath the surface (groundwater) •Geologic work of groundwater
▫Caverns Features found within caverns
Form in the zone of aeration Composed of dripstone Calcite deposited as dripping water evaporates Common features include stalactites (hanging
from the ceiling) and stalagmites (growing upward from the floor)
Cave features in Carlsbad Caverns National Park
Water beneath the surface (groundwater) •Geologic work of groundwater
▫Karst topography Formed by dissolving rock at, or near, Earth’s
surface Common features
Sinkholes – surface depressions Sinkholes form by dissolving bedrock and
cavern collapse Caves and caverns
Area lacks good surface drainage
Features of karst topography
End of Chapter 5