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116 Cards in this Set
- Front
- Back
Drainage basin |
The fundamental unit for collection and distribution of water and sediment on the earths surface |
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Divide |
Each drainage basin is separated from adjacent basins by a |
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River valley |
A _______________ is a terrain in which a linear channel system is established. |
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Interfluves |
____________ are land along divides which separate adjoining valleys. |
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Stream order or stream rank |
Is assigned beginning with a rank of 1 (1st order) from streams that have no tributaries indicated with a blue line on a topographic map. |
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Rank or order |
Where two streams of the same rank meet, the next channel segment goes up one _________________. |
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Sinuosity |
Channel ____________ is the ratio between the length of the channel and the straight-line path length along the valley floor. |
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Meandering |
A _____________ channel has a sinuosity greater than 1.5. |
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Braided |
______________ river channels are favored by: erodible banks, abundant coarse sediment supply, and rapid changes in discharge. |
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Erodible banks, abundant coarse sediment supply, and rapid changes in discharge. |
Braided river channels are favored by: |
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Gradient |
River _________ is the vertical drop over a certain horizontal distance. |
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Decrease |
River gradient tends to ___________ down-valley so that most rivers have a concave upward profile. |
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Concave upward |
River gradient tends to decrease down-valley so that most rivers have a ___________________ profile. |
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Base level |
_______________ is the limit to which a river can downcut it’s channel, an imaginary surface extending beneath the continents from sea level. |
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Erosion |
_____________ occurs at cut banks on the outside of river bends. |
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Deposition |
____________ occurs at the inside on point bars. |
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Discharge |
River ___________ (Q) is the amount of water passing a given cross-section in a given amount of time. |
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Q = w*d*v |
Simplified discharge calculation: |
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Stage |
Flood _______ is the height to which the water rises above a stream gauge datum. |
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Stream gauge datum |
Flood stage is the height to which the water rises above a ____________________. |
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Depth |
Flood stage is usually somewhat different from the average ______ of flow used to calculate the discharge. |
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Velocity |
Flow _________ increases downstream as the gradient decreases from the headwaters to the river mouth. |
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Increases; Decreases |
Flow velocity _________ downstream as the gradient ____________ from the headwaters to the river mouth. |
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Velocity and discharge |
Both _________ and _____________ increase during a flood because more water is flowing into a smaller space. |
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Increase |
Both velocity and discharge ___________ during a flood because more water is flowing into a smaller space. |
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Hydrograph |
A ____________ plots changes through time in discharge, depth, stage, or some other hydrological variable. |
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Floods; snowmelt |
___________ can occur daily in areas of spring ______________, but usually come during particular seasons of the year or in a pattern determined by longer term atmospheric and climatic variation. |
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Flash floods |
_________________ occur in the upper part of a drainage basin from intense rainfall of short duration falling over a small area. |
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Flash floods |
_________________ occur in the upper part of a drainage basin from intense rainfall of short duration falling over a small area. |
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Drainage basin |
Flash floods occur in the upper part of a ________________ from intense rainfall of short duration falling over a small area. |
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Santa Elena Canyon of Big Bend NP Big Thompson Canyon in Colorado Front Range |
Examples of flash flood: |
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Downstream Floods |
__________________ cover a wide area when storms of long duration saturate the soil and produce increased runoff. |
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Asia |
Worldwide, the greatest number of floods and of people killed as well as the greatest economic loss occurs in _______ compared to Europe, Africa, or the America’s. |
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Indus River |
In July - August 2010, the _______________ flooded ~ 5,500 km2 including 20 percent of Pakistan. |
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Pakistan |
In July - August 2010 the Indus River flooded ~ 5,500 km2 including 20 percent of ___________. |
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Indus River flood |
Around 1800 deaths resulted as well as 100,000 dead cows |
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Indus River flood |
An intense summer monsoon also played a role. |
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Indus River flood |
Similar to the Mississippi River floods of 1993, the long levees which controlled floodwaters and channeled then to agricultural fields caused there to be multiple peaks in these floods. |
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Flood frequency |
_________________ is calculated as a “recurrence interval” (R.I.) from the series of peak annual floods. |
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10 year flood |
The _____________ is a flood for which R.I.= 10, and the probability is 1 in 10 (0.1) that a flood of that magnitude will occur in any given year. |
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Frequency |
Floods of a given ____________ can be mapped by zones with a particular flood probability, an approach widely used by planners and insurance companies. |
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Injury Loss of life Property damage Loss of soil and vegetation Pollution Disease Displacement |
Effects of floods |
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Floods |
_________ were the number 1 disaster in the United state’s during the past century. |
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Fertile food plains Cleaning of aquatic habitats New alluvial landforms |
Natural service functions of floods |
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Agriculture |
____________ caused erosion of southeastern piedmont between 1850 and 1930. |
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Topsoil and subsoil |
Gullies were filled with _________ and ________ eroded from farmland. |
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Channels |
____________ have been incisions down between 1930 and the present |
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Suburban |
_____________ development causes the greatest sediment yields, with up to 800 tons per square kilometer per year measured in the streams of the mid Atlantic by Wolman (1969). |
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“Impervious surface” |
Sharp spike in sediment yield because erosion ceases once the drainage basin is turned into an ____________ by paving. |
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Storm sewers |
In addition to impervious cover, _________________ result in more peaked hydrographs because they transfer runoff straight to channels. |
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Levees Dams Retention ponds |
Flood protection: |
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Effects of dams |
Upstream reaches afraid to new base level, downstream reaches incise and transport less sediment |
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Effects of dams |
Upstream reaches afraid to new base level, downstream reaches incise and transport less sediment |
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Channelization |
Intended to control flooding or erosion, drain wetlands, or improve navigation. |
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Larger; increased |
Channelization actually results in ___________ downstream discharge because of ____________ channel gradient. |
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Levees |
_________ spaced widely apart will preserve natural meandering channel while protecting land from flooding. |
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Channel Restoration of meandering streams |
Point bars and cutbacks, pool and riffle spacing, etc. |
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Gravity |
Mass wasting is downslope movement driven by _________. |
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Angle of repose |
The steepest angle that can be assumed by loose fragments on a slope without downslope movement. |
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Angle of repose |
The steepest angle that can be assumed by loose fragments on a slope without downslope movement. |
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Fall Slide Slump Earth flow Mudflow Debris flow Creep Solifluction |
Types of mass wasting: |
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Fall |
Fast and dry, the most rapid form of mass wasting |
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Flow |
Fast and wet (mass wasting) |
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Flow |
Fast and wet (mass wasting) |
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Slump |
Occurs on a curved path |
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Flow |
Fast and wet (mass wasting) |
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Slump |
Occurs on a curved path |
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Rotational; Translational |
Slump and some slides are ___________ as opposed to ______________ movements of rock and other earth materials. |
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Creep |
Gradual movement of soil and regolith downslope, aided by the expansion and contraction of the surface materials. |
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Solifluction |
Occurs in regions underlain by permafrost, where the “active layer” thaws in summer and flows gradually downslope. |
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Lahars |
Are mudflows which occur following volcanic eruptions where ash and water vapor fall out downwind of an eruption |
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Stability factor |
Slope stability can be summarized with a ________________ (F) calculated by dividing the resisting force by the driving force. |
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Failure |
A value less than 1 for F (stability factor) indicates that slope ________ is very likely. |
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Slope stability |
Climate, vegetation, water, time, type of earth materials, and slope or topography are all important factors affecting _________________. |
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Water |
Often acts as the immediate trigger, and the incident of mass wasting can usually be reduced by improving drainage from slopes. |
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Avid |
_______ climates have rock falls, debris flows, and shallow soil slips due to sparse vegetation, thin soils, and more exposure to bare rock. |
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Humid |
________ climates have deep and complex landslides, earth flows, and soil creep. |
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Vegetation |
____________ generally increases slops stability, although trees do add weight on the slope. |
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Soil compaction |
__________________ increases slope stability, and slopes with loosely compacted soils fail more rapidly. |
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Evaporation Condensation Sublimation Melting Freezing |
H2O molecules and changes of state: |
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Hydrologic cycle |
One of many cycles of moment of matter and energy on the earths surface. |
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Precipitation |
The movement of water which condensed out of clouds to the ground. |
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Evaporation |
The transfer of water to the atmosphere from surface reservoirs such as oceans, lakes, and rivers. |
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Transpiration |
The transfer of water to the atmosphere from the leaves and stems of plants |
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Infiltration |
The transfer of water into the subsurface through the soil. |
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Infiltration |
The transfer of water into the subsurface through the soil. |
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Runoff |
The transfer of water across the surface by overland flow and into rivers and streams. |
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Groundwater |
Most of earths freshwater is stored as |
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Saturated zone |
The water table is the top of the __________________. |
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Permeability |
____________ of soil or sediment is its ability to transmit water between the atmosphere above it and subsurface aquifer below it. |
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Confined aquifer |
A __________________ is one where groundwater is separated from the soil by an impermeable layer that hinders or prevents water movement. |
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Sodium (Na) and calcium (Ca) |
These elements can be completely dissolved. |
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Sodium (Na) and calcium (Ca) |
These elements can be completely dissolved. |
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Iron (Fe) and aluminum (Al) |
These elements are essentially insoluble. |
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Doline |
A _________ is a large sinkhole which results from the collapse of the roof of a subsurface cavern. |
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Uvala |
A ________ or dry valley forms when sinkholes or dolines intersect and capture all of the surface drainage. |
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Ponor |
A swallow hole or ______ which is associated with a disappearing stream. |
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Karst |
Dry steam beds often occur in _________ areas where surface flow disappears underground. |
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Speleothems |
_____________ are deposited in caverns when water leaves behind the compounds (principally Ca and CO3) it was carrying in solution. |
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Speleothems |
_____________ are deposited in caverns when water leaves behind the compounds (principally Ca and CO3) it was carrying in solution. |
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Stalactites |
____________ hang down from on top. |
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Speleothems |
_____________ are deposited in caverns when water leaves behind the compounds (principally Ca and CO3) it was carrying in solution. |
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Stalactites |
____________ hang down from on top. |
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Stalagmites |
____________ build up from the bottom. |
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Speleothems |
_____________ are deposited in caverns when water leaves behind the compounds (principally Ca and CO3) it was carrying in solution. |
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Stalactites |
____________ hang down from on top. |
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Stalagmites |
____________ build up from the bottom. |
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Pillars |
_________ form when stalactites and stalagmites unite. |
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Tower karst |
___________ occurs in the latest stage of karstificafion when most of the limestone has been dissolved leaving behind a few steep sided hills. |
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Sinkhole disaster |
Draining of Scott lake on June 13, 2006 |
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Sinkhole disasters |
Winter park, Florida on May 8-10, 1981 |
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Sinkhole disasters |
Seffner, Florida on February 28, 2013 |
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Sinkhole disasters |
Clermont, Florida on August 12, 2013 |
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Sinkhole disasters |
Macungie, Pennsylvania on June 23, 1986 |
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Sinkhole disasters |
Snake nation road in Valdosta in September 2011 |
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Sinkhole disasters |
Tifton, Georgia in August 2012 |