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Cape Girardeau Floods EarthCache

Hidden : 5/29/2014
Difficulty:
3 out of 5
Terrain:
1.5 out of 5

Size: Size:   other (other)

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Geocache Description:


The Mississippi River is the chief river of the largest drainage system in North America. Flowing entirely in the United States (though its drainage basin reaches into Canada), it rises in northern Minnesota and meanders slowly southwards for 2,340 miles to the Gulf of Mexico. With its many tributaries, the Mississippi's watershed drains all or parts of 31 US states and 2 Canadian provinces between the Rocky and Appalachian Mountains. The Mississippi ranks as the fourth longest and tenth largest river in the world. The river either borders or passes through the states of Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and Louisiana.

The Years 1844, 1908, 1927, 1943, 1973 and 1993 saw huge floods of major proportion in Cape Girardeau Missouri. The area saw roads, businesses, and homes that were flooded with widespread damage occurring that ran into the billions of dollars.

This earthcache will take you to a spot along the edge of the Mississippi River right next to the Downtown area. This is a very susceptible spot for flooding and is closely watched by local professionals. The listed coordinates will take you to the approximate "high water marks" for some of the flood years that have struck Cape Girardeau.

 


Erosion

Erosion is the process by which soil and rock are removed from the Earth's surface by natural processes such as wind or water flow, and then transported and deposited in other locations.
 

Types of Erosion:

Splash Erosion: Small soil particles are detached and sent airborne through the impact of raindrops on soil.

Sheet Erosion: Raindrops break apart the soil structure and it's moved down-slope by water that flows overland as a sheet rather than definitive channels. This occurs frequently during cloud bursts.

Rill Erosion: This process develops small, short-lived, concentrated flow paths. These paths create a sediment source and delivery system for hill-slope erosion. Areas where precipitation rates exceed soil infiltration rates are more prone to this type of erosion.

Gully Erosion: Water flows in narrow channels during or directly following heavy rains or melting snow. The gullies can erode to considerable depths.

Valley or Stream Erosion: Continual water flow alongside land (along a linear feature) creates this type of erosion. It extends downward, deepening a valley, and head-ward, extending the valley into the hillside. This occurs most frequently in times of flooding.

Bank Erosion: Over time, banks of rivers and streams are naturally worn down.

Freezing and thawing: Cold weather causes water trapped in tiny rock cracks to freeze and expand, breaking the rock into several pieces.

Wind erosion is a major geomorphological force, especially in arid and semi-arid regions. Wind erosion is of two primary varieties: deflation, where the wind picks up and carries away loose particles; and abrasion, where surfaces are worn down as they are struck by airborne particles carried by wind.

Mass movement is the downward and outward movement of rock and sediments on a sloped surface, mainly due to the force of gravity. Mass movement is an important part of the erosional process, and is often the first stage in the breakdown and transport of weathered materials in mountainous areas. It moves material from higher elevations to lower elevations where other eroding agents such as streams and glaciers can then pick up the material and move it to even lower elevations. Mass-movement processes are always occurring continuously on all slopes; some mass-movement processes act very slowly; others occur very suddenly, often with disastrous results.


**Logging requirements**
DO NOT POST ANSWERS IN YOUR LOG.
Send the following answers to me via email.

  1. The text "GC55WHA Cape Girardeau Floods" on the first line
  2. Standing next to the “high water” marks do you think you could stay standing there during the lowest “high water” mark year?
  3. What years would you have been under water completely?
  4. If the flood gates are open, walk down the river sidewalk, how many steps are there not covered by water?
  5. How high would the water need to rise before it covered your feet at the “high water” marks?
  6. At waypoint “year” What does the mural painted sign say, that is attached to the chain, that stretches across the mural’s painted arch? {No photos of this}
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