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Funk Lagoon - Rainwater Basin EarthCache

Hidden : 7/14/2008
Difficulty:
1 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This EarthCache is accessible to nearly anyone! The coordinates will take you to an informational sign. From there you will follow the paved pathway to the East to gather more information. A second coordinate location will provide a view of the lagoon. The terrain has been bumped to a 1.5 due to vegetation growing over the paved walkway occasionally.


The Funk Lagoon Waterfowl Production Area (WPA) is the largest marsh in the Rainwater Basin. The Rainwater Basin is a 4,200 square mile region of flat to gently rolling Peorial Loess Plains in South Central Nebraska that attracts millions of birds each year during migration. The basins were formed at the end of the last ice age when glacial winds carved out thousands of depressions in the landscape. A glacial wind is “a localized current of air occurring as a result of a glacier's melting processes; when the surface of glacial ice melts, the air above the glacier cools and becomes heavier than the surrounding air and flows downward.”

Once the glacial winds carved out the large shallow depressions, clay particles gradually formed a layer in the bottom of the depressions. This created natural ‘bowls’ in the landscape capable of holding snowmelt and rainwater throughout the year. Often, during hot summer months, evaporation occurs and the marshes dry out. This is a natural cycle and is important for plant growth which birds use to regain energy to continue their migration.

The soils that surround the basins are very fertile and consist of silt loams and silty clay. These soils are optimal for the cultivation of corn and beans as can be seen surrounding Funk Lagoon.

In early years of farming a long dry spell would dry out a marsh for several seasons. This prolonged dryness would entice farmers to plow into the dry marsh and plant crops. However, the disturbance of the soil could damage the clay layer and destroy the wetland permanently. On the other hand, a very wet year might cause a farmer to lose some of the field to flooding and this led to marshes being drained.

Biologists have estimated when the first settlers arrived in the region there may have been close to 4,000 wetland areas. Today, ninety percent of those wetlands are gone or have severe damage in the clay pan and can no longer hold water at the Earth’s surface.

Since 1963 the U.S. Fish & Wildlife Service, along with many other groups, has been working to restore the wetlands of the Rainwater Basin. Agricultural practices have improved and a better knowledge of the importance of the Rainwater Basin has led to the preservation of these areas.

Information provided by: U.S. Department of the Interior, US Fish & Wildlife Service, Rainwater Basin Joint Venture, Ducks Unlimited, Friends of the Rainwater Basin, National Snow & Ice Data Center.

To log the Earthcache begin at the posted coordinates. Here you will find a large sign with a soil cross section illustration.

1) What is the thickness of the clay pan layer beneath the basins?

Next, follow the concrete trail and read the signs to answer the following two questions:

2) How many Nebraska counties are contained by the Rainwater Basin?

3) How can managers control water levels at Funk and other Rainwater Basin wetlands?

Finally, hike or drive to N 40°29.834 W 099°13.113.

4) What year did Nels P. Peterson homesteaded this site.

E-mail us the answers (please do not post them with your log) and if possible, include a picture of yourself or group at the Funk Lagoon.

The photography blind is a great place to sit and watch birds and get some great shots!

Permission for placement of this EarthCache was granted by Gene Mack of the USFWS.

Additional Hints (Decrypt)

Ernq gur fvtaf pybfryl.

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)