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The Great Flood EarthCache

This cache has been archived.

Geocaching HQ Admin: It has now been over 30 days since Geocaching HQ submitted the disabled log below and, unfortunately, the cache owner has not posted an Owner maintenance log and re-enabled this geocache. As a result, we are now archiving this cache page.

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Hidden : 3/3/2011
Difficulty:
2.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

During the last ice age, glaciers repeatedly blocked the Clark Fork River Valley just up stream from Pend Orielle Lake. An ice dam was created (Glacial Lake Missoula). This ice dam periodically collapsed and then reformed. Each collapse released a huge wall of water, mud and boulders that rushed through Lake Pend Orielle, down the Rathdrum Prairie and out into Eastern Washington, eventually reaching the Pacific Ocean.


It is very difficult to imagine these floods. At the flood’s maximum, more than 9 cubic miles of water roared past a given point in the valley every hour. “The flow was equivalent to 10 times the combined flow of all the rivers in the world today, or 1,000 times the flow of today’s Columbia River”, which drains the Columbia basin.

As the depth of the water in Lake Missoula increased, the pressure at the bottom increased enough to lower the freezing point of water below the temperature of the ice forming the dam. This allowed water to seep into minuscule cracks present in the ice dam. Over a period of time, the friction from water flowing through these cracks generated enough heat to melt the ice walls and enlarge the cracks. This allowed more water to flow through the cracks, generating more heat, allowing even more water to flow through the cracks. This feedback cycle eventually weakened the ice dam so much that it could no longer support the pressure of the water behind it, and it failed catastrophically.

The flood waters carried a huge load of gravel, cobbles and boulders as it rushed through the Spokane Valley, which has been known to cause the Spokane Floods and the channeled scablands of Eastern Washington. Once the water started to subside the gravel, cobbles, and boulders were left in the valley. The finer minerals like sand and silt washed far down stream, leaving a relatively clean layer rocks behind. If you look around this site you will see some of the large boulders moved by these floods.

Covered by a thin soil layer, this very coarse, highly permeable rock layer is now filled with water. Today, this underground water source, the Spokane Valley-Rathdrum Prairie Aquifer, is a protected "Sole Source Aquifer", the only source of drinking water.

Geologists estimate that the cycle of flooding and reformation of the lake lasted an average of 55 years and that the floods occurred several times over the 2,000-year period between 15,000 and 13,000 years ago. Alternate estimates for the peak flow rate of the largest flood include 17 cubic kilometers per hour and range up to 60 cubic kilometers per hour. The maximum flow speed approached 36 meters/second (130 km/h or 80 mph).

Resources: Signage at the posted coordinates. Suburban Emergency Management Project (http://www.semp.us/publications/biot_reader.php?BiotID=429). Wikipedia-Missoula Floods (http://en.wikipedia.org/wiki/Missoula_Floods)

To claim this Earthcache you will have to answer the following questions and complete two assignments. Please email me (AmplePeach@gmail.com) the answers. Please do not post answers in your log, If answers are posted, your log could be deleted without warning. Sorry, but this is to make the find fair for all.

1. Visit the above coordinates to start your lesson.

2. Look around you (River Bank) and explain why you think these "Pebbles" and "Boulders" did not make it farther down the river.

3. Estimate the distance across the river.

4. Please post the time you started this Earthcache along with the weather conditions.

You must now complete the following assignments, both are required!

Assignment #1 Determine the flow rate of the river at the time of your visit. This may be done by measuring & marking a distance along the river bank, then tossing in a stick upriver from your starting point. With a stop watch, time how long it takes your stick to complete your measured distance course. Then calculate that into "Feet Per Second" for the river (Distance divided by Time). Once you have your answer please (Click Here) to determine an approximation on how fast the river is going in Miles Per Hour (MPH). Provide your answer in your email.

Assignment #2. Visit the Geological Feature (N 47.40.715, W 117.12.544). Your task is to determine the volume (Cubic Feet) of this feature. You can do this by multiplying the length x width x height. Explain how you think this feature got to its current location. Provide your answers in your email.

Remember while reading above it was estimated the maximum flow rate was 80mph when the flood came through here. After completing this assignment you will have an idea of the difference between today and then.

Although not a requirement a photo of yourself near the site would be appreciated. :)

Please note that I will not be responsible for personal injury or damage to your equipment. Please be careful when you are near the river. Thank you!

Additional Hints (Decrypt)

[All you have to do is try. This is not difficult and you should learn a lot about this area. Thanks for stopping by!]

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)