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Fort Lisa's Loess Bluffs EarthCache

Hidden : 7/9/2009
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

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To log this EarthCache you will be required to take material samples from 2 locations on site.  Items needed are pre-labeled envelope or other small container for each sample, dull object to scrape samples (keys, coin etc.) magnifying glass, and a strong light source.

The History

N 41°22.408 W 095°57.228

In 1812 Manuel Lisa, president of the Missouri Fur Company, established near this spot a trading post to engage the local Indian tribes and fur trappers in commerce, supplying necessities and luxuries to both in trade for furs, cattle, horses and land, and served as a base from which Manuel Lisa acted as a subagent to neighboring tribes for the federal government. With his wide trading network, Manuel Lisa had a unique role in relation to American Indian tribes. He traveled extensively among them to share agricultural products and build relations, as well as to promote trade. According to one source, the influence of Manuel Lisa, exerted from Fort Lisa, was strong enough to hold all the Missouri River Indians firmly in alliance with the American people. Lisa supplied the Lewis and Clark expedition 8 years prior in their exploration of this region and himself became the first U.S. settler of Nebraska by establishing this post which he ran successfully until his death in 1820 when Joshua Pilcher succeeded Lisa as president of the fur company. Fort Lisa was closed in 1823 after Pilcher's Post was established downriver at what was to become Bellevue Nebraska.

The Geology

N 41° 22.020 W 095° 57.426

To the immediate west of this spot are bluffs comprised of windblown Loess. East of this spot lies a flood plain and beyond that the Missouri River.

Loess

A wind-deposited accumulation composed of silty material with an open structure and a relatively high cohesion. Loess is usually deep, fertile soil, rich in organic remains (especially the shells of snails) and characterized by slender, vertical tubes that are said to represent stems and roots of plants buried by sediment. When cut by streams or other agencies, loess remains standing in cliffs exhibiting a vertical, columnar structure; this is attributed to the vertical tubes and to the angularity of the grains and their tendency to interlock. The uncompacted character of Loess makes it subject to rapid erosion. Loess grains are angular, with little polishing or rounding, composed of crystals of quartz, feldspar, mica and other minerals. Because the grains are angular, loess will often stand in banks for many years without slumping. This soil has a characteristic called "vertical cleavage", which makes it easily excavated.

Flood Plains

Flood plains are created when the slope of the stream bed becomes slight and the decreasing velocity deposits sediments from higher regions. Under these conditions a stream will often begin to meander and widen the valley by eroding  the outside curve of the stream loops due to a higher velocity current and depositing on the inside curves where the velocity is lower. This tends to level out the stream valley. In times of flood, the rush of water down the whole valley both erodes, when the velocity is high, and deposits when receding, resulting in further planation (creation of flat terrain) of the stream's valley.

Missouri River

The Missouri Riverhas always carried, in suspension, an immense amount of solid matter, mostly very fine light sand, discoloring the water and justifying the name of "Big Muddy." The yearly average of solid matter carried into the Mississippiby this river is estimated at over 500 million tons. While the Missourihas a greater annual flow of water than the Mississippiabove its mouth, it is subject to greater fluctuations. These have affected its navigability in certain seasons and caused the shoreline to shift, some farms and villages to disappear, and others to be left far back through deposits of the soil in front of them. The Missouriis the longest river in the United States(2,466 miles). It drains a watershed of approximately 580,000 square miles as it winds around hills and bluffs, through one of the most fertile valleys in the world, to its junction with the Mississippi. Although it was thought for years that no keelboat could ascend the Missouri, it later became the great highway into the West.

Logging Tasks

N 41° 22.020 W 095° 57.426

To log this EarthCache you will be required to take material samples from 2 locations on site.  Items needed are pre-labeled envelope or other small container for each sample, dull object to scrape samples (keys, coin etc.) magnifying glass, and a strong light source.

Remove a minimal amount of Loess from the hillside exposure (1 tsp) at N 41 22.020 W 095 57.426 and place into container. Use caution in wet weather as the Loess soil underfoot is slick and unstable. Cross the road to the east beyond the walkway and brush away loose material to reach the soil and sample an equal amount. Recover sampled area with the loose material. Do not gouge or dig at either site, you will be taking surface samples only.

Compare the properties of each soil sample: Appearance, color, texture, reflective qualities, odor. Based on your observations, describe in an email to the cache owner, the properties of each sample and what you believe are their origins. These observations do not need to be done on site.

And

Give your opinion based upon the three features (bluffs, floodplain, and river) of this area why would Manuel Lisa choose this area for his trading post/fort?

There are no incorrect answers for this part, the question is asked to illustrate how each of these resources could contribute to the success of Manuel Lisa's business.

Optional

Upload a photo of yourself, an avatar, or your gps at the historical marker or the Loess exposure.

You will not need to wait for a response to log the cache online, however, logs not meeting all of the requirements within a reasonable time frame will be deleted.

 

 

 

References:     http://www.answers.com/topic/missouri-river

                                Wikipedia contributors, "Floodplain," Wikipedia, The Free Encyclopedia,         

                                  http://en.wikipedia.org/w/index.php?title=Floodplain&oldid=220387910 (accessed June 19, 2008).

                                 http://www.answers.com/topic/loess

                                  Wikipedia contributors, "Manuel Lisa," Wikipedia, The Free Encyclopedia,     

                                  http://en.wikipedia.org/w/index.php?title=Manuel_Lisa&oldid=294690049 (accessed June 6, 2009).

 






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