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Spring Valley Lake EarthCache

Hidden : 7/28/2008
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Welcome to the Spring Valley Wildlife Area. This wetland area is full of wildlife and plant activity especially during the Spring and Summer.


Geology and History of the area

The topography of the Little Miami River Basin, including Caesar Creek, is characterized by rocky gorges and narrow valleys separated by extensive sections of bottomlands. The nature of soil types and vegetation relate to events that occurred thousands or even millions of years ago. Alterations of the drainage system and the formation of many of the scenic features of the valley can be traced to the Kansan, Illinoian and Wisconsin periods of glaciation.
The foundation of the area consists of layers of flat, sedimentary bedrock formed from the effects of these glaciers. Below the present-day soil surface lies a solid bedrock that can range from being only a few inches below the surface to over 400 feet below the surface. The last of these glaciers that affected southwestern Ohio was the Wisconsin glacier. The Wisconsin glacier left the area much as it was found by early settlers.
Around 14,000 years ago the last of the Wisconsin Glacier ice left Ohio and the current landscape and climate developed.

What Is a Wetland?

Although wetlands are often wet, a wetland might not be wet year-round. In fact, some of the most important wetlands are only seasonally wet. Wetlands are the link between the land and the water.

Generally speaking there are four categories of wetlands: marshes, swamps, bogs and fens.

A marsh is a wetland frequently or continually filled with water. Marshes can be found on the coast and inland, and can be either freshwater or saltwater. Characterized by grassy, soft vegetation that grows in the soggy soil conditions, marshes can be one of two types -- tidal or non-tidal. Found along coastlines, tidal marshes are most prevalent on the eastern coast of the United States and in the Gulf of Mexico. Non-tidal marshes are the most common type of wetlands in North America and occur along the boundaries of streams, rivers, ponds and lakes. Water is generally only a few inches or feet deep with soil that's extremely mineral-rich and organic. Non-tidal marshes host vegetation like lily pads, cattails, and reeds as well as a varied sample of animal life, including muskrats, otters, blue herons and blackbirds.

A swamp is any wetland dominated by woody plants and several feet of water. The Everglades in Florida is one example of a swamp. As with most wetlands, swamps function as flood protection and nutrient removal. The saturated ground and standing water form a black,­ thick and nutritious soil, providing a favorable environment for water-tolerant shrubs and trees. Fittingly, then, there are two types of swamps -- shrub swamps and forested swamps­. The difference between the two swamps simply is the type of vegetation present. You will often find shr­ub swamps and forest swamps adjacent to each other. Shrub swamps are swamps filled with lower, bushy vegetation such as willow, dogwood, swamp rose and mangroves. Forested swamps host trees like red maple, pin oak, tupelo, cypress and willows. They play a vital role in the survival of wetland-dependent animals, like ducks, snakes and otters.

Bogs receive most of their water from precipitation, rather than runoff or floodwaters. Their spongy, mossy floors contain fewer nutrients than a marsh or swamp. As the moss decomposes, it forms acidic peat. Acidic peat will burn for a very long time, and people harvest it for fuel. This peat is also very low in nutrients, and only specially adapted creatures may call a bog home, like salamanders, dragonflies, snakes and carnivorous plants. Found mostly in the northeast U.S. and Great Lakes regions, bogs are also an excellent area to grow cranberries.

A fen is similar to a bog, except that a fen receives its water from the ground­ rather than from precipitation. The water that feeds a fen is actually water from melted glaciers. As the glacier melts, it deposits sand and gravel into the soil, preventing its runoff from permeating into the soil. Instead, it flows sideways and picks up minerals and sediment as it travels. This means a fen's ­water is much more rich and nutritious than a bog. Therefore, fens host a diverse community of plants and animals. Wildflowers, deer, turtles, butterflies and even fish may find a home in a fen. Fens are rare, found primarily in the northern hemisphere in areas with low temperatures. It can take up to 10,000 years for a fen to form naturally.

Why Do we need Wetlands?

Long regarded as wastelands, wetlands are now recognized as important features in the landscape that provide numerous beneficial services for people and for fish and wildlife. Some of these services, or functions, include protecting and improving water quality, providing fish and wildlife habitats, storing floodwaters, and maintaining surface water flow during dry periods. These beneficial services, considered valuable to societies worldwide, are the result of the inherent and unique natural characteristics of wetlands.


Your visit

The beginning waypoint will lead you to an observation deck in the middle of the wetland. From the parking area where the bird blind is located, walk to the trail with the orange barrier in front of it. Follow the trail straight down the small hill until you reach the boardwalk. Several hundred feet in front of you will be the boardwalk. During our visit we heard many frogs and saw many birds in the area. This location is very popular for bird and wildlife viewing. Once at the observation deck you will have a wonderfull view of the wetland area around you. As this is an active wildlife area, please be aware that during the months from September thru January active hunting may be taking place.
Extreme caution should be used during those times. Once at the deck, you can perform requirement #2 below. Then hike back to your vehicle and drive around the wetland to the second waypoint. Here you should find an Ohio Historical Marker that has information about the bird species that have been spotted here and other information including requirement #3. At either location you can peform the requirments for #4.


Important reminders
Please email your answers to requirement 1-3 below to our email and post in your log the picture you take for requirement 4.
This is an active wildlife area and hunting is allowed during Ohio's hunting seasons.
All wildlife areas are closed to all activity other than hunting, trapping, and fishing from 8 p.m. to 6 a.m. September 1 through May 1 and from 10 p.m. to 6 a.m. May 2 through August 31.


Now on to the logging requirements for this Earthcache:

1) Based on your observations and the definitions above What type of wetland is this?

2) From the observation deck area - measure from the boardwalk just before the deck the distance from the top of the wood to the water level.
What is that distance on the day of your visit?

3)According to the sign at the second waypoint - how much (in percentage) of the state's orginal wetlands have been destroyed.

4) Finally - take a photo of yourself and gps with the wetland in the background at either location - THIS OF COURSE IS OPTIONAL.


Hunting in area - use caution Hunting in area - use caution
Generated by The Selector

Additional Hints (Decrypt)

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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)