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Matchedash Wetlands EarthCache

Hidden : 5/27/2009
Difficulty:
2.5 out of 5
Terrain:
3.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

The posted coords are within a section of the wetlands. You will probably get your feet wet if you try to go to the posted coords. Your best bet is to initially go to the coords indicated in Question #1.


The Matchedash Wetlands can be accessed from Swift Rapids Road (high clearance 4 wheel drive vehicle recommended) and are geographically located within the southern portion of the Canadian Shield, which is the largest shield in the world. The area owes its present-day appearance to both a very long period of erosion, which has worn down contours that were once spectacular and also much more recent events which occurred during the last glacial period which ended 10,000 years ago. Like monstrous machines, the ice sheets literally scraped and denuded the area, pushing loose soil ever farther in front of them. The glaciers also greatly disrupted the watercourses, filling creek beds and carving canals. Many poorly drained depressions as well as natural faults in the bedrock were left behind and these formed millions of lakes, ponds and wetlands which give this ecozone it's distinctive character. These upheavals explain the young and somewhat erratic character of the current hydrographic network, with its multitude of lakes and swamps and its series of falls and rapids. The multitude of rivers and lakes in the entire region is caused by the watersheds of the area being so young and in a state of sorting themselves out with the added effect of post-glacial rebound. The area originally consisted of very large mountains (about 12,000 meters in height) with much volcanic activity, but over the millennia the area was eroded to its current topographic appearance of relatively low relief and contains some of the most ancient volcanoes on Earth. The wetlands here are freshwater and while driving along the Swift Rapids Road one can see at least 4 of the 5 examples of the types of wetlands indicated below including a spectacular and very eerie example of a swamp that goes right up to and is almost level with the road during the Spring season.

A wetland is an area of land whose soil is saturated with moisture either permanently or seasonally. Such areas may also be covered partially or completely by shallow pools of water. There are many different types of wetlands. The water found in wetlands can be saltwater, freshwater, or brackish. Wetlands are considered the most biologically diverse of all ecosystems.

Wetlands are not land or water, but a fluid combination of both, wetlands are among the most productive habitats on Earth. Wetlands are all built on a simple foundation: water becomes trapped, either through poor drainage, periodic flooding or by coastal barriers such as sandbars, and a wetland -- that unique mix of land and water -- is born.

From this beginning, wetlands develop in a number of ways depending on local climate conditions, the availability of nutrients, and the geography and soils of a site. They also change over time: an open marsh may dry out enough to become a wooded swamp, only to revert back to open marsh again after heavy flooding.

Wetlands represent one of the most important life support systems in the natural environment. Wetlands provide:

  • A water filtration system...removing contaminants, suspended particles and excessive nutrients, improving water quality and renewing water supplies.
  • An irreplaceable habitat...nesting, feeding and staging ground for several species of waterfowl and other wildlife such as reptiles and amphibians, and also for many species at risk.
  • A high quality spawning and nursery area for many species of fish.
  • Natural shoreline protection...protecting coastal areas from erosion.
  • A reservoir...helping to control and reduce flooding through water storage and retention.
  • A source of oxygen and water vapour...playing a vital role in the natural atmospheric and climatic cycles.
  • Recreational activities...hiking, birdwatching and fishing.
The functions and values of wetlands are becoming increasingly clear to scientists and those who manage wetlands. However, the difficulty faced by these individuals is how to communicate these functions and values in a way that will be understood by land owners, government regulators and the public. In other sectors of the economy, the most common way of demonstrating the value of something is to quote a price. But what is the price of a wetland?

The five major freshwater wetlands types in Ontario are:

Marshes:
These wetlands are periodically or permanently covered by standing or slowly moving water. Marshes are rich in nutrients and are characterized by an emergent vegetation of reeds, rushes, cattails and sedges. Water remains within the rooting zone of these plants for most of the growing season. Marshes are the most productive wetlands habitat.

Swamps:
Swamps are dominated by shrubs or trees. They may be flooded seasonally or for long periods of time. Swamps are both nutrient rich and productive. Vegetation may be composed of coniferous or deciduous forest or tall thickets. Swamps are most common in temperate areas of Canada.

Bogs:
Bogs are peat-covered wetlands in which the vegetation shows the effects of a high water table and a general lack of nutrients. Due to poor drainage and the decay of plant material, the surface water of bogs is strongly acidic. Although they are dominated by sphagnum mosses (peat) and heath shrubs, bogs may support trees. More common in northern Ontario and rare in the south, bogs are the least productive of all wetland types.

Fens:
These wetlands are characterized by a high water table with slow internal drainage by seepage down low gradients. Their surface waters may be acidic or alkaline. Fens are not as low in nutrients as bogs and as a result are more productive. Although fens are dominated by sedges they may also contain shrubs and trees. Like bogs, they are more common in the north.

Shallow Open Water:
These wetlands include potholes and sloughs (ponds), as well as waters along rivers and lakeshore areas. They are usually relatively small bodies of standing or flowing water commonly representing a transitional stage between lakes and marshes, or between spring high water levels and levels during the remainder of the year.

Questions to Answer:

1) Go to N44 48.913 W79 32.313 where you will have an elevated view of the wetlands. Look across the wetlands to the north. About how far is it to the other side? Either estimate or walk in a counter clockwise direction in order to get to the other side.

2) What may have contributed to these lands turning into wetlands? Hint: Try going to N44 48.967 W79 32.238 and N44 49.014 W79 32.326 to find a possible answer.

3) Go to the edge of the wetlands where you will find some open water around part of the perimeter and measure how deep the water is.

4) Would this water be safe to drink? Why or why not? If you had something to be concerned about, what things might you be concerned about if you decided to (or needed to) drink the water?

5) What type of wetlands is this here? Select one of the 5 types described above.

6) Finally, take note of any wildlife that you spot either in the wetlands themselves or on your way to these wetlands.

7) Pictures are always appreciated. If possible try to post some pictures of the wetlands.

Go ahead and log your find after you email me the answers to the above questions. You do not need to wait for me to reply.

Additional Hints (No hints available.)