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Hidden : 09/21/2014
5 out of 5
5 out of 5

Size: Size:   other (other)

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Geocache Description:

Beaver Creek Fiddlar's Rapids is 350 metres of amazing examples of the ancient processes which occurred both during the glacier period and in the thousands of years since that time. You will need a boat to get to the rapids where you can get out and walk down the river bed when water levels are low enough to be able to hop from rock to rock or wade in rubber boots or water shoes.



(A Comparative Analysis of Glacial Erosion and Flood/River Water Erosion)

The put-in at the bridge on Beaver Creek Road

N  44° 32.008     W  077° 41.845

Use the southeast side of the bridge to pull over and park your vehicle. From there you can slide your boat over the grass and down the slope to the water. It is a one kilometre flat paddle to Fiddlar's Rapids.

Alternate put-in :  Marmora Mag's Landing Boat Launch, Cordova Road, on the Crowe River. There is ample parking and a portable toilet. It is about 1 kilometre from the boat launch to the entrance to Beaver Creek and another 2 kilometres up Beaver Creek to the south end of Fiddlar's Rapids. However, if you choose this route, you will be unable to access the Labyrinth Rock as it is in the river, just north of the rapids. If you choose this route, you will have a lovely paddle and the CO will allow you to log it as a "find", but you will miss the "Wow!" of seeing the Labyrinth Rock.

Background Information:

Beaver  Creek  is a river flowing south from Limerick Lake, near Bancroft, to the Crowe River in Marmora.  The river lies predominantly in the rugged Canadian Shield where outcrops of granite and other Precambrian rocks are located at or near the surface.
The Precambrian Era is the most ancient of all earth's historical periods and dates back to the very formation of the world as we know it. The rocks at this Earthcache, therefore, could be as old as the earth itself.
In this particular location on Beaver Creek,  there is striking evidence of the Great Ice Age and the huge glaciers which carved and gouged out the landscape, scraping away the topsoil and leaving depositions of granite rocks, bare rock outcrops, cracked and broken slabs of limestone, a variety of metamorphic rock formations caused by pressure and stress, and the rough terrain typical of the Canadian Shield.
This section of  Beaver  Creek  called, Fiddlar's Rapids, is a textbook example of the variety of processes that took place at the time of the receding glaciers, and the eroding remnants of that period in the earth's history.

What is also fascinating here in the Fiddlar's Rapids, is that we can see erosion happening in front of our eyes. Because this river is flooded every spring, there is a significant amount of water erosion taking place on the limestone beds, that we can witness, photograph and document.

Why is this Earthcache listed as Difficulty Level 5 and Terrain Level 5 ?

You are being asked to give descriptions of what you see and then make deductions based on your observations. The requirements may take some time, some research and some thought, in order to fulfil them. Furthermore, Beaver  Creek  Earthcache  is only accessible by watercraft (canoe, kayak) and then, only in the months when fluctuating water levels are low enough so that the rocks are visible. The best, and perhaps only, months to visit are during July, August, September and possibly early October, (if warm enough). It is not possible to obtain the answers during the winter months when the rocks will be covered by ice and snow. Nor is it possible to complete this Earthcache in the months of April or May, as the spring run-off makes water levels so high that Beaver Creek's rocks are hidden below several feet of rushing water. In fact, Beaver Creek, including Fiddlar's Rapids, becomes a popular playground for white water kayakers ( MACKFEST, Marmora and Area Canoe and Kayak Festival).   Environment Canada now posts information on water discharge levels for the various months of the year for Beaver Creek which you can access online (see the link in the RESOURCES).

From the chart, you can see that your best bet for exploring the river bed of the Fiddlar's Rapids is during the summer and early fall.  Please wear appropriate footwear for walking on a rough river bed and be prepared to get wet. Take a first aid kit in your boat and watch the sharp rocks on the bottom of your boat. Steer around them.


There are two main types of erosion evident in Fiddlar Rapids:

* Glacial Erosion

- historical (occurred in the past)

* Water/Flood Erosion

- current (is still happening)

Glacial Erosion:

Glaciers were the giant bodies of ice, sometimes up to several kilometres high, that covered much of North America before receding north; and which are responsible for most of the topography of the Canadian Shield. These glaciers were a powerful eroding machine that could pluck up huge pieces of rock, rolling and tumbling them until finally dumping them off (this process is called "plucking"). The plucked rocks and the ice in the glaciers gouged and carved the landscape. In Fiddlar Rapids, many of the features you see, are from glacier erosion. During the time of the glaciers, there were many catastrophic forces being exerted on the rock below the heavy masses of ice. The basal igneous rock, below the surface, was under immense pressure and stress, as well as temperatures of up to 700 degrees Celsius (which can be deduced by the presence of gneiss rock), causing minerals to be altered into the spectacular metamorphic formations you will see in Fiddlar's Rapids.  (United World College)

Water Erosion:

Water erosion occurs from chemicals, saline content, and acid in the water, as well as the force (velocity) of the flow of water in a river. There are many chemicals that enter a river; and those chemicals can break down sedimentary rock, such as limestone. This eroded rock is then carried down the river. Sometimes, a crack or crevice develops. When the force of the flowing river smashes into that crack, continuously, over long periods of time, the rock can break away. Post glacial melt waters and the thousands of years of natural erosion following the Ice Age, in addition to our Canadian seasons of extreme temperature changes, have further impacted the rocks in Fiddlar's Rapids.

The following are the predominant features of Fiddlar's Rapids which fall into either the category of Glacial Erosion or River Erosion:


- is a feature of the glacier age. A fold occurs when one or a stack of originally flat and planar surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation. Similar to the way an accordion folds when pressure is applied to the outside of the instrument and the accordion is squeezed, folds in rock form under conditions of stress, hydrostatic pressure and temperature fluctuations.  There is evidence here at Fiddlar Rapids of catastrophic folding of soft, waterlogged sediment and structures resulting from movement of sediment after deposition but prior to cementation. Some folds are symmetrical, while others are asymmetrical. Folds in rock are formed in relation to the rheology (the method of response to stress). For example, rocks that deform more easily, form many short-wavelength, high-amplitude folds. Rocks that do not deform as easily form long-wavelength, low-amplitude folds.


Glacial striations

are scratches or gouges cut into bedrock by glacial abrasion. Glacial striations are usually multiple, straight, and parallel, representing the movement of the glacier using rock fragments and sand grains, embedded in the base of the glacier, as cutting tools. Large amounts of coarse gravel and boulders carried along underneath the glacier provide the abrasive power to cut trough-like glacial grooves. Ice itself is not a hard enough material to change the shape of rock but because the ice had rock embedded in the basal surface, it could effectively abrade the bedrock.


Clints, Grykes, Fissures and Interstices

- These are all erosive features mainly from the glacial period, although rocks do crack due to water erosion and the pressure of ice or tree roots. Limestone is slightly soluble in water and especially in acid rain, so corrosive drainage along joints and cracks in the limestone can produce slabs called "clints" isolated by deep fissures or interstices called "grikes" or "grykes".  As water moves through spaces between mineral grains, it works to dissolve and carry away different elements. Some types of minerals are easily dissolved and others less so. Rainwater absorbs carbon dioxide (CO2) as it falls through the air. The carbon dioxide combines with water to form carbonic acid. This naturally occurring weak acid readily dissolves many types of rock, including limestone.  Fissures are long, narrow cracks or openings in the face of a rock. Sometime fissures will fill with minerals of a different type from those in the surrounding rock. Limestone has a distinctive crystal structure and it will fracture and crack in a specific pattern. High carbon dioxide levels made the river water slightly acidic and it dissolved the limestone here in Fiddlar's Rapids, over thousands of years, widening the natural cracks and fissures in the rock.



- Potholes are small kettles (also known as "rockmills"). These develop in the bed of a fast flowing river wherever an eddy in the current causes stones or sand grains to be caught and swirled around in the same place over a long period of time. There are many small potholes in Fiddlar's Rapids. Geologists believe these were initially formed at the time of the Ice Age.


- Slate is shale that has been subjected to heat and intense pressure deep under the surface, usually in plate collision settings. Slate is created by regional, low-grade metamorphism of shale. It is composed of micaceous minerals, and could contain quartz, calcite, dolomite, feldspar, pyrite, graphite, chlorite, and other minerals. Slate is the finest grained foliated, homogeneous metamorphic rock. Chunks of flat dark grey slate are scattered throughout Fiddlar Rapids.

Fiddlar's Rapids is a geologist's heaven, because of the variety of geological features that can be clearly seen simply by walking up the river bed when water levels are low enough to be able to hop from rock to rock or simply wade in your rubber boots or water shoes. Beaver Creek's Fiddlar's Rapids is 350 metres of amazing examples of the ancient processes which occurred both during the glacier period and in the thousands of years of natural river erosion since that time.

Every rock in Fiddlar's Rapids has a story to tell. Your job is to figure out what those stories might be.


Assuming you put in at the bridge on Beaver Creek Road and traveled south on the river, you will attempt the following challenges in this sequence:

1. Go to the "Labyrinth Rock" which is upriver (north) of Fiddlar's Rapids, about 230 metres. The co-ordinates for the "Labyrinth Rock" are  N  44° 31.585    W  077° 42.128   .  Describe the size of the rock (what you can see) and the features of the rock. Postulate how this geological feature was formed; was it as a result of glacial erosion or more recent river/water erosion? Take a picture of your hand or your GPS with the Labyrinth Rock in the background. (The photo is optional as per Earthcache regulations). Post the picture online with your log. Send the answers to the CO in an email.

2. Next, you will arrive at the top of Fiddlar's Rapids where you can pull your boat up on the rocks and get out to explore. You will be at  N  44° 31.528    W  077° 42.242   .  Walk to N  44° 31.499    W  077° 42.209.   What is the geological feature at those co-ordinates? Again tell whether or not you think this feature is a result of glacial erosion or water erosion.  Email the CO your answers.

3. Continue on to  N  44° 31.493    W  077° 42.198   .   What is happening here? Is this erosion a feature of the glacial period, or of more recent erosion due to the action of water flow? Email the CO your answers.

4. Go to  N  44° 31.509    W  077 ° 42.193   .   What is here? Email the CO your answers. 

5. Find a fold. You cannot use my Labyrinth Rock for this requirement. Find your own ! It does not need to be a fold which has interstices. It could just be an "S" shape you see in the rock. Tell whether the fold is a short wavelength, high amplitude fold or a long wavelength, low amplitude fold, relative to (as compared to) the folds in the Labyrinth Rock. (Optional : Take a photo of the fold and post this with your log).

6. Find a chunk of dark grey slate and a piece of limestone. Using the limestone as chalk and the slate like a school blackboard, write something on your chalkboard and take a picture, (the photograph is optional). Post the picture with your log online.  This requirement does not break the "Leave No Trace" ethics, as the next rainfall will erase your chalkboard.

Resources    Outside Web Page :

Many thanks go to Moorely for all the help with html and developing this page.

I have earned GSA's highest level:

Additional Hints (Decrypt)

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Decryption Key


(letter above equals below, and vice versa)

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