Skip to content

Flow, Flow the Waters of Holland Marsh EarthCache

This cache has been archived.

Ge0tchr: Taking down all of my caches as I am disabling my account for a time as I am disillusioned with geocaching and do not have the time/interest in maintaining caches anymore.

More
Hidden : 12/5/2008
Difficulty:
2 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:


Thanks to Juicepig for all of your help!

The Holland Marsh forms one of two large valleys that were originally arms of Glacial Lake Algonquin. Formed by the result of the melting of this giant lake over 15, 000 years ago, this northeast-southwest valley forms a tunnel channel and is an integral part of the Oak Ridge’s Moraine system. For many years, the rich sediment here acted as a filter for the groundwater produced by the aquifer in the area.

Figure 1: The Holland Marsh and surrounding area geological landforms

Then along came Professor Day... In the early 1900s a Bradford Grocer, Dave Watson, wrote to William H. Day, then a University of Guelph physics professor, about his idea to turn this area into agricultural lands. Day then began his plan of re-routing rivers, building dykes and canal systems until the marsh had been drained into agricultural lands. Through the continued use of pesticides and agricultural development, serious concerns through numerous hydrological and hydro chemical studies have been raised as to the levels of pollutants in the groundwater in this area.

Figure 2: Geological formation of Oak Ridges Moraine

In addition to this, little is known about the effects of rapid urbanization in the area. Roads and surfaces such as this may reduce the recharge rates of groundwater and lead to it being backed up in storm sewers. Other effects that may lead to damage of the area may include large-scale urban consumption of groundwater, salting of roads and the effects of septic systems. As the aquifer releases ground water slowly, the damage may not be evident for many years. Pumping stations were established in the Marsh to drain groundwater off of the Marsh. The coordinates above will take you to the Art Janse Pumping Station, one of two in the Holland Marsh.

TO LOG THIS ONE!

1) Got to the following coordinates N 44 06.638 W 079 32.735. Be careful of your footing here and be careful of any children you have along with you. Take a look at the ground water being pumped out of the pump house (the ripples in the water near the pump). The pipe is located underneath the pump in the water and pumps directly into the river. You need to calculate the rate of flow of the discharge and the depth of the water being pumped out into the holding tank. The discharge is intermittent so you might have to wait ( Take note of the hint especially in winter). For this calculation you need to determine the velocity (v=d/t) of the water coming out of the pipe and the diameter of the pipe which is 2 metres. Take your best guess of the velocity and the depth of the water. Send your findings to me via an e-mail.

2) Take a look at the Holland River next to the pump house. Estimate the depth of the river. You don’t need to go near the river. Just stand on the road next to it. Send your findings to me via an e-mail.

Additional Hints (Decrypt)

Gurer ner znal jrofvgrf gung jvyy uryc jvgu gur sybj engr pnyphyngvba. Gur qvfpunetr engr vf irel fybj va jvagre gvzr fb vs gurer vf ab boivbhf qvfpunetr gur sybj engr jbhyq or 0.

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)