Waterloo Moraine

The Waterloo Moraine is a geophysical landform in the Regional Municipality of Waterloo, in Ontario, Canada. It covers a large portion of the cities of Waterloo and Kitchener, and the township of Wilmot, and some parts of the townships of Wellesley and North Dumfries.

During late 1989 and early 1990, groundwater contamination in Elmira forced the Region to shut down some well fields.Cite web
url=http://www.waterloohydrogeologic.com/consulting/project_pdfs/RMOW_web.pdf
format=PDF
title=Aquifer Characterization and Capture Zone Delineation for the Region of Waterloo
publisher=Waterloo Hydrogeologic
accessdate=2006-10-05] As a result, new land use management guidelines and water protection measures have been enacted.

The Waterloo Moraine is the largest of fourteen moraines in the Region, spanning approximately 400 square kilometres.Cite web
url=http://www.region.waterloo.on.ca/web/region.nsf/0/5E9A98FD583B353F852570000056FA92/$file/protectingsuprep.pdf?OpenElement
format=PDF
title=Protecting Significant Moraines in Waterloo Region
publisher=Waterloo Region
accessdate=2006-10-05] It is an interlobate moraine, consisting primarily of sand and gravel. It contains large aquifers, which discharge into the Grand River and its tributaries and maintain a base water flow rate into that system.

The origin of the Waterloo Moraine

The Waterloo Moraine was formed as three huge ice lobes retreated across what is now Waterloo Region from Lake Huron in the west, Georgian Bay in the northeast, Lake Ontario in the east and Lake Erie in the southeast. As the glaciers moved, they carried huge boulders, along with sand and gravel and debris. As the ice disappeared, the Waterloo Moraine remained, a huge complex of glacial sediments that is more than 100 metres thick in places. Meltwater streams cascading from the surface of the ice lobes carried enormous deposits of sand and gravel and blocks of bedrock.

International significance

The Waterloo Moraine provides drinking water for over 300,000 people throughout Waterloo RegionCite web
url=http://www.therecord.com/graphics/awards/2106_J01.PDF
archiveurl=http://web.archive.org/web/20061112190209/http://www.therecord.com/graphics/awards/2106_J01.PDF
archivedate=2006-11-12
format=PDF
title=Our Buried Treasure
last=Burtt
first=Bob
publisher=The Record
date=2003-06-21
accessdate=2006-10-05] making this the largest area in North America dependent on ground source drinking water.Fact|date=February 2007 The Waterloo Moraine is currently not protected by provincial legislations although there is an active movement from citizens to see that this takes place.

Louisette Lanteigne and David Wellhauser of Waterlooians have used the Environmental Bill of Rights to submit a Request for Review for a Waterloo Moraine Protection ActCite web
url=http://waterloomoraineact.com/
title=Waterloo Moraine Request for Review] . This resulted in a 16 month review of source water and groundwater protection for the Waterloo Moraine. The findings will be published in September 2008.

How it works

In the vicinity where the three ice lobes began to retreat, sits the recharge areas that allow surface water to enter back into the ground source. The speed of absorption depends on the density of aquifers and aquitards. Aquifers are made up of sand, gravel and silt where the water filters down relatively quickly. The shallow aquifers feed area bodies of water such as creeks and streams while the deeper aquifers feed down to replenish the ground water. The aquitards are the protective layers of clay that slowly filters the water and act to protect the main source from contamination. Left on its own, it is a naturally renewable way to gather fresh drinking water.

Ratio of moraine to recharge

The moraine covers much of the City of Waterloo, Kitchener, Wellesley, Wilmot and North Dumfries covering 400 square kilometres of land. Almost half of the ground water recharge takes place on only 15% of the Grand River Watershed and 80% occurs on only 30% of the land mass most of which is located at the west end of Waterloo Region in the townships of Wilmot and Wellesley.

Dangers to the moraine

The ground water travels down from west to east feeding area wells throughout the region. Subdivision developments in the west end would create more impervious surfaces in the vicinity of the recharge area. Instead of allowing the water to refill the source, the run off will be diverted to sewage systems instead. This will mean a permanent decrease in the volume of water entering area wells. The reduction of water in the wells will significantly increase the parts per billion of contaminants in the system jeopardizing the quality of water in the aquifer and increasing the costs of filtration.

If an increase in traffic follows the development in the vicinity of the aquifer, there will be an increased risk of contamination by road salt which is, according to Environment Canada, a known toxic substanceCite web
url=http://www.ec.gc.ca/substances/ese/eng/psap/final/roadsalts.cfm
title=Assessment Report - Road Salts
publisher=Environment Canada
date=2001-12-01
accessdate=2006-10-05] . Road salt is a form of chloride that kills fish and destroys area creeks and streams.

References

External links

* [http://www.grandriver.ca/index/document.cfm?Sec=14&Sub1=66&Sub2=86 Professor Alan Morgan speaks of the History of the Waterloo Moraine]
* [http://www.therecord.com/graphics/awards/2106_J02.PDF Road Salt Danger to the Waterloo Moraine]
* [http://www.waterlooians.ca/blog/2005_02_27_archive.html International Ground Water Expert Emil Frind Speaks out to protect the Waterloo Moraine]
* [http://www.grandriver.ca/index/document.cfm?Sec=26&Sub1=30 Grand River Conservation Authority's Water Forum Review 2004]

Images and maps

* [http://www.execulink.com/~frind/Vista-Hills/FIG1-P-030.pdf View of the Waterloo Moraine and Recharge areas]
* [http://www.execulink.com/~frind/Vista-Hills/FIG2-P-030.pdf Cross Section of the Waterloo Moraine (west to east)]