Surface Water and Groundwater

Credit River Watershed

Precipitation that falls as rain or snow follows one of three major routes:

  • Runs off to a lake, wetland or pond
  • Runs off over the land to a river or creek
  • Is absorbed into the ground and eventually seeps through into the groundwater (known as infiltration). 

Surface water is the water that flows on the surface of the earth, as in the first and second point above. But groundwater is different. Groundwater is found underground in the cracks and spaces in rocks, soils and sands.

Imagine pouring a glass of water onto a pile of sand. Where does the water go? The water moves into the spaces between the particles of sand. Groundwater is the same. Groundwater is stored in, and moves slowly through layers of soil, sand and rocks called aquifers. Heavy rains or melting snow may cause the water table to rise as more water is stored in the aquifer. An extended period of dry weather may cause the water table to fall, as less water is stored in the aquifer.

The speed at which groundwater flows depends on the size of the spaces in the soil or rock and how well the spaces are connected. It may move several hundred metres a year in fractured limestone rock, or only move several centimetres a year through clay.

In our area groundwater eventually flows into creek, a river or even into Lake Ontario itself.

In many communities, groundwater is the sole source of water. In the Credit River Watershed, our municipalities are the largest consumers of groundwater, providing it to their local communities from underground wells.

Did you know…?

  • Two-thirds of the world’s freshwater supply is found underground
  • Approximately 50% of the average flow in the Credit River comes from groundwater
  • The Caledon Creek Wetlands, Silver Creek, and the Credit River all depend on groundwater

Water that flows into the watershed also leaves our watershed by four natural means:

  • Evaporation from lakes, rivers and soil
  • Released by plants and trees, called transpiration
  • Creek and river runoff to Lake Ontario
  • Discharges of groundwater into a river or creek or into Lake Ontario

Recently, people have become concerned about the removal of water from watersheds by other, human-caused, means. These include diversions (damming or changing the course of a river to increase or decrease water supplies elsewhere) and removal (losing water by shipping it out as bottled water or in agricultural products high in water).

Data and information released from Credit Valley Conservation (CVC) are provided on an 'AS IS' basis, without warranty of any kind, including without limitation the warranties of merchantability, fitness for a particular purpose and non-infringement.

Availability of this data and information does not constitute scientific publication. Data and/or information may contain errors or be incomplete. CVC and its employees make no representation or warranty, express or implied, including without limitation any warranties of merchantability or fitness for a particular purpose or warranties as to the identity or ownership of data or information, the quality, accuracy or completeness of data or information, or that the use of such data or information will not infringe any patent, intellectual property or proprietary rights of any party. CVC shall not be liable for any claim for any loss, harm, illness or other damage or injury arising from access to or use of data or information, including without limitation any direct, indirect, incidental, exemplary, special or consequential damages, even if advised of the possibility of such damages.

In accordance with scientific standards, appropriate acknowledgment of CVC should be made in any publications or other disclosures concerning data or information made available by CVC.