Groundwater Mapping Program
Program Manager: Alfonso Rivera
Groundwater is important to health, economy and ecosystems in Canada. It provides drinking water to about one third of all Canadians and up to 80% of the rural population. It has been routinely surveyed since early last century, yet groundwater has not been mapped in a systematic way across the country. The NRCan Groundwater Mapping program, a current federal groundwater initiative, aims to establish a conceptual framework of national, regional and watershed-scale groundwater flow systems.

The nine hydrogeological regions include:

The nine hydrogeological regions include:
Cordillera: Mountains with thin sediment over fractured sedimentary, igneous and metamorphic rocks of PreCambrian to Cenozoic age. Intermontane valleys are underlain by glacial and alluvial deposits of Pleistocene age.
Western Canada Sedimentary Basin: Region-wide basin of sub-horizontal Paleozoic to Cenozoic sedimentary rocks are overlain by thick glacial deposits filling buried valleys. Incised post-glacial valleys provide local relief. Shallow gas, coal, and brines may occur.
Canadian Shield: Undulating region of thin glacial sediment overlying complex deformed, fractured PreCambrian igneous, metamorphic and sedimentary rocks. Region contains several terrains: sedimentary basins, structural belts, and glacial-lacustrine basins.
Hudson Bay Basin: Sedimentary basin of Paleozoic to Mesozoic subhorizontal carbonate and clastic sediment covered by surficial deposits, with low relief and poor drainage.
Southern Ontario Lowlands: Eastern Great Lakes region is underlain by gently-dipping Paleozoic, carbonate, clastic and gypsum-salt strata overlain by glacial sediments up to 200 m thick with tunnel valleys. Karst, bedrock valleys, shallow gas and brines are also important components.
St. Lawrence Lowlands: Lowlands underlain by shallow-dipping Paleozoic sedimentary rocks and thick glacial sediment in glacial-marine basins. Appalachian and PreCambrian uplands discharge water to valleys. Shallow gas and saltwater intrusion are possible.
Appalachian Mountains: Upland to mountainous region with thin surficial sediment on folded Palaeozoic sedimentary and igneous rocks. Range of rock types yields a wide range of water compositions. Valleys contain important alluvial aquifers.
Maritimes Basin: Lowlands with flat-lying, Carboniferous clastic , salt, and gypsum rocks contain shallow coal deposits. Surface glacial sediment is thin and discontinuous. Salt water intrusion is possible.
Permafrost: Arctic islands and most areas north of 60° contain frozen ground affects on groundwater flow. Diverse topography and geology define sub-regions of sedimentary basins and crystalline rocks. Glacial sediment is thin, discontinuous; local peat accumulations are significant.
| Region | Aquifer | ID on map | Province | Size | Usage | Status | Risk |
|---|---|---|---|---|---|---|---|
| Cordillera | Gulf Islands fractured aquifers | 1 | BC | 475km2 | D | Completed | GP, C |
| Nanaimo Lowland | 2 | BC | D, A | ||||
| Fraser Lowlands | 3 | BC | D, A | Completed | |||
| Okanagan Valley | 4 | BC | 1000 km2 (CAN) | D | Underway | GP, A | |
| Shushwap Highlands | 5 | D | |||||
| Western Plains | Paskapoo | 6 | AB | 70000 km2 | D, E, A, I | Underway | GP, E, A, I, G |
| buried valley/blanket aquifers | 7 | AB, SK, MB | D, E, I | ||||
| Upper Cretaceous sands | 8 | AB,SK | D, A | ||||
| Milk River | 9 | AB | D, A | ||||
| Judith River | 10 | SK, AB | D, A | ||||
| Eastend-Ravenscrag | 11 | SK | D, A | ||||
| Inter-till aquifers | 12 | AB, SK, MB | D, A | ||||
| Carbonate rock | 13 | MB | D | ||||
| Basal Clastic Unit (Winnipeg) | 14 | MB | D, I | Completed | |||
| Odanah shale | 15 | MB | D | ||||
| Sandilands | 16 | MB | 400 km2 | D | Underway | GP, A | |
| Assiniboine delta | 17 | MB | D | ||||
| Southern Ontario | Oak Ridges Moraine [1] | 18 | ON | 2500 km2 | D, I | Completed | GP, I |
| Grand River Basin | 19 | ON | D | ||||
| Credit River | 20 | ON | D | ||||
| Waterloo Moraine | 21 | ON | D | ||||
| Upper Thames | 22 | ON | D | ||||
| Maritimes Basin | Annapolis-Cornwallis valleys | 23 | NS | 2600 km2 | D, A | Completed | GP, A |
| Carboniferous basin | 24 | PEI, NB, NS | 11000 km2 | D, A | Completed | GP, A | |
| St. Lawrence Lowlands and Appalachia | Mirabel | 25 | QC | 1500 km2 | D, A, I | Completed | GP, A, I |
| Châteauguay | 26 | QC | 1450 km2 (CAN), 1200 km2 (USA) | D, A, I | Completed | A, I | |
| Richelieu | 27 | QC | D, A | A | |||
| Chaudière | 28 | QC | D, A, I | A | |||
| Maurice | 29 | QC | D, I | ||||
| Portneuf | 30 | QC | 525 km2 | D, A | Completed | ||
|
Usages = Domestic (D), Agriculture (A), Energy (E), Industry (I) Risks = Growing Population (GP), Agriculture (A), Industry (I), Energy (E), Contamination (C), Geothermal Energy (G) Note: blank cells denote unknown information |
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Project Highlights (2003-2009)
Project J01 - Groundwater Knowledge synthesis and Program Management
Project J02 - National Groundwater Database, Outreach and Monitoring
Project J03 - Assessment of Regional Aquifers: Towards a National Inventory
Project J04 - Thematic Groundwater Research
Project J05 - Remote sensing in support of groundwater monitoring and vulnerability assessment
Project J06 - Groundwater Inventory: aquifer systems in Canada
Project J07 - Groundwater Pathways, Database, Information Transfer
Project J08 - Groundwater Earth Observation and Thematic Research