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BC aquifer 1276 · sand and gravel · 13 km² · Central Kootenay

Aquifer 1276: Norns Creek Overburden

Aquifer 1276 (Norns Creek Overburden) is an unconfined sand and gravel (late glacial outwash) aquifer of 13 km² in the Central Kootenay regional district, mapped in 2024. The province rates its productivity moderate, its vulnerability to contamination from the surface high, and the demand on it not rated. 12 wells on record are linked to it; water-supply wells there are typically 17.1 m deep and tested at a median 53 L/min.

How the province rates it

Productivity moderate, vulnerability high, demand not rated.

RatingWhat it means
Productivity
how much water the aquifer gives up to wells, judged from well yields, the aquifer material and pumping tests
moderateMiddling yields: the guide's moderate band is medium sand, or typical well yields of about 0.3 to 3 L/s (18 to 180 L/min).
Vulnerability
how easily something spilled at the ground surface could reach the water, judged from what lies above the aquifer and how deep the water is
high (class A)Little natural protection (the guide's class A): a shallow water table or sand and gravel above it lets surface water and spills soak down quickly.
Demand
how much the aquifer is used now, judged from the number and density of wells and what they're used for
not ratedThe province hasn't rated this for this aquifer.
Level of development Inferred
demand compared with productivity
unclearUnclear: the province hasn't rated both demand and productivity.

Ratings are the province's, set when the aquifer was mapped (2024) from wells, geology and local studies. Vulnerability is about the ground, not what's built on it: a well-protected aquifer under a busy area can still be at more risk than an exposed one in the bush.

Sources: Ground Water Aquifers, Water Protection and Sustainability Branch, Province of BC and Groundwater Wells (GWELLS), Province of BC, as published on October 1, 2026 (Open Government Licence – British Columbia); ratings explained after Berardinucci and Ronneseth (2002), Guide to Using the BC Aquifer Classification Maps for the Protection and Management of Groundwater, BC Ministry of Water, Land and Air Protection. Summaries by PlaceDossier.

The wells in it

12 wells on record are linked to this aquifer.

Wells linked12 (9 water-supply)
Water-supply well depthmedian 17.1 m; middle half 16.2 m to 24.4 m (9 wells)
Tested yieldmedian 53 L/min; middle half 25.5 L/min to 128 L/min (8 wells tested)
Water level below groundmedian 7.6 m when drilled (7 wells)
Drilled1961 to 2019

Depths are how deep the driller finished the well; yields are the driller's test, often an hour or less, in litres per minute. A domestic well's yield is usually judged against the household's peak use; ask a driller what's enough for yours.

Where it is

N 02 km

Outline simplified by us from the provincial map; not for locating a lot. It lies under Central Kootenay, Electoral Area I (64%), Central Kootenay, Electoral Area J (32%).

KindUnconfined sand and gravel - late glacial outwash
Geological unitLate Wisconsinan glaciofluvial sand and gravel
Location, as describedNorns Creek, North of the confluence of the Columbia and Kootenay Rivers
Area13 km²
Mapped2024

Unconfined: nothing tight lies over it, so rain and surface water soak straight down to it; the water table rises and falls with the seasons. The province's page for this aquifer lists the studies behind it and its observation wells: GWELLS aquifer 1276.

Sources: Ground Water Aquifers, Water Protection and Sustainability Branch, Province of BC and Groundwater Wells (GWELLS), Province of BC, as published on October 1, 2026 (Open Government Licence – British Columbia); ratings explained after Berardinucci and Ronneseth (2002), Guide to Using the BC Aquifer Classification Maps for the Protection and Management of Groundwater, BC Ministry of Water, Land and Air Protection. Summaries by PlaceDossier.

What this record doesn't cover

The province maps aquifers where wells and studies give enough to go on, mostly in settled valleys; most of BC isn't mapped, and a lot outside every outline can still have groundwater. Outlines are drawn from geology and well logs at the scale of the study, so an edge can be well off on the ground, and one aquifer can lie under another. Wells are linked to an aquifer by provincial staff from the driller's log: not every well inside an outline is linked, and well depths and yields are as the driller reported them, often from a short test.

These are mapped ratings and drillers' records, not a test of any one lot. Before you buy a property on a well, or plan to drill, ask a qualified hydrogeologist or a registered well driller what this aquifer gives where you are, and test the water.