PlaceDossier / BC places / Aquifers

BC aquifer 277 · sand and gravel · 96 ha · Thompson-Nicola

Aquifer 277: Davidson Creek

Aquifer 277 (Davidson Creek) is an unconfined sand and gravel (late glacial outwash) aquifer of 96 ha in the Thompson-Nicola Regional District, mapped in 1996. The province rates its productivity moderate, its vulnerability to contamination from the surface moderate, and the demand on it moderate. 8 wells on record are linked to it; water-supply wells there are typically 11.7 m deep and tested at a median 30.3 L/min. It lies under Thompson-Nicola, Electoral Area L (Grasslands) (52%), Kamloops (48%).

How the province rates it

Productivity moderate, vulnerability moderate, demand moderate.

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
moderate (class B)Some natural protection (class B), which can vary across the aquifer.
Demand
how much the aquifer is used now, judged from the number and density of wells and what they're used for
moderateModerately used: about 4 to 20 domestic wells per km² where homes rely on private wells.
Level of development Inferred
demand compared with productivity
Moderate (class II)Read by us from the guide's table of demand against productivity; where it gives two classes the mapper chose with local knowledge. Heavy (I): new wells should be carefully assessed; moderate (II): given careful thought; light (III): more use is usually fine if the aquifer can supply it.

Ratings are the province's, set when the aquifer was mapped (1996) 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

8 wells on record are linked to this aquifer.

Wells linked8
Water-supply well depthmedian 11.7 m; middle half 5.5 m to 13.7 m (8 wells)
Tested yieldmedian 30.3 L/min; middle half 30.3 L/min to 56.8 L/min (5 wells tested)
Water level below groundmedian 5.3 m when drilled (8 wells)
Drilled1945 to 2004

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 01 km

Outline simplified by us from the provincial map; not for locating a lot.

KindUnconfined sand and gravel - late glacial outwash
Geological unitKamloops drift
Location, as describedDavidson Creek
Area96 ha
Water useHousehold wells
Mapped1996

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 277.

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.