PlaceDossier / BC places / Aquifers

BC aquifer 1293 · sand and gravel · 53 km² · Comox Valley

Aquifer 1293: East of Comox Lake, south of Courtenay

Aquifer 1293 (East of Comox Lake, south of Courtenay) is a sand and gravel aquifer of 53 km² in the Comox Valley Regional District, mapped in 2025. Its productivity, vulnerability and demand are not rated. 34 wells on record are linked to it; water-supply wells there are typically 7 m deep and tested at a median 22.7 L/min. It lies under Comox Valley, Electoral Area A.

How the province rates it

Productivity not rated, vulnerability not rated, 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
not ratedThe province hasn't rated this for this aquifer.
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
not ratedThe province hasn't rated this for this aquifer.
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 (2025) 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

34 wells on record are linked to this aquifer.

Wells linked34 (31 water-supply)
Water-supply well depthmedian 7 m; middle half 4.3 m to 13.4 m (31 wells)
Tested yieldmedian 22.7 L/min; middle half 11.4 L/min to 37.9 L/min (13 wells tested)
Water level below groundmedian 3.5 m when drilled (22 wells)
Flowing (artesian) wells2: water rose to or above the ground when drilled
Drilled1950 to 2024
Well depth shallower than 95% of the 637 BC aquifers with at least 10 wells with a depth
131030100300 m Median 7 m from 31 wells
Tested yield lower than 70% of the 542 BC aquifers with at least 10 wells tested
1310301003001,0003,000 L/min Median 22.7 L/min from 13 wells

This aquifer's medianIts middle half of wellsAnother BC aquifer's median

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.

KindSand and Gravel
Geological unitFluvial, and lacustrine sediments
Location, as describedEast of Comox Lake, south of Courtenay
Area53 km²
Mapped2025

The province's page for this aquifer lists the studies behind it and its observation wells: GWELLS aquifer 1293.

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.