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BC aquifer 1235 · sand and gravel · 11 km² · Metro Vancouver

Aquifer 1235: West Langley

Aquifer 1235 (West Langley) is an unconfined sand and gravel (large river system) aquifer of 11 km² in the Metro Vancouver regional district, mapped in 2019. The province rates its productivity not rated, its vulnerability to contamination from the surface high, and the demand on it not rated. 57 wells on record are linked to it; water-supply wells there are typically 9.6 m deep and tested at a median 161 L/min.

How the province rates it

Productivity not rated, 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
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
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 (2019) 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

57 wells on record are linked to this aquifer.

Wells linked57 (15 water-supply)
Water-supply well depthmedian 9.6 m; middle half 5.6 m to 15.1 m (15 wells)
Tested yieldmedian 161 L/min; middle half 89.9 L/min to 260 L/min (6 wells tested)
Water level below groundmedian 4 m when drilled (13 wells)
Drilled1901 to 2017
Well depth shallower than 92% of the 637 BC aquifers with at least 10 wells with a depth
131030100300 m Median 9.6 m from 15 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. It lies under Langley (78%), Surrey (19%).

KindUnconfined sand and gravel - large river system
Geological unitFraser River Sands and Sumas Drift
Location, as describedTownship of Langley/Surrey
Area11 km²
Mapped2019

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 1235.

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.