BC aquifer 456 · sand and gravel · 10 km² · Columbia Shuswap

Aquifer 456: Golden, confluence of 2 rivers

Aquifer 456 (Golden, confluence of 2 rivers) is an unconfined sand and gravel (medium stream system) aquifer of 10 km² in the Columbia Shuswap Regional District, mapped in 2003. The province rates its productivity high, its vulnerability to contamination from the surface moderate, and the demand on it moderate. 47 wells on record are linked to it; water-supply wells there are typically 22.6 m deep and tested at a median 1,325 L/min. It lies under Golden (82%), Columbia-Shuswap, Electoral Area A (18%).

How the province rates it

Productivity high, vulnerability moderate, demand moderate.

	Rating	What it means
Productivity how much water the aquifer gives up to wells, judged from well yields, the aquifer material and pumping tests	high	Wells here tend to yield well: the guide puts high productivity at coarse sand and gravel, or typical well yields over about 3 L/s (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	moderate	Moderately used: about 4 to 20 domestic wells per km² where homes rely on private wells.
Level of development Inferred demand compared with productivity	Moderate or light (class II or III)	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 (2003) 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

47 wells on record are linked to this aquifer.

Wells linked	47 (24 water-supply)
Water-supply well depth	median 22.6 m; middle half 12.5 m to 25.9 m (23 wells)
Tested yield	median 1,325 L/min; middle half 961 L/min to 1,893 L/min (6 wells tested)
Water level below ground	median 4.6 m when drilled (19 wells)
Drilled	1950 to 2023

Well depth shallower than 73% of the 637 BC aquifers with at least 10 wells with a depth

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

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

Kind	Unconfined sand and gravel aquifer - medium stream system
Location, as described	Golden, confluence of 2 rivers
Area	10 km²
Water use	Several uses (for example household wells, water systems, irrigation or industry)
Water quality concerns	None documented
Mapped	2003

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 456.

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.