PlaceDossier / BC places / Aquifers
BC aquifer 909 · sand and gravel · 23 ha · qathet
Aquifer 909: Indian Point - Savary Island
Aquifer 909 (Indian Point - Savary Island) is an unconfined sand and gravel (late glacial outwash) aquifer of 23 ha in the qathet regional district, mapped in 2007. The province rates its productivity low, its vulnerability to contamination from the surface high, and the demand on it high. No wells are linked to it in the provincial well records.
How the province rates it
Productivity low, vulnerability high, demand high.
| Rating | What it means | |
|---|---|---|
| Productivity how much water the aquifer gives up to wells, judged from well yields, the aquifer material and pumping tests | low | Water comes slowly: the guide's low band is silt, fine sand or fractured bedrock, or typical well yields under about 0.3 L/s (18 L/min). A well may still supply a house, but it isn't assured. |
| 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 | high | Heavily used: where homes rely on private wells, the guide's heavy band is over 20 domestic wells per km². |
| Level of development Inferred demand compared with productivity | Heavy (class I) | 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 (2007) 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
No wells are linked to this aquifer in the provincial well records.
Wells may still draw from it: linking is done by hand from drillers' logs and many old wells were never registered.
Where it is
Outline simplified by us from the provincial map; not for locating a lot. It lies under qathet, Electoral Area A.
| Kind | Unconfined sand and gravel - late glacial outwash |
|---|---|
| Geological unit | Quaternary Quadra sands |
| Location, as described | Indian Point - Savary Island |
| Area | 23 ha |
| Water use | Household wells |
| Water quality concerns | Regional: concerns documented across much of the aquifer |
| Mapped | 2007 |
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 909.
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.