Regional groundwater summary • GWDrill Historical Log Extraction
Bottom Line Up Front
In RM of Armstrong, the median completed well is 123 ft deep.
A published hardness range for this place and aquifer is under 60 to above 180 mg/L as CaCO₃. That is a regional estimate, not a test of your well. Source: Estimate based on Health Canada hardness bands.
Most production draws from LIMESTONE OR DOLOMITE (about 77% of local wells).
These municipal aggregates support planning only — they do not replace an accredited laboratory potability test for your own well.
Interactive Well Depth & Geological Stratigraphy (From Local Driller Logs)
Drag the indicator line or tap a geological stratum below to read the recorded depth range
Modelled Depth
123 FT
Area median
Drilling cost
$8,610–$18,450
Estimate
Published hardness
under 60 to above 180 mg/L as CaCO₃
From local driller logs.
Local measurements compared against Manitoba provincial benchmarks.
| Hydrogeological Metric | From the registry or a cited study | MB Provincial Benchmark |
|---|---|---|
| Total Registered Wells | 1,420 | — |
| Median Well Depth | 123 ft | 88 ft provincial median |
| Average Well Depth | 138.6 ft | — |
| Recorded Depth Range | 11 – 1201 ft | — |
| Dominant Aquifer | LIMESTONE OR DOLOMITE | — |
| Hardness | under 60 to above 180 mg/L as CaCO₃ — Estimate. Estimate based on Health Canada hardness bands | — |
| Drilling cost | $8,610–$18,450 — Estimate. Typical drilling prices in Canada, about $70–$150 per foot | — |
| Domestic Household Use | 0% of wells | — |
Approximate boundary of RM of Armstrong
Shaded area is an approximate municipal outline for orientation only. Well records are aggregated across the entire RM of Armstrong.
Most completed wells fall near the median depth of 123 ft. Recorded depths cover 1,211 wells.
Median depth of 123 ft falls inside the reported range. Deeper completions here usually mean higher mineral content but steadier year-round pressure.
Bedrock and drift aquifers recorded by drillers in this area.
1,094 of 1,420 Major regional bedrock aquifer formed by Ordovician/Silurian dolomite. Known for reliable, high-volume yields with elevated mineral hardness and dissolved calcium/magnesium carbonates.
311 of 1,420 Unclassified hydrogeological formation from legacy provincial drill records.
11 of 1,420 Shallow to intermediate glacial drift aquifer deposited in alluvial channels or outwash plains. Yields softer water but requires continuous sediment filtration and shallow bacterial monitoring.
2 of 1,420 Fractured sedimentary shale formation (including Odanah / Pierre members). Characterized by high total dissolved solids (TDS) and potential sulfur/iron compounds.
1 of 1,420 Deep basal sandstone bedrock unit (including Winnipeg Formation). Supplies exceptionally stable yields; often exhibits moderate mineral hardness with silica-rich water.
1 of 1,420 Dense, low-permeability clay-rich glacial deposits with localized silt lenses. Serves as a natural confining barrier protecting deeper aquifers from surface contamination.
69 holes found no usable water. test holes, observation or monitoring wells, dewatering wells, decommissioned wells, dry holes, no-aquifer holes, and other non-supply wells filtered out of the headline
A published hardness range, when one exists for this place and aquifer. Not a test of your well.
Measured nearby
Measured government tests within 25 km of RM of Armstrong.
USGS (2018) bands reprinted by Health Canada. A range can cross more than one band. This is not a sample.
What this is not
Health Canada has not set a maximum acceptable concentration for hardness. A wide published range can sit in more than one USGS band.
43 wells tested, range 275–679 mg/L.
1.67 km away, nearby.
Tests dated 1994, some undated.
These results are old (tested 1994).
43 wells test above 180 mg/L.
Worked out by wellwaterguide.ca from 43 government lab tests.
calculated from measured calcium and magnesium
Water quality of the carbonate rock aquifer, southern Manitoba (GSC Open File 3725) Open Government Licence - Canada
Historical permit and construction activity by decade.
65% of dated wells are over 30 years old (pre-1995). Steel casing installed before 1995 can lose integrity over time. Any older well should get a casing inspection and a certified bacterial test before reliance.
Treatment
This page does not turn a hardness range or a well depth into an equipment total, a grain capacity, or a drilling price. Read the methodology, the filtration guide, and the products catalog.
Suggested system
Test kit
estimate, confirm with a lab testA test of your own well comes before any equipment. Test for coliform bacteria.
Water testingIron and manganese filter
estimate, confirm with a lab testAn iron filter is worth considering because wells in this place draw from LIMESTONE OR DOLOMITE. This follows the aquifer type. Iron and manganese were not used from a monitoring-well test.
Iron and manganese guideWater softener
estimate, confirm with a lab testSome wells nearby test above 120 mg/L, a softener may help, confirm with a lab test. 43 wells test above 180 mg/L.
Hard-water guideBecause water wells in RM of Armstrong average 123 ft into limestone or dolomite, contractors equipped with heavy rotary rigs and proper casing seals are recommended. Contact local drillers directly or request competitive bids.
Yard: Inwood, MB (19.5 km away)
Yard: Matlock, MB (38.7 km away)
Yard: Warren, MB (61 km away)
Yard: Selkirk, MB (64.4 km away)
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Quick answers about water wells in RM of Armstrong.
Among 1211 producing water wells with a recorded depth, the median is 123.0 ft (37.4904 m).
The most frequently recorded producing aquifer is LIMESTONE OR DOLOMITE, on 1069 of 1420 wells with a producing aquifer name.
Explore neighbouring hydrogeological formations and compare drilling depths