Sample report

A real example of the detailed AI-assisted report you receive after you unlock a location. The depth-to-groundwater estimate on the map is free; unlocking adds a location's drilling suitability, expected yield, suggested well depth and this full report.

EXAMPLE — a demonstration location, not your site 📄 Open the full sample (PDF) →

The PDF is the actual deliverable — with a satellite view of the location and your chosen branding. Below is the same report as text.

Charles Hill Production · 36.381301, -81.905823 · 2026-07-27 · (example client branding)

Preliminary Hydrogeological Assessment (AI-assisted)

— Location prospectivity for drilling a well

1. Basic location parameters

Coordinates	36.381301°, -81.905823°
Ground elevation	781 m above sea level
Estimated depth to water table	~151.3 m
Suggested drilling depth	~176.3 m
Distance to erosion base	468 m, river
Climate zone	Humid temperate

2. Location prospectivity and expected yield

The analyzed site is classified as a Favourable location within a karst terrain (pronounced morphology). In hydrogeology, karst environments consist of soluble carbonate rocks (limestones and dolomites) where water flows through interconnected fractures, joints and solution cavities. Because these structures generally have high secondary permeability, the location offers high prospectivity for well drilling. Where a borehole intersects an active water-bearing fracture or conduit, expected yields can exceed 4 l/s (240 l/min, 63.4 GPM, 14.4 m³/h).

Significant depth to water: the static water table lies deep (~151.3 m); reaching the recommended ~176.3 m requires heavy-duty rigs for deep bedrock penetration.
Subsurface heterogeneity: karst aquifers are irregular. If a borehole hits dense, massive rock between fracture paths, local yield can be much lower until a water-bearing void is struck.

3. Regional experience and local context

The coordinates are in northeastern Tennessee (Appalachian / Blue Ridge transition). Regional studies confirm that carbonate bedrock formations (such as the Shady Dolomite and associated limestones) act as prominent regional aquifers. Groundwater movement is strongly governed by tectonic fracturing, jointing and solution-enlarged bedding planes; yields are generally generous where boreholes strike open fracture networks, though production can vary with exact micro-location.

4. Final recommendation

Prospectivity: Favourable. The site shows strong potential for a reliable groundwater supply.
Drilling-depth strategy: do not stop at the first inflow (~151 m); continue to ~176.3 m to create a ~25 m water column and pump sump, allowing safe drawdown during dry seasons.
Contractor advice: engage a licensed driller experienced in deep rock/karst drilling who can perform air-lift yield testing to verify flow from struck fractures.

Automated informational desk study — not a professional geological or engineering service, not sealed by a licensed geologist/engineer, and not to be relied upon as such. Verify on site before drilling. Data: Copernicus WorldDEM-30, HydroRIVERS/HydroLAKES (© WWF/HydroSHEDS), GLiM (Hartmann & Moosdorf, 2012), Köppen-Geiger (Beck et al., 2018).

Try it for your own location → See pricing

The example above uses a demonstration location and example client branding. Reports are preliminary, model-based estimates from global datasets — not a substitute for a field hydrogeological survey. The decision to drill is yours.