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Geothermal Exploration Demo

Map Geothermal Systems from the Surface

This simulation shows how PWI's passive sensor network progressively reveals a geothermal system — from initial heat anomaly detection through full characterization of the salt dome, cap rock, and hydrothermal conduit at depth.

Based on real PWI geothermal survey
Stage: Baseline Survey(Month 0)
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Baseline SurveyHeat Anomaly DetectedDome MappedConduit ResolvedBrine IdentifiedFull Characterization

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Temp. Gradient

35 °C/km

Dome Depth

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Conduit Width

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Vs Cap Rock

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Progressive Discovery Timeline

1

Deploy & Listen

33 sensors deployed in a ring around the hot springs area. Within weeks, passive data accumulates and the first subsurface anomalies emerge.

2

Map the Structure

The salt dome footprint (3.3 km) and cap rock (839m) are resolved. Seismic interferometry confirms a velocity spike at the cap rock boundary.

3

Characterize the System

The hydrothermal conduit is located and sized. Brine pathways from dome to surface are traced. Full geothermal model delivered.

What You're Seeing

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Salt Dome & Cap Rock

The beige dome structure is a salt diapir extending to ~1,165m depth. The gray shell at 839m is the cap rock — confirmed by a seismic velocity spike of 1,534 m/s.

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Geothermal Conduit

The orange vertical cylinder is a hydrothermal conduit (598–781m depth, ~183m wide) channeling hot brine from depth to the surface hot springs.

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Temperature Gradient

The colored points show subsurface temperature estimates derived from sensor data. The gradient increases from 35 to 102 °C/km as more data is collected and the thermal structure is resolved.

Why Passive Geothermal Exploration?

Traditional Methods

  • • Seismic surveys cost $500K+ and take months
  • • Drilling exploratory wells: $1M+ per hole, months of permitting
  • • Magnetotellurics gives resolution at 100s of meters
  • • Point measurements miss spatial patterns

PWI Geothermal Survey

  • • Deploy 33 sensors in 2 days for a fraction of the cost
  • • Continuous data — structure resolves progressively
  • • 3D dome, cap rock, and conduit mapped from surface
  • • Seismic interferometry confirms velocity structure
  • • No active source, no permitting delays

Explore Your Geothermal Resource

From hot springs prospecting to reservoir characterization — we deliver 3D subsurface intelligence from passive sensors.