CL South America Updated 2026-08-21

Chile Geothermal Screening

Central-case models place 185 °C within 5.5 km of the surface beneath the great majority of Chile, and 200 °C is reached as shallow as 0.84 km somewhere in the country.

Key Geothermal Metrics

Land Reaching 185°C by 5.5 km High Potential
89%

Primary baseline screening criterion

Shallowest Depth to 200°C Very Shallow
0.84 km

Minimum drill depth for high enthalpy

Peak Temperature at 5 km Depth Commercial EGS
268 °C

Maximum modeled temperature

Typical Geothermal Gradient Elevated
39 °C/km

Average to 5 km depth (15°C surface)

Grid Connectable Prospective Area Moderate Distance
61%

Hot territory within 50 km transmission

Stored Heat In-Place (3–7 km) 1 ZJ = 10²¹ Joules
1203.4 ZJ

Thermal volume in place (>80°C baseline)

Depth vs. Temperature Matrix (% Land Area)

Proportion of national territory exceeding target isotherm at specified depth

0.1° Inversion Grid
Isotherm 3.0 km 4.0 km 5.0 km 6.0 km 7.0 km 8.0 km
150°C 48% 86% 92% 94% 95% 96%
175°C 26% 64% 88% 92% 93% 94%
200°C 15% 28% 69% 88% 92% 93%
225°C 3% 12% 24% 59% 86% 91%
250°C 6% 15% 34% 75%

4-Stage Geothermal Resource & Infrastructure Funnel

Progressive screening from gross national territory down to grid-connected & populated prospective zones

1 Whole country
920 500 km² 100%
2 Reaches 185°C by 5.5 km
815 000 km² 89%
3 ...and within 50 km transmission
557 200 km² 61%
4 ...and within 100 km town
414 200 km² 45%

Geological Setting & Subsurface Parameters

Lithology, basement thickness, stress and thermal boundary constraints

Median Depth to 200°C Isotherm 4.6 km
Best 10th Percentile Depth to 200°C 2.42 km
Median Temperature at 5 km Depth 209 °C
Best 10th Percentile Temp at 5 km 244 °C
Median Sediment Thickness 0.23 km
Sediment / Hard-Rock Well Share 5%
Territory Under 1 km Sediment Cover 84%
Lithostatic Pressure at 5 km Depth 137 MPa
Moho Crustal Discontinuity Depth 33.8 km
Thermal Lithosphere Thickness 54.7 km
Curie Temperature Isotherm Depth 26.3 km
Model Temperature Spread Uncertainty (200°C) ±4.9 km

Transmission Grid & Demand Colocation

Infrastructure interconnectivity and urban power demand proximity

High-Voltage Transmission Network Length 30 884 km
Land Area Within 25 km of Grid 58%
Land Area Within 50 km of Grid 70%
Land Area Within 100 km of Grid 82%
Average Proximity to Nearest Substation / Line 21.61 km
Urban Centers (>10,000 Population) 65
Total Urban Population 12.9 M
Prospective Resource Colocated Near Demand (>1M Pop) 2%

Target Sensitivity & Deep EGS Upside

Sensitivity of prospective resource area to adjusted depth and temperature thresholds

150°C Baseline at 5.5 km nearly all
185°C Baseline at 7.5 km nearly all

Global Peer Benchmarking (vs. 278 Assessed Jurisdictions)

Relative ranking distribution of Chile across 11 standardized geothermal indicators

Chile Rank Global Peer Spread
Share of land meeting the headline target
89% Above average
P0 (Lowest) P50 (Median) P100 (Highest) • 80th percentile
Median depth to 200°C
4.6 km In the strongest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 82th percentile
Median temperature at 5 km
209.0 °C In the strongest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 84th percentile
Hottest temperature at 5 km
268.0 °C In the strongest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 86th percentile
Shallowest 200°C
0.84 km In the strongest tenth
P0 (Lowest) P50 (Median) P100 (Highest) • 96th percentile
Average gradient to 5 km
39.0 °C/km In the strongest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 82th percentile
Median sediment thickness
0.23 km Above average
P0 (Lowest) P50 (Median) P100 (Highest) • 75th percentile
Share of the well drilled in sediment
5% Above average
P0 (Lowest) P50 (Median) P100 (Highest) • 78th percentile
Distance from prospective ground to the grid
21.61 km In the weakest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 22th percentile
Stored heat per 1,000 km²
1.31 ZJ In the strongest quarter
P0 (Lowest) P50 (Median) P100 (Highest) • 85th percentile
Lithosphere thickness
54.7 km In the strongest tenth
P0 (Lowest) P50 (Median) P100 (Highest) • 92th percentile
Asset-Level 3D Simulation Available

Need Interactive 3D Spatial Inversion for Chile?

High-resolution 3D temperature cubes, localized Curie depth inversions, fault network stress tensors, and drilling capex curves for Chile are accessible through our Premium & Enterprise subscription tiers.

Direct Founder Contact: founders@geothermalradar.com

Analytical Geothermal Assessment & Discussion: Chile

Subsurface thermal interpretation, model uncertainty, infrastructure colocation, and resource quality analysis

Resource Overview & Thermal Base

Across Chile, the great majority of the land area reaches 185 °C within 5.5 km of the surface under central assumptions. Under optimistic assumptions that rises to nearly all of the country, while ground that reaches the target even on conservative assumptions covers a small share. The typical location reaches 200 °C at 4.6 km; across the best tenth of the country it is 2.42 km or shallower.

Uncertainty & Model Spread

The resource is poorly constrained here: the optimistic and conservative depth estimates for 200 °C differ by 4.9 km at the typical location. The case for any single site therefore depends on which thermal model applies locally, which is the question a screening study exists to answer and is not answerable from published maps alone.

Infrastructure & Grid Colocation

On infrastructure, a clear majority of the country lies within 50 km of existing transmission and around half within 100 km of a town of 10,000 or more. Prospective ground sits a median 21.61 km from the nearest line. Combining resource and access, a clear majority of the country is both prospective under central assumptions and within reach of the grid.

Sedimentary Cover & Basement Setting

Sedimentary cover is very thin across most of the country, a median 0.23 km, which is 5% of the way to 200 °C. That sets how much of each well is drilled through soft rock before reaching basement, and with it much of the cost. Beneath it the crust runs to 33.8 km and the lithosphere to 54.7 km.

Stored Heat Volume (3-7 km)

Taken as a whole, the rock between 3-7 km beneath Chile holds 1203.4 ZJ of heat above a reference of 80 °C, equivalent to roughly 2,000 years of total world primary energy consumption. That is stored heat in the ground, not recoverable energy: what can actually be produced is a small fraction of it and depends on the engineering that follows this screening.

Peer Benchmarking (237 Global Areas)

Against the 237 areas assessed so far, Chile sits above average for share of land meeting the headline target, and in the weakest quarter for how close its prospective ground lies to existing transmission.

Drilling Depth & Target Sensitivity

Accepting a deeper well changes the picture: at 7.5 km, nearly all of the country reaches 185 °C under central assumptions. Relaxing the temperature requirement instead, to 150 °C at 5.5 km, brings in nearly all of the country.

Screening Methodology, Parameters & Limitations

This screening assessment for Chile is generated from Geothermal Radar Data Pack 22 July 2026 utilizing global 0.1° hex-grid thermal inversion across 2 818 model cells (land area: 920 544 km²). Baseline prospective criterion is defined as reaching 80°C at or above 5.5 km depth with surface temperature normalized to 15°C.

  • Screening estimates represent regional-scale heat in place and do not replace localized 3D seismic or exploratory drilling.
  • Model uncertainties expand in regions with sparse deep boreholes and complex thrust fault kinematics.
  • Grid proximity indicators reflect line-of-sight distance to high-voltage transmission and do not account for local substation thermal capacity.
Need Detailed Asset-Level Due Diligence?

Access 3D temperature grids, drilling cost curves, and micro-siting GIS layers.

Request Full Technical Dossier