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Fossil Water⚡ Fossil Water VerifiedSilver Data

Snake River Plain Deep Basalt Fossil Aquifer

Minidoka, Idaho, USA

Deep basalt aquifer in the Eastern Snake River Plain. While the shallow aquifer receives modern recharge, deep confined zones contain fossil water from volcanic and Pleistocene origins. One of the most productive aquifer systems in the western US.

83Grade A
High Value
Private
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Overview

Deep basalt aquifer in the Eastern Snake River Plain. While the shallow aquifer receives modern recharge, deep confined zones contain fossil water from volcanic and Pleistocene origins. One of the most productive aquifer systems in the western US.

Additional Notes

Idaho Department of Water Resources Eastern Snake Plain Aquifer Model area. Deep zones show pre-modern isotopic signatures.

Water Source Data

Asset TypeFossil Water
Flow Rate2.0k GPM
Seasonal FlowNo (perennial)
Depth800 ft

Water Intelligence Score Breakdown

Total: 83/100
Flow RateGeologicalLegal RightsSustainabilityRarity
Flow Rate
Yield & consistency
25/25
Geological
Formation quality
15/20
Legal Rights
Rights clarity
18/20
Sustainability
Long-term viability
10/20
Rarity
Scarcity premium
15/15

Risk Assessment

Overall: High(51/100)
Dry-up Risk
High
27/40

Source depletion probability

LowCritical
Legal Risk
Medium
16/35

Rights & regulatory exposure

LowCritical
Environmental
Medium
8/25

Contamination & ecosystem risk

LowCritical

Geological Intelligence

Formation & aquifer context
Rock Type
Igneous
Igneous and metamorphic rock

Dense, low primary porosity — yields via fractures

Aquifer Type
Fossil
fossil

Ancient water, no modern recharge — non-renewable on human timescales

Formation
Snake River Basalt
Basin
Elevation
Region

Land Details

Private
Acreage
Asking Price
Not listed
Buildable
Unknown
Zoning
Parcel ID

Water Rights

Unverified

Prior Appropriation

First in time, first in right

Rights are established by historical beneficial use. Senior rights holders receive full allocation before junior holders, regardless of land ownership.

  • Seniority date determines priority order
  • Requires continuous beneficial use
  • Can be severed from land and transferred
  • "Use it or lose it" — abandonment risk
Common in western US states (CO, MT, WY, ID, NV, UT, AZ, NM, OR, WA, CA)• Asset location: Idaho

Disclaimer: Water rights information is provided for research and informational purposes only and does not constitute legal advice. Rights status, seniority, transferability, and enforceability vary by jurisdiction and change over time. Always consult a licensed water rights attorney and verify status with the relevant state water resources agency before any acquisition or use decision.

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Location

Latitude42.73
Longitude-113.64
State/ProvinceIdaho
CountyMinidoka
CountryUSA
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Data Sources & Attribution

Updated Apr 5, 2026
Primary Source
hi3_fossil_water_research

Data is sourced from public and authoritative providers. Hi3 Water aggregates, normalizes, and scores records but does not assert ownership of underlying source data. Always verify critical details with the primary source before any decision.

Data Quality

Silver Quality
Gold = Field verified + lab tested
Silver = Reported + partial verification
Bronze = User reported
Unverified = Pending review