Mtprinceton Henderson

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    Mt. Princeton Geothermal LLC

    Iceland Trade Mission

    Governors Energy Office

    and Colorado School of Mines

    7-8 January 2009

    Frederick B. Henderson III, Ph.D.

    Chief Scientist, Mt. Princeton Geothermal LLC

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    Mt. Princeton Geothermal LLC

    Mt. Princeton Geothermal ProjectFirst Geothermal Electricity in Colorado

    Stages

    I. Geology, Geophysics, Land LeasingPermitting - 2008II. Thermal Gradient Drilling

    Targeting -

    2009

    III. Deep Slim Hole Drilling & Pump Tests - 2009IV. Production & Injection Drilling and PlantDevelopment -

    2010

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    Baseline Geothermal Electricity

    Why Geothermal Energy Now?

    1. Onlybaseline alternative energy

    2. 24/7 on off3. No air or water pollution4. No storage requirement5. Upfront cost; no fuel supply required6. In many US Co-op back yards

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    Mt. Princeton

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    Study Area

    BuenaVista

    Salida

    San LuisValley

    TOPOGRAPHYUpper Arkansas River Basin

    Source: USGS SeamlessIn ArcGIS database

    N

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    Hot Springs

    Occur Along the RangeFront Fault

    Appear at Offset Zones

    Altered Quartz Monzonite

    Temperatures Vary

    40-82 C

    Unique Geochemistry

    N

    http://earth.google.com

    SawatchRang

    e

    Mosquito

    Rang

    e

    Hot Springs

    J. Dimick, 2007

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    Mt. Princeton Geothermal LLC

    Primary Target

    Deep (2,000 3,000) Fracture ReservoirProve sustainable flow of 15,000 gpm for 10MW production

    Deep target for

    1) hotter temperature ~ 250F

    2) Prove no surface water table impact

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    Mt. Princeton Hot Springs Well Log Study

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    2006LINE

    PROPOSED2009LINE

    2008LI

    NE

    BUENA VISTA

    GIS Database

    Based on Chaffee CountyGIS database; D. Reimer

    N

    1 Mile

    GravityPoints

    GravityPoints

    SP &Resistivity

    Mt Princeton H.S.

    2005 LINE

    A

    A

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    A A

    HEAT SOURCE

    LITHOLOGY STRUCTURE

    Fault with

    Inferred Motion

    Fractures

    HYDROTHERMALSYSTEM

    Mt Princeton

    Hot Springs

    Maxwell

    Park

    Trout Creek

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    Total field magnetic intensity vs distance

    along 2008 CSM seismic line

    MPHS

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    High

    Low

    (Dots only!)North Line Gravity

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    398000 398100 398200 398300 398400 398500 398600 398700 398800

    4287700

    4287800

    4287900

    4288000

    398000 398100 398200 398300 398400 398500 398600 398700 398800

    4287700

    4287800

    4287900

    4288000

    398000 398100 398200 398300 398400 398500 398600 398700 398800

    4287700

    4287800

    4287900

    4288000

    SP Response Contours and ArcGis

    Elevation and Roads MapUTM, northing

    UTM, easting

    mV

    Orientationof Fracture

    Silica Precipitation causes plugging.

    -30

    -25

    -20

    -15

    -10-5

    0

    5

    10

    15

    20

    25

    3035

    40

    45

    50

    55

    60

    65

    70

    75

    80

    85

    90

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    Fault Maps after: Cleaning up the lines

    Shallow

    Deep

    Very Deep

    Shear

    Drill Location

    Where to drill?

    Chalk

    Cliffs

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    Add SP & DC

    Fault Maps after: Self PotentialResistivity

    Shallow

    DeepVery Deep

    Shear

    North Rift

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    Mt. Princeton Geothermal LLC

    Stage II: Thermal Gradient Drilling

    Description and Goal Thermal gradients and Heat Flow State heat flow map AMAX 1973-5 heat flow drilling

    Plans for 2009

    Permitting

    Estimated Cost: $100,000 +

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    Baseline Geothermal Electricity

    Thermal Gradient (degrees/distance)

    X Rock Heat Conductivity= Heat Flow

    (in mW/m)

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    Mt. Princeton

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    AMAX WELLSAMAX WELLS

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    Mt. Princeton Geothermal LLC

    Permitting Process and Land Owner Response

    Proposed Thermal Gradient Drilling

    4-6 500

    holes (not wells) to augment AMAX holes

    Temperature gradient measured every 10

    Rock heat conductance X thermal gradient

    yields heat flow value

    High heat flow indicates deep heat source

    Completed heat flow anomaly helps define deep (3,000-

    5,000

    deep geothermal reservoir target

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    Mt. Princeton Geothermal LLC

    Permitting Process and Land Owner ResponseRon Cabe

    Two Meeting MPGLLC and DWR Mt. Princeton Project new to state

    new ground

    Project dubbed Non-Consumptive Pump & Dump

    While non consumptive, exploration (thermal gradient)drilling requires construction permit

    Later deep drilling needs construction and production

    permits

    Geohydrologic Studies required for non tributary permit

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    Mt. Princeton Geothermal LLC

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    Mt. Princeton Geothermal LLC

    Future Plans and New Technologies General Plan

    Fall 2008; Additional geophysicsas needed (CSM Proposal) $150,000+Thermal Gradient Drilling $150,000

    Spring Summer 2009: Initialdeep reservoir drilling $ 2-4 Million Fall 2009 2010: Additional production andre-injection drilling $5+ Million

    Surface plant development $30-40 Million

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    Mt. Princeton Geothermal LLC

    Geothermal Hot Spring Energy:The perfect exploration storm

    1. Exploration I: Hot springs + transmission lines2. Exploration II: Geology +thermal gradient ID

    3. Deep drilling + PUC allowed utilitydevelopment funding + Extended Tax Credits+ PPPAs4. New technology: UTC-type mid Theat systems5.

    New

    markets: Utility required profile

    standards 20% alternative energy by 2020

    11.5 years

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    Baseline Geothermal Electricity

    Shallow Temperature Survey (STS)

    Mt. Princeton Geothermal LLC is workingwith GEO, CSM and CGS to develop a

    STS system in the Mt. Princeton-ChaffeeCounty area in order to do a state wide

    first cut of hot springs prospects for largethermal indication of producible deeptargets. Development costs $55,000

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    Mt. Princeton Geothermal LLC

    OPPORTUNITIES

    FOR INVESTMENT