HomeMy WebLinkAbout1.20 Legal Water SupplyCORONA
WATER LAW
Craig V. Corona, Esq.
1018 Lauren Lane
Basalt, CO 81621
(970) 948-6523
cc@craigcoronalaw.com
February 23, 2022
Glenn Hartmann, Senior Planner
Garfield County Community Development
108 8th Street
Glenwood Springs, CO 81601
RE: Spring Valley Ranch PUD Legal Water Supply
Dear Glenn,
This letter is on behalf of Spring Valley Holdings, LLC regarding the legal water supply
available to Phase 2 of the Spring Valley Ranch PUD. In addition, this letter provides responses
to address conditions of approval stated in prior Garfield County approvals for the PUD.
In sum, Spring Valley Holdings owns water rights and augmentation plans that provide a
legally adequate water supply for the entire PUD, including Phase 2. The Phase 2 water supply
will be provided by two existing permitted wells located on the Spring Valley Ranch property, and
by surface water diverted pursuant to Spring Valley Holdings’ senior irrigation water rights.
Analysis of the physical supply available to Phase 2 is provided by Roaring Fork Engineering in a
separate memo.
I.Phase 2 Legal Water Supply
A. Summary.
Spring Valley Holdings owns water court decrees for changes of water rights and plans for
augmentationauthorizinguse of water sufficient for the entire Spring Valley Ranch PUD including
residential and commercial uses and irrigation of golf course, open space landscaping, and
agricultural open space, as shown on the project plans. A list of the decrees, well permits, and
structures available to provide water service to the PUD is included as Exhibit A and available via
this link, [https://bit.ly/3uXo2BS]. Spring Valley Holdings also holds Basalt Water Conservancy
District water allotment contracts by which the Basalt District provides augmentation water to
offset out-of-priority depletions from the development. Copies of these contracts and the
assignments of the contracts to Spring Valley Holdings are attached as Exhibit B and available
via this link, [https://bit.ly/357H11B].
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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B. Senior Irrigation Rights.
Spring Valley Holdings owns all of the senior ditch water rights from Landis Creek,
totaling 12 cfs with priority dates in the 1880’s. Under these rights, all the water available in Landis
Creek has historically been diverted to irrigate 300 acres on Spring Valley Ranch. The water rights
include the Kendall and Stricklett Ditch, Forker and Gibson Ditch, Landis Ditch Nos. 1 and 2,
O.K. Ditch, and Frank Chapman Ditch. These water rights are all diverted at the same consolidated
point of diversion per the decree in Case No. 81CW193 (Exhibit C;[https://bit.ly/3uSH1O2]).
C. Wells and Springs.
The domestic in-house supply for the PUD will be provided by wells and springs. Spring
Valley Holdings has the right to use the following 33 wells and two springs:
Hopkins Spring Nos. 1 and 2
Spring Valley Well No. 1
Spring Valley Ranch Well Nos. 2-3
SVH Well Nos. 5-10
ASR Well Nos. 13-16
SVR Well Nos. 17-36
These structures were previously decreed individual conditional water rights in Case No.
98CW256 (Exhibit D; [https://bit.ly/3H0C87X]). During the Great Recession, Spring Valley
Holdings acknowledged that these structures could still be used pursuant to the augmentation plans
and change cases described below and elected not to undertake the expense ofpursuing water court
diligence findings for these rights, resulting in their cancellation.
Spring Valley Holdings recently filed an application in water court, Case No. 22CW3009, for
new conditional water rights for these structures to establish new priorities. A copy of the water
court application in Case No. 22CW3009 is attached as Exhibit E, [https://bit.ly/355jRJc].
D. Alternate Points of Diversion – Wells and Springs.
The wells and springs listed above operate as alternate points of diversion for the Basalt
Conduit water right under its 1957 priority through two water court decrees, Case Nos. 84CW212
and 98CW255, and Spring Valley Holdings’ Basalt District contracts. Case No. 84CW212
established nine wells and the springs as Basalt Conduit alternate points (Exhibit F,
[https://bit.ly/3gSEBGK]);and Case No. 98CW255 amended that decree to add 24 additional wells
as alternate points (Exhibit G, [https://bit.ly/3rWyK9K]).
Based on these decrees, when the springs and wells are out of priority, they operate under the
1957 Basalt Conduit priority. When the Basalt Conduit 1957 right is out of priority, the structures
operate under the augmentation plans described below.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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There are no other water rights in the Spring Valley Aquifer watershed with priorities senior
to the 1957 priority date of the Basalt Conduit water right. Thus, Spring Valley Holdings’ wells
and springs are only at risk of being out of priority vis-à-vis water rights on the Roaring Fork and
Colorado Rivers and those rights are protected from injury by releases under Spring Valley
Holdings’ Basalt District allotment contracts pursuant to the augmentation plans described below.
E. Augmentation Plans.
The augmentation plans decreed in Case Nos. 87CW155 and 98CW254 ensure that Spring
Valley Holdings can continue to provide water to the development even during calls by senior
water rights. Both augmentation plans use releases from Ruedi Reservoir or Green Mountain
Reservoir to address senior calls in an amount equal to out-of-priority depletions for in-house
domestic use, irrigation, and pond evaporation.
Case No. 87CW155.
The 87CW155 plan authorizes use for 2,642 residential units and 150 acres of irrigation. This
equates to 1,371 acre feet of diversions and 453.6 acre feet of depletions annually. A copy of the
87CW155 decree is attached as Exhibit H and available via this link [https://bit.ly/3rXxbZi]. This
plan only included the following structures:
Hopkins Spring Nos 1 and 2
Spring Valley Well No. 1
Spring Valley Ranch Well Nos. 2-3
SVH Well Nos. 5-10
Case No. 98CW254.
The 98CW254 plan supplements the 87CW155 plan allowing for additional irrigation and
adding new structures to supply the development’s water supply (See Exhibit I
[https://bit.ly/33ub977]). The decree adds ASR Well Nos. 13-16, SVR Well Nos. 17-36, ASR
Ditch No. 1, and treated effluent under the Spring Valley Sanitation District Pipeline right decreed
in Case No. 00CW21. The 98CW254 plan reduces the number of residential units to 577 (the
majority to be served by Spring Valley Sanitation District and 91 units to be on ISDS systems),
and increases irrigation from 150 acres to 420 acres.
The 98CW254 plan contemplates annual demand of 1,457 acre feet and depletions of 974
acre feet. Because much of the use will occur at times of free river when there is no senior call, the
augmentation requirement is only 420 acre feet. Importantly, the decree establishesthat the overall
uses at the development may be altered so long as the annual depletions do not exceed the
contemplated 974 acre feet. Thus, Spring Valley Holdings may modify the development plan
without having to modify or amend the existing water court decrees.
F. Treated Effluent – Spring Valley Sanitation District Pipeline.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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Spring Valley Holdings has the right to use treated effluent from Spring Valley Sanitation
District for golf course and open space irrigation. Spring Valley Holdings, Berkeley Family
Limited Partnership and Colorado Mountain College obtained a water right decree in Case No.
00CW21 for the Spring Valley Sanitation District Pipeline right to use treated effluent from the
wastewater treatment plant on their respective properties (See Exhibit J
[https://bit.ly/34TQYzY]).
In addition, by agreement, the Spring Valley Sanitation District must allow Spring Valley
Holdings to use the amount of treated effluent that corresponds to the amount of wastewater that
is generated within the Spring Valley Ranch PUD. A copy of this agreement is attached as Exhibit
K and available via this link [https://bit.ly/3LBuvZf]. This use is also augmented by the decree in
Case No. 98CW254. Using effluent would reduce demand for groundwater from the wells and
supplement aquifer recharge.
Depending on the feasibility of meeting regulatory requirements for using treated effluent, the
necessary infrastructure will be installed when there is sufficient effluent for irrigation to be
practical. If feasible in the future, Spring Valley Holdings intends to use treated effluent for
irrigation.
G. Reservoirs.
Spring Valley Holdings owns the water right for the Hopkins Reservoir for up to 119 acre
feet of storage. The reservoir has historically been used to control irrigation water for use on the
Spring Valley Ranch. Spring Valley Holdings has gone to great effort and expense to rehabilitate
the dam for the reservoir and has received approval from the Division of Water Resources for the
dam. Attached as Exhibit L [https://bit.ly/36rqqXz], is the Division of Water Resources’
Engineer’s Inspection Report from June 2021 which states that the reservoir may be filled to full
capacity. The reservoir will be used to supplement irrigation on the PUD.
In addition, Spring Valley Holding’s augmentation plans provide for three ponds to be built
on the property, ASR Reservoir Nos. 1-3, and augments a total of 24 acres of surface area
evaporation from those reservoirs. These reservoirs will be used to supplement irrigation and other
uses on the property. Spring Valley Holdings included claims for these three ponds for a total of
65 acre feet of storage in the recently filed 22CW3009 water court application.
H. Adequacy of Legal Water Supply.
Attached with this memo as Exhibit M [https://bit.ly/3HZ0mRb] is the analysis of Wright
Water Engineers from 2007 demonstrating that the water rights, plans for augmentation, and
change cases provide an adequate legal water supply for development of the entire PUD. The
report demonstrates that the legal water supply actually exceeds the demands for the 2007
development design. The development design has not changed since the time of the Wright Water
Engineers’ report.
As noted in the report, the projected annual water demand for the development is 717 acre
feet for potable use (in-house domestic and lawn irrigation) and 493 acre feet for non-potable use
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(golf course and open space irrigation and pond evaporation), for a total of 1,210 acre feet of
demand. The augmentation plan in Case No. 98CW254 authorizes diversions (i.e., demand) of up
to 1,457 acre feet which exceeds the contemplated demand.
The report also demonstrates that development depletions will be 141 acre feet for potable
uses and 404 acre feet for non-potable uses, a total of 545 acre feet. The 98CW254 plan authorizes
974 acre feet of depletions, much greater than what is required for the current PUD development
design. Based on the 2007 Wright Water Engineers’ report, the legal water supply for the entire
PUD is more than adequate and, therefore, for Phase 2, as well.
I. Phase 2 Development.
Phase 2 development will consist of 20 Cabin Lots, 26 Estate Lots, and 9 Ranch Lots, all
with single family residences. In addition, there are four Open Space Parcels, and one Light
Industrial Parcel. Water will be necessary to serve in-house domestic uses in fifty-five homes and
irrigation for residential lawn areas. No open space irrigation is planned at this time; however, this
may change as the developer provides landscaping along streets and public areas.
As detailed in the Wright Water Engineers’ 2007 report, Spring Valley Holdings’ water
rights, augmentation plans, and change cases are adequate to serve 192 Cabin Lots, 253 Estate and
Ranch Homes, 58 acres of lawn irrigation, and 120 EQRs for light industrial use. The 98CW254
augmentation plan authorizes 420 acres of open space irrigation. On that basis, Spring Valley
Holdings’ court-decreed plans for augmentation and changes of water rights, along with their
senior irrigation water rights provide a legally adequate water supply for the Phase 2 demands.
J. Phase 2 Supply.
Phase 2 will be supplied by two wells, ASR Well No. 16 and SVR Well No. 20. Both wells
were decreed as alternate points of diversion for the Basalt Conduit in Case No. 98CW255 and
both are augmented structures in Case No. 98CW254. ASR Well No. 16 is permitted to pump 100
gpm under Well Permit No. 86629F (Exhibit N, [https://bit.ly/3JCewby]). SVR Well No. 20 is
permitted to pump 300 gpm under Well Permit No. 86628F (Exhibit O,
[https://bit.ly/3gVSAM4]).
The permits for these wells allow use for 577 residential units, two 18-hole golf courses,
limited commercial development, and irrigation of 90 acres of lawns and gardens and 420 acres of
golf courses, open space, and agricultural areas. The well permits, therefore, authorize use of the
wells for the 55 homes, lawn irrigation, commercial use, and open space irrigation planned for
Phase 2.
K. Conclusion – Legal Water Supply.
Spring Valley Holdings owns water rights, court-decreed augmentation plans and change
cases, well permits, and water allotment contracts that provide an adequate legal water supply for
Phase 2 development. As noted in the 2007 Wright Water Engineers’ report, Spring Valley
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Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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Holdings’ water rights and water resources exceed the water requirements for the entire PUD,
including Phase 2.
II.Conditions of Approval.
Following are responses regarding the legal water supply related conditions of approval
contained in Resolution No. 2008-56 regarding Approval of a Preliminary Plan Application for
Spring Valley Ranch PUD recorded April 22, 2008 at Reception No. 747016, and Resolution No.
2010-38 regarding Approval for Spring Valley PUD recorded June 8, 2010 at Reception No.
786992. Each condition of approval is re-typed below in italics with the response following. The
numbers correspond to the numbering in the resolutions.
A. Resolution 2008-56 PUD Conditions of Approval, Reception No. 747016 (April 22,
2008).
20.0 Condition:With the exception of Lot P23 and OSR Parcel E, individual well
development shall be prohibited for new development.
Response: The Master Declaration of Covenants, Conditions and Restrictions for Spring
Valley Ranch P.U.D. recorded at Reception No. 793245, at paragraph 3.31, prohibit
development of individual wells except as set forth in the PUD Approval. A copy of the
CCR’s are included as Appendix K of the application.
21.0 Condition:The Applicant shall work with the water district providing potable
water service to the development to adopt a water usage rate structure that encourages
conservation.
Response: Spring Valley Holdings is committed to working with Landis Creek
Metropolitan District No. 1 to develop a rate structure that encourages conservation. The
Metro District is unable to develop a rate structure at this time since that will require the
District to undergo a rate study, first. The rate study will have to be based on the population
to be served, the overall uses of the water, and rates charged by other water suppliers in the
area at the time of service. Once the District has been able to undertake an appropriate rate
study, Spring Valley Holdings will work to have the District develop a structure that
encourages conservation.
22.0 Condition:Well water usage for agricultural and golf course purposes shall be
allowed to supplement surface water sources in the event of a shortage of surface water supplies.
Response: The water court decree issued in Case No. 98CW254 authorizes the use and
augmentation of well water to supplement surface water supplies for the entire 420 acres
of golf course, open space, and agricultural irrigation contemplated in the development
plan.
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Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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23.0 Condition:Valid well permits must be obtained for all of the wells included in the
water supply plan and copies submitted to the Planning Department prior to Final Plat approval.
Response: Spring Valley Holdings has valid production well permits for the wells that will
serve Phase 2, ASR Well No. 16 and SVR Well No. 20 (see Exhibit N,
[https://bit.ly/3JCewby]; and Exhibit O, [https://bit.ly/3gVSAM4]).
Spring Valley Holdings also holds valid production well permits for four other wells,
Spring Valley Well No. 1, Spring Valley Ranch Well Nos. 2-3, and SVR Well No. 17. See
Exhibit Q, [https://bit.ly/3sHFOpS].
B. Resolution 2010-38 PUD Conditions of Approval, Reception No. 786992 (June 8,
2010).
9.0 Condition:Future use of additional wells (Gamba wells) requires the development
of water rights and well permits if required by the appropriate state agency.
Response: There should not be need for more wells in addition to the 33 wells Spring
Valley Holdings currently has rights to develop, but, if there is, Spring Valley Holdings
will obtain the necessary water rights and well permits.
Spring Valley Holdings holds valid production well permits for the following six wells:
o Spring Valley Well No. 1 (Permit No. 86630-F)
o Spring Valley Ranch Well No. 2 (Permit No. 51363-F)
o Spring Valley Ranch Well No. 3 (Permit No. 86631-F)
o SVR Well No. 17 (Permit No. 86627-F)
o SVR Well No. 20 (Permit No. 86628-F)
o ASR Well No. 16 (Permit No. 86629-F)
See Exhibits N, O, Q.
Spring Valley Holdings’ consultantsestimatethatthesesixwells willprovidesufficient
physical supply for the entire PUD. For Phase 2, Spring Valley Holdings will use ASR
Well No. 16 and SVR Well No. 20. Based on the conclusions in the memo provided by
Roaring Fork Engineering, ASR Well No. 16 and SVR Well No. 20 produce sufficiently
to supply Phase 2. All six wells listed above operate pursuant to the plans for augmentation
and changes of water rights decreed by the water court in Case Nos. 84CW212, 87CW155,
98CW254, and 98CW255.
In addition to the six wells listed above, Spring Valley Holdings has the right to develop
and use 27 more wells to serve the PUD. If these additional wells are needed in the future,
Spring Valley Holdings has only to apply for well permits from the Division of Water
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Resources and, because the wells are fully augmented pursuant to water court decrees, the
Division of Water Resources must issue the permits for all PUD uses.
There is no indication at this time that Spring Valley Holdings’ 33 wells and 2 springs
will be inadequate to physically supply the PUD; however, if, somehow, that becomes the
case, Spring Valley Holdings will apply in water court to add additional wells to the
structures in their existing augmentation plans and change decrees or will apply to change
the locations or diversion amounts associated with the authorized structures and obtain the
necessary well permits.
10.0 Condition:All conditions of the Division of Water Resources shall be met. Those
conditions include but are not limited to:
1.The claimed water rights are dedicated to the project; and
Response: The Landis Creek Metropolitan District Nos. 1 and 2 Service Plan establishes
that Spring Valley Holdings must provide the PUD water rights to the Districts for water
supply. See Exhibit R [https://bit.ly/3uZQcwg]. At the appropriate time, Spring Valley
Holdings will convey the water rights necessary for Phase 2 to Landis Creek Metropolitan
District No. 2 which will be the rights to ASR Well No. 16, SVR Well No. 20, and the
portions of the decrees issued in Case Nos. 84CW212, 87CW155, 98CW254, and
98CW255, and the senior ditch irrigation rights, that are necessary to supply Phase 2 uses.
2.The plan for augmentation is operated according to decreed terms and conditions.
Response: Spring Valley Holdings is committed to operating the decreed plans for
augmentation, all other water rights decrees, and all well permits according to their terms
and conditions as they are legally required to do. Spring Valley Holdings will not put the
development at risk of having the Division of Water Resources curtail diversions to the
water supply system by operating the water supply system contrary to the court decreed
terms and conditions.
11.0 Condition:Available surface water supplies shall be used to their fullest extent to
provide the irrigation supply to the golf courses in order to minimize groundwater withdrawals.
Response: Phase 2 does not include the golf course so this condition is not directly
applicable to the current application. Nonetheless, the Landis Creek Metropolitan District
Service Plan establishes that the surface water rights historically used to irrigate the
property (i.e., the ditch rights) must be used to irrigate the golf course. (Exhibit R, III.C.3
[https://bit.ly/3uZQcwg]). Spring Valley Holdings commits to using the surface water
rights as the primary source for golf course irrigation which is in the developer’s best
interest as surface water supplies will be less expensive to use than groundwater supplies.
Condition 11.0 (cont.):A groundwater monitoring plan shall be developed to monitor
future water levels near the Spring Valley Ranch wells. The monitoring plan shall include water
level measurements in the production wells and other wells at the PUD that can be used as
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Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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monitoring holes. The monitoring plan shall include measurements made with enough frequency
to observe seasonal groundwater fluctuations and long term groundwater trends. Results of the
monitoring program shall be available to the public.
Response: Spring Valley Holdings provides a groundwater monitoring plan developed by
Zancanella & Associates included as Exhibit S and available via this link
[https://bit.ly/3556YPF]. Based on this plan, three existing wells will be used for
monitoring, ASR Well No. 15, SVH Well No. 6, and Monitoring / Observation Well No.
1. These locations were selected to monitor the aquifer on the upper bench and in the valley
floor, both near production wells and at a distance. Monitoring / Observation Well No. 1
is at least 2,000 feet from any production well location.
These monitoring wells will be outfitted with battery-operated transducers to take daily
water-level measurements. Baseline monitoring will start before development and before
production wells begin pumping. All production wells will also be monitored as they are
brought into production. For Phase 2, ASR Well No. 16 and SVR Well No. 20 will both be
monitored. All data will be stored with Landis Creek Metropolitan District No. 2 and will
be publicly available.
11.1 Condition:There will be an additional monitoring well developed or identified that is at
least 2000 feet from the production wells. Either a new well or an off-site well meeting those
criteria could meet the criteria. All of the monitoring reports will be available to the public.
Response: Well 03-2 identified in the groundwater monitoring plan is greater than 2,000
feet from ASR Well No. 16 and SVR Well No. 20, which are the wells that will be used
for Phase 2. As noted above and in the groundwater monitoring plan, all monitoring data
will be available to the public.
C. Conclusion.
Based on the responses above and the documents provided, Spring Valley Holdings has
complied with all the conditions of approval contained in the resolutions approving the PUD.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
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LIST OF EXHIBITS
Exhibit A List of Water Court Decrees [https://bit.ly/3uXo2BS]
Exhibit B Basalt Water Conservancy District Water Allotment Contracts and Assignments
[https://bit.ly/357H11B]
Exhibit C Water Court Decree Case No. 81CW193 [https://bit.ly/3uSH1O2]
Exhibit D Water Court Decree Case No. 98CW256 [https://bit.ly/3H0C87X]
Exhibit E Water Court Application Case No. 22CW3009 [https://bit.ly/355jRJc]
Exhibit F Water Court Decree Case No. 84CW212 [https://bit.ly/3gSEBGK]
Exhibit G Water Court Decree Case No. 98CW255 [https://bit.ly/3rWyK9K]
Exhibit H Water Court Decree Case No. 87CW155 [https://bit.ly/3rXxbZi]
Exhibit I Water Court Decree Case No.98CW254 [https://bit.ly/33ub977]
Exhibit J Water Court Decree Case No. 00CW21 [https://bit.ly/34TQYzY]
Exhibit K Pre-Inclusion Agreement with Spring Valley Sanitation District
[https://bit.ly/3LBuvZf]
Exhibit L Division of Water Resources Dam Inspection Report [https://bit.ly/36rqqXz]
Exhibit M 2007 Water Supply Report Wright Water Engineers [https://bit.ly/3HZ0mRb]
Exhibit N Well Permit No. 86629-F ASR Well No. 16 [https://bit.ly/3JCewby]
Exhibit O Well Permit No. 86628-F SVR Well No. 20 [https://bit.ly/3gVSAM4]
Exhibit P [Purposely Omitted]
Exhibit Q Well Permits Spring Valley Well No. 1, Spring Valley Ranch Well Nos. 2-3, SVR
Well No. 20 [https://bit.ly/3sHFOpS]
Exhibit R Landis Creek Metropolitan Districts Service Plan [https://bit.ly/3uZQcwg]
Exhibit S Zancanella & Associates Groundwater Monitoring Plan [https://bit.ly/3556YPF]
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EXHIBIT A
List of Water Court Decrees
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APPENDIX 8
EXHIBIT A
Spring Valley Ranch PUD
Water Rights Decrees and
Proceedings
1.Kendall & Stricklett Ditch, decreed in C.A. 304 for 0.1 c.f.s. on April 18, 1890,
with a priority date of May 15, 1882.
2.Landis No. 1 Ditch, decreed in C.A. 304 for 1.6 c.f.s. on April 18, 1890, with a
priority date of June 1, 1882.
3.Landis No. 2 Ditch, decreed in C.A. 304 for 1.6 c.f.s on April 18, 1890, with a
priority date of June 1, 1882.
4.O.K. Ditch, decreed in C.A. 304 for 1.2 c.f.s on April 18, 1890, with a priority date
of May 1, 1884.
5.Forker & Gibson Ditch, decreed in C.A. 304 for 5.5 c.f.s on April 18, 1890, with a
priority date of April 30, 1885.
6.Frank Chapman Ditch, decreed in C.A. 304 for 2 c.f.s on April 18, 1890, with a
priority date of April 25, 1886.
7.Case No. 81CW193, October 4, 1982, which decreed a change in point of diversion
for the Kendall & Stricklett Ditch, Landis Ditches 1 & 2, O.K. Ditch, Forker &
Gibson Ditch, and Frank Chapman Ditch to a consolidated point of diversion on
Landis Creek, for the irrigation of up to 300 acres.
8.Hopkins Reservoir, decreed for 119.6 acre-feet on April 30, 1910, with a priority
date of May 18, 1909.
9.Hopkins Spring No. 1, decreed in W-3121 for 0.0614 c.f.s. on May 19, 1978, with a
priority date of June 30, 1900.
10.Hopkins Spring No. 2, decreed in W-3122 for 0.0924 c.f.s. on November 7, 1977,
with a priority date of June 30, 1900.
11.Spring Valley Well No. 1, Application pending, Case No. 22CW3009; Exhibit E
[https://bit.ly/355jRJc] for 300 gpm conditional for all PUD uses.
12.Spring Valley Ranch Well No. 2, Application pending, Case No. 22CW3009
Exhibit E [link] for 300 gpm conditional for all PUD uses.
13.Spring Valley Ranch Well No. 3, Application pending, Case No. 22CW3009
Exhibit E [https://bit.ly/355jRJc] for 300 gpm, conditional, for all PUD uses.
14.SVH Well No. 5, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
15.SVH Well No. 6, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
16.SVH Well No. 7, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
17.SVH Well No. 8, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
18.SVH Well No. 9, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
19.SVH Well No. 10, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 100 gpm conditional for all PUD uses.
13
20.Case No. 84CW212, which decreed alternate points of diversion for 6.0 c.f.s. of the
Basalt Conduit water right as decreed in C.A. 4613 on June 20, 1958, for 450 c.f.s.
with a priority date of July 29, 1957. The alternate points of diversion are at the
Hopkins Spring Nos. 1 and 2, Spring Valley Well No. 1, Spring Valley Ranch Well
Nos. 2 and 3, and SVH Well Nos. 5-10. Exhibit F; [https://bit.ly/3gSEBGK]
21.Case No. 87CW155, July 7, 1989, which decreed a plan for augmentation for water
service for up to 2642 residential units, and 150 acres of irrigation, for a total annual
water requirement of 1371 acre-feet and a total annual consumptive use of 453.6 acre-
feet. This augmentation plan contemplates water service to the Spring Valley Ranch
from the following water rights: Hopkins Spring No. 1, Hopkins Spring No. 2, Spring
Valley Well No. 1, Spring Valley Ranch Well Nos. 2-3, SVH Well Nos. 5-10. Exhibit
H[https://bit.ly/3rXxbZi].
22.Case No. 98CW255, Water Division No. 5, which amended the decree in Case No.
84CW212 to include the ASR Well No. 13-16, together with up to 20 Additional
Wells that could be developed on the Spring Valley Ranch PUD, as additional
alternate points of diversion for the Basalt Conduit water right. Exhibit G
[https://bit.ly/3rWyK9K].
23.ASR Ditch No. 1, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 1 cfs for all PUD uses.
24.ASR Reservoir Nos. 1-3, Application pending, Case No. 22CW3009 Exhibit E
[https://bit.ly/355jRJc] for 15, 30 and 20 acre-feet respectively for all PUD uses.
25.Case No. 98CW254, December 9, 2002, which decreed a plan for augmentation for
water service for up to 695 EQR, 24 acres of pond surface area, and 420 acres of
irrigation in conjunction with the augmentation plan in 87CW155, for a total annual
water requirement of 1457 acre-feet and a total annual consumptive use of 974 acre-
feet, up to a total augmentation requirement of 420 acre-feet per year. This
augmentation plan contemplates water service to the Spring Valley Ranch from the
following structures: Hopkins Spring No. 1, Hopkins Spring No. 2, Spring Valley
Well No. 1, Spring Valley Ranch Well Nos. 2-3, SVH Well Nos. 5-10, ASR Well
Nos. 13-16, and SVR Well Nos. 17-36 to be located anywhere on the Spring Valley
Ranch PUD.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 12 of 28
EXHIBIT B
Basalt Water Conservancy District Water
Allotment Contracts and Assignments
"11&/%*96
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Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 13 of 28
EXHIBIT C
Water Court Decree Case No. 81CW193
"11&/%*96
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Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 14 of 28
EXHIBIT D
Water Court Decree Case No. 98CW256
"11&/%*96
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Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 15 of 28
EXHIBIT E
Water Court Application Case No.
22CW3009
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FILING ID: DA351F34438BE
CASE NUMBER: 2022CW3009
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Spring Valley Well No. 1
SVH Well No. 6
Spring Valley
Ranch Well No. 3
Spring Valley Ranch Well No. 2
SVH Well No. 7
SVH Well No. 5
SVR Well No. 17
ASR Reservoir No. 1
ASR Ditch No. 1
ASR Well No. 16
ASR Well No. 13 ASR Well No. 14
SVH Well No. 9
SVH Well No. 10
SVR Well No. 20
ASR Well No. 15
Hopkins Landis Creek
Feeder Ditch
Hopkins Reservoir and
First Enlargement
Landis Creek Pump Station
ASR Reservoir No. 2
ASR Reservoir No. 3
SVH Well No. 8
DATE FILED: January 31, 2022 11:37 PM
FILING ID: DA351F34438BE
CASE NUMBER: 2022CW3009
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DATE FILED: January 31, 2022 11:37 PM
FILING ID: DA351F34438BE
CASE NUMBER: 2022CW3009
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 16 of 28
EXHIBIT F
Water Court Decree Case No. 84CW212
"11&/%*96
&9)*#*5'
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 17 of 28
EXHIBIT G
Water Court Decree Case No. 98CW255
"11&/%*96
&9)*#*5(
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 18 of 28
EXHIBIT H
Water Court Decree Case No. 87CW155
"11&/%*96
&9)*#*5)
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 19 of 28
EXHIBIT I
Water Court Decree Case No. 98CW254
"11&/%*96
&9)*#*5*
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 20 of 28
EXHIBIT J
Water Court Decree Case No. 00CW21
"11&/%*96
&9)*#*5+
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 21 of 28
EXHIBIT K
Pre-Inclusion Agreement with Spring
Valley Sanitation District
"11&/%*96
&9)*#*5,
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 22 of 28
EXHIBIT L
Division of Water Resources
Dam Inspection Report
Dam Safety Branch
202 Center Drive, Glenwood Springs, CO 81601 P 303.518.1829 https://dwr.colorado.gov
Jared S. Polis, Governor | Dan Gibbs, DNR Executive Director | Kevin G. Rein, Director/State Engineer
June 22, 2021
SUBJECT:2021 Engineer’s Inspection Report
Dear Mr. Van Ardenne,
On June 21, 2021, representatives from our dam safety office completed inspection of
Hopkins Dam in accordance with Section 37-87-107 of the Colorado Revised Statutes; which
assigns to the State Engineer’s Office (SEO) responsibility for determining safe storage levels
for all reservoirs in the State of Colorado. I would like to thank Mr. Matt Weisbrod of
Zancanella & Associates for taking time to participate in the 2021 inspection.
Enclosed is a copy of the Engineer’s Inspection Report (EIR) and field photographs of the
referenced dam for your files. Please sign the signature block on page 4 of the EIR to
acknowledge your receipt of the report and return a copy to our office via electronic or regular
mail. If you have any questions regarding this EIR or require assistance with dam safety related
issues, please feel free to contact me on my cell phone at (303) 518-1829.
Sincerely,
Korey J. Kadrmas, P.E.,
Division 5 Dam Safety Engineer
Enc. a/s
ec: Bill McCormick, Chief, Dam Safety Branch
Heather Ramsey, Water Commissioner
James Heath, Division Engineer, Division 5
Matt Weisbrod, Zancanella & Associates; mweisbrod@za-engineering.com
Doreen Herriott, Spring Valley Holdings; daherriott@gmail.com
Mr. Martin Van Ardenne
Seligman Group
500 Montgomery St., 40th Floor
San Francisco, California 94111
via email: mvanardenne@seligmangroup.com
When replying, please refer to:
HOPKINS DAM, DAMID 380113
Water Division 5, Water District 38
Sincerely,
Korey J. Kadrmas, P.E.,
Division 5 Dam Safety Engin
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CONDITIONS
OBSERVED
WATER LEVEL:
GROUND MOISTURE CONDITION:
BELOW DAM CREST FT. FT. GAGE ROD READING
DRY WET SNOWCOVER OTHER
',5(&7,2160$5.$1;)25&21',7,216)281'$1'81'(5/,1(:25'67+$7$33/<
DAM NAME:HOPKINS
DAM ID:380113
&855(175(675,&7,21121(
DAM HEIGHT(FT):25.0
DAM LENGTH(FT):700.0
CRESTWIDTH(FT):15.0
CLASS:Significant hazard
EAP:11/10/2019
DATE OF INSPECTION:6/21/2021
DIV:5 WD:38
15060S0880W
0DWW:HLVEURG +HDWKHU5DPVH\ .RUH\.DGUPDV
SPILLWAY WIDTH(FT):20.0
FREEBOARD (FT):6.0
T:
OWNER:6(/,*0$1*5283
ADDRESS:0217*20(5<67CONTACT NAME:'25((1+(55,277
CONTACT PHONE:;
YRCompl:2020
S:R: COUNTY:GARFIELD
CRESTELEV(FT):9001.0
SPILLWAY CAPACITY(CFS):700.0
DRAINAGE AREA (AC.):350.0
NORMAL STORAGE (AF):113.0
SURFACE AREA(AC):12.0
OUTLET INSPECTED:8/27/2020
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3DJHRI
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
202 Center Drive, Glenwood Springs, CO 81601 P 303.518.1829 https://dwr.colorado.gov
Jared S. Polis, Governor | Dan Gibbs, DNR Executive Director | Kevin G. Rein, Director/State Engineer
PHOTOGRAPHS
Upstream Slope
Photo 1. View from left abutment of the
upstream slope. Reservoir filled to
about stage 4.5 feet and most of the
upstream slope was exposed all season.
Upstream Slope
Photo 2. View looking right along the
upstream slope from near Sta. 3+00.
Slope is uniform with well graded riprap
rock that is angular and interlocked. No
areas of exposed riprap bedding.
Upstream Slope
Photo 3. View of shoring wall pile
installation from the spillway stilling
basin. Precast concrete shoring wall
panels to be installed from downstream
end up as the CMP is being installed.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
2 of 9
PHOTOGRAPHS
Upstream Slope
Photo 4. View from the right abutment
of the upstream slope. Large riprap and
boulders placed along the right
abutment to protect against possible
erosion.
CREST
Photo 5. View of the dam crest from
the right abutment with the Landis
Ditch diversion in the foreground.
CREST
Photo 6. Dam crest is in good condition
with positive drainage toward the
reservoir. Gravel surfacing on road is
uniform with no observed rutting.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
3 of 9
PHOTOGRAPHS
Downstream Slope
Photo 7. Looking east along the
downstream toe of the dam. Toe area
graded to avoid surface water along the
toe area.
Downstream Slope
Photo 8. Looking west (right) along the
downstream slope from about Sta. 2+00.
Slope is uniform with native grass
establishment in process. Engineer
noted that this item is under 2 year
warranty and likely will take 2 seasons
to establish native grasses.
Downstream Slope
Photo 9. A low lying area at the
downstream toe along the spillway
channel was observed to have a thicker
establishment of grasses. Based on low
reservoir levels, grasses in this area
likely thicker since fill had a high
quantity of clay and this area was
graded as a bowl feature and likely
retains water lower than other portion
of the reseeded areas.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
4 of 9
PHOTOGRAPHS
Downstream Slope
Photo 10. Looking east along the
downstream slope from the right
abutment. Slope is uniform and stable.
Seepage
Photo 11. No signs of seepage or drain
activity was observed on the dam.
Drains were dry during the inspection
and Engineer has not observed any drain
discharge to date.
Outlet
Photo 12. Intake structure on the
outlet was submerged. Trashrack
observed in place on the intake
structure.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
5 of 9
PHOTOGRAPHS
Outlet
Photo 13. View of the outlet manual
operator at the dam crest. Engineer
successfully exercised the gate.
Outlet
Photo 14. Looking downstream at the
outlet outfall structure currently in
operation.
Outlet
Photo 15. Looking upstream at the
outfall structure from the discharge
channel. Riprap downstream of the
structure was mounded at the structure
outfall resulting in deflection of the
flow with higher rates along the sides of
the riprap apron. Engineer noted that a
swale (i.e., belly) will be graded in the
riprap from the outfall to improve
conveying of flows downstream of the
structure.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
6 of 9
PHOTOGRAPHS
Outlet
Photo 16. Profile view of the outlet
discharge. Note the deflected water
spilling along the riprap apron and
backwater pool to the right side of the
outfall channel.
Outlet
Photo 17. View of the outlet outfall
pool area prior to operation of the
outlet. Minor bank erosion noted along
the right side of the backwater pool
area..
Outlet
Photo 18. Looking downstream at the
outlet discharge channel from the
riprap apron below the outfall
structure. Apron consists of gap graded
riprap with infilled rock to stabilize the
rock fill.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
7 of 9
PHOTOGRAPHS
Spillway
Photo 19. Looking west along the dam
axis with the emergency spillway
control structure in the foreground.
The concrete control sill was in good
condition with no observed cracks.
Spillway
Photo 20. Looking downstream at the
spillway discharge channel from the left
abutment area. Spillway control
structure (i.e., buried cutoff sill) in the
foreground.
Spillway
Photo 21. View along the lower spillway
cutoff wall Concrete in good condition
with no observed cracks.
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
8 of 9
PHOTOGRAPHS
Spillway
Photo 22. Looking upstream at the
spillway discharge channel from end of
riprap lining about 200 feet downstream
of the control sill.
Monitoring
Photo 23. Typical view of the reservoir
staff gauge/concrete grade beam with
1-foot elevation steel plates. Maximum
reservoir level this season appears to be
about El. 8980.5 (~stage 4.5 feet).
Monitoring
Photo 24. View of typical piezometer
with lockable steel casing. Engineer
measures piezometer levels during each
ENGINEER’S INSPECTION REPORT DATE: 06.21.2021
DAM NAME: HOPKINS DAM KJK DAMID: 380113, C-0090C
9 of 9
PHOTOGRAPHS
Monitoring
Photo 25. View of piezometer with
locking well cap (on left) and survey
monument with yellow marker lathe (on
right). Location shown near mid-
downstream slope along the maximum
section.
Diversion Structure
Photo 26. Intake end of the diversion
culvert on the Landis Ditch (location
along the dam axis just outside of the
dam embankment footprint.
Diversion Structure
Photo 27. Outfall end of the diversion
ditch culvert location about 50 feet
from the upstream toe of the dam at
the right abutment.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 23 of 28
EXHIBIT M
2007 Water Supply Report
Wright Water Engineers
"11&/%*96
&9)*#*5.
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 24 of 28
EXHIBIT N
Well Permit No. 86629-F
ASR Well No. 16
"11&/%*96&9)*#*5/
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 25 of 28
EXHIBIT O
Well Permit No. 86628-F
SVR Well No. 20
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Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 26 of 28
EXHIBIT Q
Well Permits
Spring Valley Well No. 1
Spring Valley Ranch Well Nos. 2-3
SVR Well No. 20
"11&/%*96&9)*#*52
4QSJOH7BMMFZ3BODI8FMM/P
ORIGINAL PERMIT APPLICANT(S)
AUTHORIZED AGENT
SPRING VALLEY HOLDINGS LLC (ARDENNE, MARTIN V.)
CORONA WATER LAW (CORONA, CRAIG)
APPROVED WELL LOCATION
Water Division:
Designated Basin:
Management District:
County:
Parcel Name:
5
N/A
N/A
GARFIELD
N/A
Water District: 38
Well to be constructed on specified tract of land
Northing: 4375444.8
UTM COORDINATES (Meters, Zone:13, NAD83)
306850.4Easting:
WELL PERMIT NUMBER 86631-F
RECEIPT NUMBER 10017403
ISSUANCE OF THIS PERMIT DOES NOT CONFER A WATER RIGHT
CONDITIONS OF APPROVAL
1) This well shall be used in such a way as to cause no material injury to existing water rights. The issuance of this permit does not
ensure that no injury will occur to another vested water right or preclude another owner of a vested water right from seeking
relief in a civil court action.
2) The construction of this well shall be in compliance with the Water Well Construction Rules 2 CCR 402-2, unless approval of a
variance has been granted by the State Board of Examiners of Water Well Construction and Pump Installation Contractors in
accordance with Rule 18.
3) Approved pursuant to CRS 37-90-137(2), to change/expand the use of an existing well, permit no. 52185-F (expired), and to
install a pump, on the condition that this well is operated in accordance with the Spring Valley Development, Inc., and Basalt
Water Conservancy District Augmentation Plan approved by the Division 5 Water Court in case no. 98CW0254, 98CW0255 (an
amendment to case no. 84CW0212) and 98CW0256, to operate as part of an integrated supply system to serve the Spring Valley
Ranch PUD property. If this well is not operated in accordance with the terms of said decree, it will be subject to administration
including orders to cease diverting water. This well is known as Spring Valley Ranch Well No. 3.
4) The use of ground water from this well, in combination with the other wells within the Spring Valley Ranch PUD, will consist of
577 residential units including affordable housing units and cooperative ownership cabins, two 18 hole golf courses, and some
limited commercial development. The irrigation will consist of 90 acres associated with the residential and commercial
development, and 420 acres of golf courses, open space, and agricultural areas.
5) The pumping rate of this well shall not exceed 300 GPM. The simultaneous maximum pumping rate of Spring Valley Well No. 1,
Spring Valley Ranch Well Nos. 2 and 3, SVH Well Nos. 5 through 10, ASR Well Nos. 13 through 16, and SVR Well Nos. 17 through
36 (Additional Wells), combined with withdrawals from Hopkins Spring #1 and #2, shall not exceed 2,700 GPM (6.0 cfs), as
decreed.
6) The annual withdrawal of ground water from this well, in combination with all of the wells within the Spring Valley Ranch
development, shall not exceed 1,457 acre-feet.
7) The return flow from the use of this well and the other wells within the development will be through a central system (Spring
Valley Sanitation District), except for the 91 Ranch lots which will utilize non-evaporative Individual Sewage Disposal Systems, in
which the water will be returned to the same stream system in which the well is located.
8) The owner shall mark the well in a conspicuous place with well permit number(s), name of the aquifer, and court case number
(s) as appropriate. The owner shall take necessary means and precautions to preserve these markings.
9) A totalizing flow meter must be installed on this well and maintained in good working order. Permanent records of all diversions
must be maintained by the well owner (recorded at least annually) and submitted to the Division Engineer by November 15th of
each year.
10) This well shall be located not more than 200 feet from the location specified on this permit and decreed in Division 5 Water
Court case no. 98CW0124.
PERMIT TO USE AN EXISTING WELL
SE 1/4 NW 1/4 Section 29 Township 6.0 S Range 88.0 W Sixth P.M.
Physical Address: N/A
For questions about this permit call 303.866.3581 or go to https://dwr.colorado.gov Page 1 of 2Printed 02-12-2022
4QSJOH7BMMFZ3BODI8FMM/P
11) This well shall be constructed at least 600 feet from any existing well, completed in the same aquifer, that is not owned by the
applicant.
NOTE: This permit will expire on the expiration date unless a pump is installed by that date. A Pump Installation and Production
Equipment Test Report (GWS-32) must be submitted to the Division of Water Resources to verify the well has been constructed
and the pump has been installed. A one-time extension of the expiration date may be available. Contact the DWR for additional
information or refer to the extension request form (GWS-64) available at: dwr.colorado.gov
NOTE: Expired and cancelled permit nos. 96896, 28961-F, 23518-F, and 52185-F were previously issued for this well. Spring
Valley Ranch Well No. 3 conditional in case no. W3702.
2/11/2022
2/11/2023Issued By JUSTINA MICKELSON
Expiration Date:
Date Issued:
For questions about this permit call 303.866.3581 or go to https://dwr.colorado.gov Page 2 of 2Printed 02-12-2022
WELL PERMIT NUMBER 86631-F RECEIPT NUMBER 10017403
4738FMM/P
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 27 of 28
EXHIBIT R
Landis Creek Metropolitan Districts
Service Plan
"11&/%*96
&9)*#*53
Garfield County Community Development
Spring Valley Holdings Ranch PUD Phase 2 Final Plat Application
________________________________
Page 28 of 28
EXHIBIT S
Zancanella & Associates
Groundwater Monitoring Plan
February 21, 2022
Martin Van Ardenne
The Seligman Group
600 Montgomery St, 40th floor
San Francisco, CA 94111
415-658-2889
Re: Preparation of a Groundwater Monitoring Plan for the Proposed Phased
Development of Spring Valley Ranch.
Dear Martin:
Garfield County Resolution No 2010-38 has a requirement for a Groundwater
Monitoring Plan in paragraph 11.0 -11.1.
- 11.0 Available surface water supplies shall be used to their fullest extent to
provide the irrigation supply to the golf courses in order to minimize
groundwater withdrawals. A groundwater monitoring plan shall be developed
to monitor future water levels near the Spring Valley Ranch wells. The
monitoring plan shall include water level measurements in the production
wells and other wells at the PUD that can be used as monitoring holes. The
monitoring plan shall include measurements made with enough frequency to
observe seasonal groundwater fluctuations and long term groundwater
trends. Results of the monitoring program shall be available to the public.
- 11.1 There will be an additional monitoring well developed or identified that is
at least 2000 feet from the production wells. Either a new well or an off-site
well meeting those criteria could meet the criteria. All of the monitoring
reports will be available to the public.
Zancanella & Associates has reviewed the requirements and the wells for the property
and have developed a Groundwater Monitoring Plan to meet the requirements of Garfield
County. The groundwater monitoring plan is a phased approach that matches the phased
approach of the proposed development in the Spring Valley Ranch PUD, (SVR).
"11&/%*96&9)*#*54
Zancanella & Associates, Inc.
February 21, 2022
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Garfield County requires, a monitoring well developed or identified at least 2000 feet from
the SVR production wells and water level measurement of the production wells at SVR.
The County requires that the wells be monitored at a frequency to observe seasonal
groundwater fluctuations and long-term groundwater trends.
For the Groundwater Monitoring Plan, we have identified three wells to be used for
baseline monitoring and long-term monitoring of the groundwater in the Spring
Valley Aquifer. Prior to any development of the SVR PUD, we recommend that the
identified monitoring wells have water level measurements taken at least monthly.
Baseline Monitoring:
To understand the current ground water levels in the Spring Valley area, baseline,
predevelopment measurements are needed. Three onsite SVR wells will be observed
during the period of pre-development. Once development starts, additional wells could
be brought online to measure and monitor the ground water levels if necessary.
The three wells that are proposed are: ASR Well No. 15, SVH Well No. 6, and
Monitoring2EVHUYDWLRQ Well 1R. These wells are illustrated on Figure 1 in Appendix
A with cyan labels. Below are the location of each of the proposed monitoring wells
and associated well permit numbers.
ASR Well No. 15 is located within the Spring Valley Ranch Property. This well is
located in the SWNE of Section 27, T 6S, R 88 W. The well permit associated
with this well is 36760-MH.
SVH Well No. 6 is located within the Spring Valley Ranch Property. This well is
located in the SWNE of Section 29, T 6S, R 88W. The well permit associated with
this well is 68889-F.
0RQLWRULQJ 2EVHUYDWLRQ :HOO 1R . Is located within the Spring Valley
Ranch Property. This well is located in the SWNE of Section 33, T 6S, R
88 W. The well permit associated with this well is 251164. Well 03-2,
wouldalsobe DQacceptable monitoring location on the southern property
boundary.
To monitor the wells before the development at SVR occurs, battery operated transducers
will be installed in the three designated wells. Long term permanent power will not be
available at these monitoring wells until production wells are brought online and water
diversions are required. The battery-operated transducers will be set to take a water level
reading at minimum of once a day at a consistent time. The transducers will be
downloaded a minimum of once every six months and processed. The data can then be
reviewed to track the groundwater fluctuations from the seasonal fluctuations and the
existing demands on the aquifer.
The importance of this baseline monitoring is to understand both the annual and the
seasonal groundwater fluctuations that are naturally occurring in the aquifer prior to the
Spring Valley Ranch development. The locations of wells were selected so that the
Zancanella & Associates, Inc.
February 21, 2022
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https://zanda5700.sharepoint.com/Zdrive/28000/28604 Spring Valley Ranch/28604.2 County Permitting/Groundwater Monitoring Plan/Goundwater Monitoring Plan - Report 02-21-22.docx
middle bench of Spring Valley Ranch and the lower bench of Spring Valley Ranch will be
monitored.
The well locations were chosen to be existing wells. These wells are situated in near
proximity to the proposed production wells and provide the 2000 foot spacing from other
production wells. This configuration allows for the monitoring of the direct impacts from
the production wells in proximity and the overall fluctuations in the aquifer.
Below is a brief explanation of what each well will monitor.
- ASR Well No 15. This onsite well is located on the middle bench generally in
the southern portion of the Spring Valley Ranch PUD. This well was historically
used to monitor other wells and is a good location to monitor the effects of the
production wells that are proposed on the middle bench of the SVR PUD.
- SVH Well No. 6: This onsite well is located on the lower bench of the Spring
Valley Ranch PUD. This well is centrally located along the western side of the
PUD and is in the proximity of potential production wells located on the lower
bench. This well location is proposed to monitor the aquifer water levels along
the western side of SVR.
- 0RQLWRULQJ2EVHUYDWLRQ:HOO1R. This on site well is located on the lower
valley near the southern HGJHRIWKH6SULQJ9DOOH\5DQFKSURSHUW\OLQH7KLVZHOO
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DORQJWKHVRXWKHUQSURSHUW\OLQHRI69538'
Once the specified baseline monitoring points have been put into operations and the data
process, the information should be reviewed to determine if additional monitoring points
are needed or if current monitoring points need to be modified. Baseline monitoring points
should have the flexibility to change with proper justification. If it is found that the location
does not show connection to the aquifer or if there is too much interference from a well in
close proximity that will not allow for proper groundwater monitoring, a better location
within the same general area should be allowed. Care should be taken in moving and
adjusting monitoring well locations as shifting data points may not provide the monitoring
that is intended in this plan without additional baseline monitoring from the potential
relocated locations. The purpose of the monitoring program is to observe the impacts if
any with an open mind.
The Spring Valley Hydrologic System Report prepared by Gamba & Associates dated
March 10, 2000 is included in Appendix A. This report included exhibits of the underlying
geology in the Spring Valley area that was used to determine the locations of these
monitoring wells.
Zancanella & Associates, Inc.
February 21, 2022
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Production Well Monitoring:
The requirement to measure the water levels and the fluctuations in the production wells
will be implemented in a phased approach. The Spring Valley Ranch PUD is a multi-
phased development for the water system improvements and structures being built. We
recommend monitoring Production Well SVR Well No. 20 and Production Well ASR Well
No.16 first as they are identified as Phase 2 production wells. As additional production
wells are designated, water level and meter data will be collected concurrent with their
use.
With the development of the production wells, permanent monitoring devises with
production meters are recommended to be installed. The wells that are available to
supply the PUD are shown on the exhibit in Appendix A.
If the proposed production well locations are changed or additional production wells are
identified, the requirement to monitor carries to any future production well in the Spring
Valley Ranch PUD. If a well is permanently taken out of production, the monitoring
requirements shall not apply.
Additional Information:
As stated in the prior sections, baseline monitoring shall be installed and implemented
prior to the production wells coming online. All groundwater monitoring records will be
held by Landis Creek Metropolitan District No. 1 and will be available to the public.
Please do not hesitate to contact us with any questions pertaining to this plan.
Very truly yours,
Zancanella & Associates, Inc.
Thomas A Zancanella P.E.
Attachments
Zancanella & Associates, Inc.
February 21, 2022
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Appendix A
)HHW
Well
# 03-2 Well
# 03-1
Monitoring / Observation
Well No. 1
The purpose of this report is to examine geologic and hydrologic data related to the
geographic area known as Spring Valley and, there from, prepare estimates of the
potential specific yield of the water bearing horizons (aquifers) and estimates of amount
of annual recharge to those water bearing horizons.
A segment of the natural phenomenon that will be discussed in this dissertation is often
referred to as the “Spring Valley Aquifer”. This is the approximate 1,500-acre area
basin, flanked on the east by County Road 114 and on the north by County Road 115. It
has been penetrated by a number of wells that serve Colorado Mountain College, the sod
farm and most of the single-family homes along 114 road and 115 road. The small
stream that drains the surface of the basin, discharges in Red Canyon.
This basin, as noted above, represents only a segment of a dynamic hydrologic system
comprised of highly favorable geologic conditions situated in a meteorological
environment conducive to precipitation levels substantially greater than the adjacent
lower valley areas.
GEOLOGIC CONDITIONS
The recharge area of the Spring Valley Hydrologic System is comprised of approximately
15.4 square miles. This area, illustrated on the attached map, varies in elevation from
6,870 to 9,400 feet. The surficial geology of this recharge area may be divided, for
purposes of hydrologic consideration, into three petrographic types:
xSiltstones, sandstones, clay stones and conglomerates of the Pennsylvanian/
Permian Maroon Formation;
xBasalt flows, basalt talus, colluvium comprised predominantly of basaltic
material, all of Tertiary and early Quaternary age; and
xQuaternary lacustrine materials comprised predominantly of fine-grained products
of the chemical and mechanical weathering of the older rock materials that were
deposited in a lake. Samples from recent well drilling have been examined which
indicate deposits of volcanic ash in the lower portions of the lake basin.
Stratigraphically, the Maroon Formation under lays the basalt and alluvial materials. It
overlays the Eagle Valley Evaporate Formation, sometimes referred to as the Paradox
Formation. The Maroon formation, along with underlying sediments, was elevated and
exposed by erosion in the course of the orogeny that created the White River uplift to the
north.
The Eagle Valley Evaporite formation contains beds of soluble salts such as Gypsum and
Halite. The introduction of ground water into these salt beds resulted in the slow, but
steady solution and removal of several thousand feet of this formation over a large
section of a portion of the Roaring Fork River drainage area. The area of the Spring
Valley Hydrologic System straddles the northern edge of this affected area. As the salts
were removed, the overlaying rocks settled. This activity was, likely, very similar to the
current mining of soluble minerals by hydrothermal water as demonstrated by the
Glenwood Hot Springs and the other hot springs along the Colorado River. The solution
and removal of salts was not uniform over the effected area and the collapse of the
The Spring Valley Hydrologic System
March 10, 2000
Page 2 of 11
overlaying rocks resulted in deformation, shear fracturing and faulting of the Maroon
formation as well as the overlaying rock of volcanic origin. The intensity of this
fracturing may be better understood by observing the Maroon Formation outcrops
exposed along Highway 82 from Carbondale to Red Canyon. The sandstone beds which
are interbedded with siltstones and shales are well-cemented, relatively hard rock. When
they were originally deposited and lithified, they formed straight, flat, continuous
unbroken layers of stone. Now they have the character of blocks of stone laid up in a dry
stack wall constructed on an uneven surface. While a minor amount of this fracturing
may be attributed to the White River Uplift activity, the vast majority is the result of
irregular collapse due to the solution mining of the underlying Eagle Valley Evaporites.
The volcanic materials were similarly fractured by this removal of the evaporite basement
rock. The fracturing of relatively continuous lava flows may be observed in the cliffs
along the lower reaches of Landis Creek and on the slopes northerly of county road 115.
The high infiltration rate and water bearing capacity of the volcanic rock material is the
product of the above noted, intense fracturing of the very brittle basalt coupled with the
high porosity of the subsurface beds and lenses of volcanic ash, cinders and breccias.
The strongest fault/fracture systems are indicated by geomorphologic evidence and are
illustrated on the map. It appears that most of the fracturing of the volcanic materials is
the result of bending and slumping of the rock layers which caused very little
displacement from one side of the fault/fracture zone to the other. Some of the volcanic
material outcrops and sub-outcrops are virtually rubblized while other outcrop sections
appear to be rafted basalt blocks with horizontal dimensions of several hundred feet.
Much of the land surface which slopes at 20% or greater has a very thin to virtually non-
existent soil cover. Vegetation, in these areas, is sparse and small indicating that it
survives with a minimal moisture supply, even though the area receives 25 to 30 inches
of precipitation per year. Excavation in the course of constructing pioneer roads reveals
areas of the subsoil rock, to be comprised primarily of medium sized to massive boulders
wherein the “porosity” may be visualized as that which would result from the stacking of
poorly sorted particles that range in size from basketballs to Volkswagens. The
percolation rate in these areas is obviously, very rapid.
In some areas of the surface, where the land slope is less than 15 percent, soil has
accumulated to depths of as much as 20 feet over the rock. Percolation tests were
conducted on soils of this type at 11 locations in the upland aquifer recharge area. The
average of the percolation rates measured was 25.5 minutes per inch (2.35 inches per
hour) with the range being from 3 to 64 minutes per inch. Of the 11 tests, 8 measured at
34 minutes per inch or less.
The volcanic activity events of 3 to 4 +/- million years ago deposited 100 to 200 feet or
more of interlayered basalt, cinders, ash, and breccias on a substantially more horizontal
surface than is present in the area today. The intervening 3 million +/- years of erosion
on that surface, which was slowly tilting southerly, has removed the softer,
unconsolidated cinders and ash from the surface, exposing, hard, weather resistant basalt.
The remaining, highly porous ash and cinder lenses below the hard basalt surface provide
pockets or constricted basins of high porosity where ground water is detained. Surface
The Spring Valley Hydrologic System
March 10, 2000
Page 3 of 11
water is channeled into these detention basins or “hanging aquifers” via the fractured and
rubblized surface basalt. Subsurface fractures interconnect the detention basins and act
as restricted conduits that facilitate the slow, but continuous, transmission of water from
those at higher elevations to the ones below.
The segment of the system, which is referred to, as the Spring Valley Aquifer is in fact a
composite of a series of confined aquifers in the sediments overlaying the bedrock, and
the upper portion of the bedrock, underlying these sediments, which is itself, a confined
aquifer capable of, and demonstrated to produce artesian wells.
The confined aquifers within the lakebed sediments are comprised of sand and sandy
gravel horizons confined between layers of clay or sandy, gravely clay. From previous
drilling and data from Spring Valley Ranch well #6 drilled in February and March 2000,
it appears that the lower 70 to 110 feet of the sediment section in the northwestern end of
the basin is very fine-grained sand. Samples taken from this well drilling were tested and
it was determined that the specific porosity of this material is approximately 30%.
Microscopic examination of this material reveals that it is highly angular, with the
appearance of shattered glass. The particles do not exhibit the characteristics of sand
grains that have been subjected to significant transportation and attrition by either water
or wind action. It is suspected that this sand is vitric volcanic ash, which was deposited
in and adjacent, upslope of the lake basin during the creation of the basin by subsidence,
as discussed below.
The bedrock form of the lake basin is a “half graben” with the fault on the southerly side
along County Road 119. The bedrock is comprised of Maroon Formation sediments,
capped with 100 feet or more of volcanic material similar to that which may be observed
on the north side of 115 road and in the cap rock on the south side of the valley. This
bedrock block tilts, or more accurately “slumps” southerly From the divide between the
Colorado and Roaring Fork river drainages, down the south facing slopes of Spring
Valley and under the basin, to its termination at a fault that extends along the southern
side of the valley.
An additional feature has been observed in the aquifer basin. In many of the deep drill
holes, the volcanic rock section below is separated from the overlaying lake sediments by
a layer of blue gray clay as much as 40 feet thick. This is probably montmorillonite clay
of the bentonite variety that is formed by the alteration of volcanic ash and tuff. Where
present, this clay layer acts as a seal between the lake sediments and the underlying
volcanic rock material.
HYDROLOGIC CONDITIONS
The conditions and events noted above created the geologic setting for the Spring Valley
Hydrologic System. The other component of the system is the precipitation provided by
the meteorological environment.
Average annual precipitation in the Colorado Mountains increases substantially with
elevation. This is illustrated on the Colorado Average Precipitation Map, 1951 to1980,
prepared by Colorado State University in conjunction with Climatology Report 84-5,
The Spring Valley Hydrologic System
March 10, 2000
Page 4 of 11
published by the U.S. Geological Survey. This map indicates that the uppermost part of
the recharge area of this hydrologic system receives an average of 30 inches of
precipitation per year while the lowest portion of the recharge area receives 16 inches to
20 inches per year.
PRECIPITATION INFILTRATION
The effective introduction of this precipitation into the underground hydrologic system is
largely dependent upon the character of the surface geology. Fractured basalt flows,
basalt talus and colluvium comprised predominantly of granular soil and rock are highly
permeable, wherein it is estimated that, at least 60% of the precipitation will enter the
aquifer after evaporation, transpiration and surface run-off. This high rate of infiltration
is graphically demonstrated by the drainage along County Road 115 within the Spring
Valley Ranch. The Basalt hillside northerly of the road ranges in slope from 10 to 40
percent. The average annual precipitation received by this area is 20 to 25 inches per
year. Drainage sub-basins above, discharge to these slopes, yet many of the natural
drainage swales crossed by the road do not have culverts and do not have the appearance
of areas that transport or pond water. It is reported, by longtime residents of the area, that
only on occasions of extremely high snow melt or cloud burst, does flooding of the road
occur.
This condition has also been observed on the pioneer roads constructed on the higher
portions of the Spring Valley Ranch that are underlain by fractured basalt or thin granular
soils over basalt. The inability of the thin soils to retain moisture is demonstrated by the
light vegetation cover.
The topographic characteristics of the highly basaltic surfaces are further evidence of its
high infiltration rate. This is an area that sustains an average precipitation of 20 to 30
inches per year on slopes of 10 to 50 percent. If the rate of infiltration of precipitation
was not exceptionally high, the large volume of high velocity run-off would have eroded
major drainage swales and gulches down the slopes, nearly perpendicular to the contours.
The precipitation does occur, but the run-off does not. Instead, this precipitation enters
the fractured and otherwise highly porous basaltic materials and is detained there in a
series of cascading aquifers that are interconnected by shear fracture zones. These
fracture zones function as control orifices and slowly release the gravity flow of water to
springs and the aquifers below.
Conversely, fractured Maroon formation overlain with silty, loam soils supporting
moderate to heavy vegetation will result in the infiltration of approximately 20% of the
precipitation with the balance being lost to evapotranspiration and surface runoff. Where
this surface runoff must cross the basaltic areas noted above, much of it will enter the
groundwater system.
The conditions described above were applied to the map of the recharge area, prepared on
the basis of published geologic mapping and personal observations. The following table
was prepared which estimates the average precipitation amount in the recharge area and
the potential infiltration amount entering the underground hydrologic system.
The Spring Valley Hydrologic System
March 10, 2000
Page 5 of 11
PERCIPITATION ZONE
AND ESTIMATED
INFILTRATION RATE
AREA
(ACRES)
AVERAGE ANNUAL
PRECIPITATION (A/F)
ESTIMATED
INFILTRATION TO
AQUIFER (A/F)
16’ – 20” (18”) 20% 592 888.0 177.6
16” – 20” (18”) 60% 1,497 2,245.5 1,347.3
20” – 25” (22.5”) 20% 1,050 1,968.8 393.8
20” – 25” (22.5”) 60% 2,180 4,087.5 2,452.5
25” – 30” (27.5”) 20% 450 1,331.3 206.3
25” – 30” (27.5”) 60% 3,794.6 8,694.6 5,216.8
30” 75% 277 692.5 519.4
TOTAL 9,840.6 19,908.2 10,313.7
WET/DRY YEAR 11,345.07/8,250.96
As may be observed, the above calculations indicate that more than 50% of the system
recharge occurs in the higher elevations. The possible amount of recharge to the aquifer
may also be estimated by the following formula:
recharge = precipitation – evapotranspiration – surface flow down red canyon.
Observations made by Wright Water Engineers, indicate that the surface flow down Red
Canyon will vary from 400 to 600 acre feet per year. As noted above, the estimated
average precipitation for the total system recharge area is computed to be 19, 908.2 acre
feet per year.
The following table illustrates an estimate of the probable losses to evapotranspiration in
the various precipitation zones and vegetation types. The evapotranspiration rate factors
used in the calculations were taken from Handbook of Applied Hydrology by Chow,
McGraw-Hill.
PRECIPITATION
ZONE
WATERSHED AREA
(ACRES)
VEGETATION TYPE
& EVAPOTRANSPIRATION
FACTOR (INCHES/YEAR)
POTENTIAL LOSS TO
EVAPOTRANSPIRATION
16” –20” 2,089 GRASS, BRUSH & SHRUBS
5-10 (USE 7.5)
1,305.6
20” –25” 3,230 GRASS, BRUSH & SHRUBS
5-10 (USE 7.5)
2,018.8
25” – 30” 2,122,3
2,122.3
50%GRASS, BRUSH & SHRUBS
7.5
50% ASPEN/FIR
23
1,326.4
4,067.7
30’ 277 ASPEN/FIR
23
530.9
TOTAL 9,840.6 9,249.4
Appling the equation noted above:
recharge = precipitation – evapotranspiration – surface flow down red canyon.
Probable Recharge = 19,908.2 - 9,249.4 – 600 = 10,058.8 acre feet per year
The section underlain by basaltic materials located easterly of Landis Creek accounts for
the majority of the recharge and is believed to support the greatest detention volume in
the system, which, in turn recharges the Spring Valley Aquifer.
The Spring Valley Hydrologic System
March 10, 2000
Page 6 of 11
This belief is supported by the presence of consistently flowing springs which surface in
the upland area and the characteristics of the seven wells which have been drilled there
and pump tested . One well was drilled in the Maroon formation and six in the volcanics.
All of the wells were test pumped for 24 hours immediately following drilling and 3 were
selected for extended pump tests. The extended pump tests are described in the Wright
Water Engineers, Inc., report “Spring Valley Upland Aquifer Pumping Tests – 2000”.
Peter Cabrinha has been closely associated with the Spring Valley Ranch for 37 years and
has observed the performance of springs on the property. In a recent interview with Mr.
Cabrinha, the following observations were related:
xAll of the springs appear to flow year around at relatively consistent rates with the
exception of periods following extremely low winter and spring precipitation.
xIn his 37 years of observation, there were two occasions when the upper Landis
Creek springs, at 9,100 ft elevation, stopped flowing. These stoppages occurred
in the late summer or early fall of the year following the low winter and spring
precipitation. The springs resumed flow the following spring.
xThe flows of the lower elevation springs do not appear to diminish following dry
winter/spring seasons.
ESTIMATE OF SPECIFIC YIELD OF SYSTEM AQUIFIRS
In order to accommodate to the performance described above, the hydrologic system
must receive a substantial portion of the precipitation, as indicated in the table above, and
have a sufficient volume of specific yield to detain the infiltrated precipitation of several
years.
Information is available to compute a conservative estimate of the potential specific yield
of the aquifers in the system. The following assumptions and parameters will be used in
computing the estimated specific yield.
1.The upland area in the 20-inch to 30+-inch precipitation zone covered by volcanic
materials contains approximately 5,975 acres.
2.The thickness of the volcanic materials intercepted by the six wells, drilled in
volcanics, in the upland area ranged from 112 feet to 200 feet with an average of
168 feet. The depth of water in the wells (static level to bottom) ranged from 46
feet to 310 feet with an average of 135 feet. For conservative estimating
purposes, a saturated thickness of only 50 feet will be used.
3.The porous volcanic materials will perform similarly to sand, gravel and cobbles
for which the specific yield will range from 34% to 20% (from Figure 5-4 Bear
Jacob. 1979 Hydraulics of Groundwater. McGraw-Hill). For conservative
estimating purposes, a range of 10 to 20% will be used.
4.The surface area of the Spring Valley aquifer is approximately 1,500 acres.
5.Well log information indicates that the thickness of lake sediments may average
from 250 to 300 feet. in thickness, comprised of 10 to 20 feet of gravel bed, 140
to 180 feet of sandy, clayey silt with some gravel and 70 to 110 feet of very fine
sand (vitric volcanic ash). For conservative estimating purposes, the following
will be used for the lake sediments:
The Spring Valley Hydrologic System
March 10, 2000
Page 7 of 11
Sandy, clayey silt = 140 feet; gravel = 10 feet; very fine sand = 70 feet.
6.The specific yield of gravel beds in the lake sediments will range from 25% to
34%; the silty clay may range from 3% to 25%; the sand from 25% to 35% (from
Figure 5-4 Bear Jacob. 1979 Hydraulics of Groundwater.) McGraw-Hill). For
conservative estimating purposes, 25% will be used for the gravel beds and 3%
will be used for the clayey sediments and 20% for the very fine sand.
Bear Jacob. 1979. Hydraulics of groundwater. McGraw-Hill.
The following calculations of the specific yield of the aquifers in the hydrologic system
are based on the assumptions and parameters stated above.
Upland volcanic areas
5,975 acres x 50 feet thick x 0.10 or 0.20 specific yield = 29, 875 to 59,750 acre feet
Spring valley aquifer gravel beds
1,500 acres x 10 feet thick x 0.25 specific yield = 3,750 acre feet
Spring valley aquifer silty clay sediments
1,500 acres x 140 feet thick x 0.03 specific yield = 6,300 acre feet
Spring valley aquifer very fine sand bed
1,500 acres x 70 feet thick x 0.20 specific yield = 21,000 acre feet
Volcanics at base of Spring Valley aquifer
1,500 acres x 50 feet thick x 0.10 or 0.20 specific yield = 7,500 to 15,000 acre feet
ESTIMATED TOTAL SPECIFIC YIELD OF AQUIFERS IN
SPRING VALLEY HYDROLOGIC SYSTEM = 68,425 to 105,800 AF
The Spring Valley Hydrologic System
March 10, 2000
Page 8 of 11
Note: the above calculations do not include the volcanic areas in the 16” to 20”
precipitation zone nor any of the Maroon formation area.
ADDITIONAL AQUIFER CHARACTERISTICS
Examination of the records of the State Engineer indicates that the majority of the
domestic (single family home) wells in the Spring Valley are drawing water from the
upper to middle, silty, clayey lakebed sediments. Although the specific yield of these
materials is estimated to be only 3%, it is believed to be a viable segment of the aquifer
because it can provide adequate supplies of water to small domestic wells in the valley
bottom and probably not be effected by the pumping of large volume wells which draw
from the higher yield sands and volcanics in the lower section of the aquifer.
The large volume wells of CMC, Los Amigos and the sod farm are drawing water from
the volcanic material horizon at the base of the Spring Valley aquifer. Intermediate test
pumping of Spring Valley Ranch well #6 from the fine sand zone above the clay
indicates that sustained production of at least 250 gpm is available from this material.
The static head elevations of the CMC and Los Amigos wells, on the southeast end of the
valley, is approximately 100 feet lower than the Spring Valley Ranch wells on the
northwest end indicating a general flow of northwest to southeast. This would support
the theory that the aquifer outflow generally follows the half graben fault fracture system
to the roaring fork valley.
SUMMARY AND CONCLUSIONS
1.The source of recharge for the Spring Valley Aquifer is predominantly from the
volcanic material in the upland aquifers.
2.This writer believes the average annual precipitation entering the system as
recharge and flowing through the series of aquifers, to be approximately 10,000
acre-feet. Peer review of this information by others who have not had the benefit
of on-site observations, assign substantially higher volume to loss by
evapotranspiration and therefore estimate the average annual recharge volume
more conservatively at 4,700 acre-feet. Considering that the potential total annual
depletion of the aquifer by existing and future land development is in the vicinity
of 1,300 to 1,500 acre feet, the lower figure still assures viability of the aquifer.
3.The estimated specific yield volume of the aquifers in the hydrologic system is in
the range of 68,000 to 105,000 acre feet, of which approximately 38,000 to
46,000 acre feet are contained in the Spring Valley aquifer and approximately
30,000 to 60,000 acre feet are available in the upland volcanic material aquifers to
recharge the Spring Valley aquifer. These large volumes of stored water provide
a leveling effect to the variations in annual precipitation over a period of 6 to 10
years, or more.
4.A substantial portion of the water that enters the system does not again surface in
the system, but, leaks out through fracture systems associated with the half graben
The Spring Valley Hydrologic System
March 10, 2000
Page 9 of 11
fault on the south side of the Spring Valley aquifer and probably enters the
Roaring Fork River valley gravel aquifer.
5.The most promising target zones for a large production well appears to be the
volcanic ash layer in the lower sediments and the volcanic material horizon below
the sediments in the Spring Valley Aquifer.
6.It is highly probable that water production from the lower volcanic ash layer in
the sediments and the volcanic material horizon below the sediments in the Spring
Valley Aquifer will reduce the leakage to the Roaring Fork River area, but will
have little or no effect on the small domestic wells in the upper sediments or the
surface discharge down Red Canyon.
Respectfully,
Jerome F. Gamba, P.E. & L.S. 5933
Enclosures: Exhibit 1, Map of Spring Valley Hydrologic System
Exhibit 2, Generalized Geologic Section of Spring Valley and Upland
Aquifers
The Spring Valley Hydrologic System
March 10, 2000
Page 10 of 11
REFERENCES
Bass, N.W., and Northrup, S. A., 1963, Geology of Glenwood Spring
Quadrangle and Vicinity, Northwestern Colorado: U.S. Geological Survey
Bulletin 1142-J 74p.
Colorado Average Precipitation Map, 1951 to 1980, prepared by Colorado
State University in conjunction with Climatology Report 84-5, published
by the U. S. Geological Survey.
Colorado Geological Survey, 1974, Roaring Fork and Crystal Valleys-An
Environmental and Engineering Geology Study, Environmental Geology
No. 8.
Kirkham, Robert, M. and others, 1995, Geologic Map of the Glenwood
Springs Quadrangle, Garfield County, Colorado, Colorado Geologic
Survey, Open File Report 95-3.
Kirkham, Robert, M. and others, 1995, Geologic Map of the Shoshone
Quadrangle, Garfield County, Colorado, Colorado Geologic Survey, Open
File Report 95-4.
Kirkham, Robert, M. and others, 1996, Geologic Map of the Cattle Creek
Quadrangle, Garfield County, Colorado, Colorado Geologic Survey, Open
File Report 96-1.
Kirkham, Robert, M. and Beth L. Widmann, 1997, Geologic Map of the
Carbondale Quadrangle, Garfield County, Colorado, Colorado Geologic
Survey, Open File Report 97-3
Geologic Map of the Spring Valley Ranch, 1999, CTL/Thompson, Inc.,
Consulting Engineers.
Report: Water Requirements, Water Resources, and Spring Valley Area
Water Balance, 2000, Wright Water Engineers, Inc.
The Spring Valley Hydrologic System
March 10, 2000
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