HomeMy WebLinkAboutDRB130159 REV1 Debris Flow Hazard Report.pdf . _�' L'. . _�i . I �i . . �
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HEPWORTH-PAWLAK GEOTECHNICAL F,� y��� �,�; y�;�
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May 22, 2013
Triumph Development
Atm: Mike rosier
12 Vail Road, Suite 400
Vail, Colorado 81657
inctbs�er�(i�?�,il�u��._coi�i
Job No. I 13 048B
Subject: Debris Flow Hazard Review, Proposed Noell Residencc, Lot 6, Spraddle
Creek Estates, 1000 Spraddle Creek Road, Vail, Colorado
Gentlemen:
As requested, we have reviewed the debris flow potential hazard for the proposed Noell
residence at the subject site. The purpose of our review was to evaluate if the proposed
residence is exposed to a debris flow hazu•d and is an addendum to our rockfall hazards
review report for the project dated April 30, 2013, under the above job number.
Summary of Findings: Our field observations and literature review indicate that the
proposed residence on Lot 6 is not exposed to a debris flow hazard risk.
Scope of Study: A field reconnaissance ofthe project area was made on May 19, 2013.
In addition we have looked at aerial photographs, detailed topogaphic inaps and
published regional debris flow information by Town of Vail (2000). This report
summarizes our field observations and presents our findings regarding the debris flow
hazard potential at the site. The study is supplemental to our previous proposal for
professional services with Triumph Development dated Deceinber 21, 2012.
Hepworth-Pawlak Geotechnical previously perfonned a subsoil study for foundation
design of the proposed residence at the site and submitted om� fmdings in a report dated
April 15, 2013, Job No. 112 048A.
Site Conditions: Spraddle Creek Estates is located on the south-facing Gore Creek
valley side just to the north ofthe Vail town center as shown on Figure 1. The general
Parker 303-841-7119 • Colora�loSprinhs 7�y-633-556Z • Silverrhorn� 970-�}68-I)ti)
Triumph Development
May 22, 2013
Page 2
topography in the project area is shown on Figure 2. The lots aze located on a hillside
bench and average slope ofthe bench across the proposed building site on Lot 6 is around
40% down to the south. This average 40% hillside slope continues uphill of Lot 6 to the
north. About 300 to 400 feet west of Lot 6 is Spraddle Creek, a fairly well incised
drainage. Spraddle Creek Road is located to the north of the proposed building site and
construction of the road has required several retaining walls to limit hillside disturbance.
Native vegetation in the area is mostly grass, sage brush and other brush with some aspen
trees. The existing retaining walls and revegetated cut slope uphill ofthe proposed
building site appear to be perfornung satisfactorily with respect to erosion and global
stability.
Field Observations: The steep hillside bench at Spraddle Creek Estates is underlain by
glacial till deposited by valley glaciers that occupied this part ofthe Gore Creek valley
during the middle Pleistocene-age Bull Lake and late Pleistocene-age Pinedale glaciations
(Kellogg, 2003). The Bull Lake glaciation occurred between about 132 and 302 thousand
years ago and the Pinedale glaciation occurred between about 10 and 35 thousand years
ago. The glacial till consists of subrounded, gravel- to lazge boulder-size rocks in a sandy
loam soil matrix. The glacial till has had a relatively stable, recent geologic past and
landslides or potentially unstable slopes that could produce debris flow material are not
present in the azea of Lot 6. The existing road cuts uphill ofthe proposed building site on
Lot 6 aze revegetated and erosionally stable. The existing road cuts should not be a
potential source of debris flow that could reach the proposed building site on Lot 6.
Regional Debris Flow Information: The regional debris flow map by Town of Vail
(2000) indicates a medium severity debris flow potential area that crosses the eastern part
of Lot 6 and extends through a narrow width in the central part of Spraddle Creek Estates.
The debris flow risk designation may be from a debris avalanche risk due to the locaily
very steep hillside in this azea, but based on our site specific review, in our opinion, Lot 6
is not in a debris flow (or debris avalanche) hazard area.
Limitations: This study was conducted according to generally accepted engineering
geology principles and practices in this area, at this time. We make no warranty either
express or implied. The information presented in this report is based on our field
observations. This report has been prepared exclusively for our client to evaluate if the
Job No. 113 048B
GecPteCh
Triumph Develop�nent
May 22, 2013
Page 3
proposed residence is in a debris flow hazard area. Our scope of seivices for the cunent
study is limited to debris flow hazard potential and does not include evaluation of any
other geological hazards fhat inay be present in the area. We are not responsible for
technical interpretations by others ofour information.
IfUiere are questions, please contact us.
Respectfully Submitted,
HEPWORTH -P���`�{"� TECHNICAL, INC.
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Steven L. Pac6�.�ak`�,,F�./n/i��'�
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Rev. by: DAY � `�` ��`�"-��"'
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Attachments: Figure 1, Project Site Location
Figure 2, Project Site Ma�
cc: RMT Architects—Paul Miller (paul<ci)rmtaaarcl�itects coml
Beck Building Company- Tom Solawetz (tom abeckbuilds.com)
Monroe and Newell—Craig Can�oll (ccan•oll��inonroe-newelLcom)
REFERENCES
ICellogg K. S. and Others, 2003, Geology Map of'the T�ail East Quadrangle, Eagle
County, Colorado: U. S. Geological Survey, Map MF-2375, Version 1.0.
Town of Vail, 2000, Official Debris FlowHazard Map, Town of Vail. Prepared by the
Town of Vail, Colorado (Adopted by the Town Council on October 17, 2000).
Job No. I 13 048B
VEC9tGCh
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May 2073
113 04$B �t�h Proposed Noell Residence I_ot 6 Spraddle Creek Estates
`"POdp�""w`"';GEOTEpHN1ON� Project Site Location Figure 1
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Scale: 1 In. = 250 fi.
Topographic infortnation from Town of Vail GIS Department Contour Interval: 2 ft.
May 2013
113 048B C'-s�Pte� Proposed Noell Residence Lot 6 Spraddle Creek Estates
HEPWpRTH�PAWLpKGEOTECHNICAL Project Site Map Figure 2