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NEWLAND SIERRA FEBRUARY 2017 GEOMORPHIC ASSESSMENT PHOTO EXHIBIT 2015 PHOTO No. 5 2015 PHOTO No. 4 2015 PHOTO No. 1 LEGEND POINT OF COMPLIANCE (POC) RECIEVING CHANNELS POC ANALYZED IN GEOMORPHIC ASSESSMENT 2015 PHOTO No. 2, 3 2015 PHOTO No. 6, 8 2015 PHOTO No. 26 2015 PHOTO No. 9 2015 PHOTO No. 10 2015 PHOTO No. 11, 12 2015 PHOTO No. 13 2015 PHOTO No. 14, 15 2015 PHOTO No. 16 2015 PHOTO No. 17 2015 PHOTO No. 18, 29 2015 PHOTO No. 19 2015 PHOTO No. 20, 21 2015 PHOTO No. 22 2015 PHOTO No. 23 2015 PHOTO No. 24 2016 PHOTO No. 1 2016 PHOTO No. 2, 3, 4 2016 PHOTO No. 5 2016 PHOTO No. 6 2016 PHOTO No. 8 2016 PHOTO No. 7 2016 PHOTO No. 9 2016 PHOTO No. 10 2016 PHOTO No. 11 2016 PHOTO No. 12 2016PHOTO No. 13 14 2016 PHOTO No. 15 2016 PHOTO No. 16 2016 PHOTO No. 17 2016 PHOTO No. 18 2015 PHOTO No. 25 2015 PHOTO No. 7 2015 PHOTO No. 27 2015 PHOTO No. 28 2015 PHOTO No. 29 2015 PHOTO No. 30
Transcript
Page 1: GEOMORPHIC ASSESSMENT PHOTO EXHIBIT · geomorphic assessment photo exhibit 2015 photo no. 5 2015 photo no. 4 2015 photo no. 1 legend point of compliance (poc) recieving channels poc

NEWLAND SIERRAFEBRUARY 2017

GEOMORPHIC ASSESSMENT PHOTO EXHIBIT2015 PHOTO No. 5

2015 PHOTO No. 4

2015 PHOTO No. 1

LEGENDPOINT OF COMPLIANCE (POC)

RECIEVING CHANNELSPOC ANALYZED IN GEOMORPHIC ASSESSMENT

2015 PHOTO No. 2, 3

2015

PH

OTO

No.

6, 8

2015 PHOTO No. 26

2015 PHOTO No. 92015 PHOTO No. 10

2015 PHOTO No. 11, 12

2015 PHOTO No. 13

2015 PHOTO No. 14, 15

2015 PHOTO No. 16

2015 PHOTO No. 17

2015 PHOTO No. 18, 29

2015 PHOTO No. 19

2015

PH

OTO

No.

20,

21

2015 PHOTO No. 22

2015 PHOTO No. 23

2015 PHOTO No. 24

2016 PHOTO No. 1

2016 PHOTO No. 2, 3, 4

2016 PHOTO No. 5

2016 PHOTO No. 6

2016 PHOTO No. 8

2016 PHOTO No. 7

2016 PHOTO No. 9

2016 PHOTO No. 102016 PHOTO No. 11

2016 PHOTO No. 12

2016PHOTO No. 13 14

2016 PHOTO No. 15

2016 PHOTO No. 16

2016 PHOTO No. 17

2016 PHOTO No. 18

2015 PHOTO No. 25

2015 PHOTO No. 7

2015 PHOTO No. 27

2015 PHOTO No. 28

2015 PHOTO No. 29

2015 PHOTO No. 30

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ChangCivil Engineering Hydrology Hydraulics Sedimentation

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Final Hydromodification Management Plan; Standard Urban Stormwater Mitigation Plan BMP Design

Manual

Hydromodification Screening Tools: Field Manual for Assessing Channel Susceptibility,

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Hydromodification Screening for Newland Sierra,

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Downstream Domain of Analysis

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Upstream Domain of Analysis

Study Reaches within Domain of Analysis

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Vertical Stability

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Lateral Stability

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Valley Width 4'

Valley Width 4'

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Valley Width 5'

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Valley Width 15'

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Valley Width 8'

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Valley Width 8'

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Valley Width 8'

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June 10, 2016

Project No. 10618.002 To: Ms. Rita Brandin Newland Sierra, LLC

9820 Town Centre Drive, Suite 100 San Diego, California 92121

Subject: Natural Drainage Observations, POC Areas 13B, 19 & 26 Newland Sierra, San Diego County, California In accordance with your request, we have conducted a reconnaissance of three natural drainages which exist on the slopes at the Newland Sierra project located in northern San Diego County, California (Figure 1). The undersigned visited the site on May 31, 2016 and conducted a visual reconnaissance within Point of Compliance (POC) Areas 13B, 19 and 26 which are presented on the attached Newland Sierra Critical Coarse Sediment Yield Impact Exhibit (Fuscoe, 2016). The purpose of this reconnaissance is to provide the design team with appropriate geologic information regarding the nature of the existing drainages to aid in the stream channel susceptibility characterization (armoring potential) process for storm water management design. Based on our site visit and review of our referenced preliminary geotechnical report (Leighton, 2015), the primary bedrock unit onsite is Cretaceous-aged Granite although Jurassic-aged Metavolcanic rock is present along the western margin. These units are in turn overlain by surficial units consisting of colluvium, alluvium, slopewash and minor undocumented fill soils. Surficial soil deposits generally consist of relatively fine-grained material useful during grading of a site where abundant oversize material is expected. We have confirmed through our geologic reconnaissance of POC Areas 13B, 19 and 26, that the existing channel bottoms are comprised of hard rock covered in some areas with a very thin veneer of alluvial soil that consists of fine to coarse rock fragments and boulders. It should be noted, due to thick impassable areas of brush located in all three natural drainages, our observations performed during our reconnaissance should be considered limited in terms of the extent of the reaches we could access, but not in terms of our conclusions. In other words, it is our opinion that the bed resistance of existing drainages can be considered to be a Coarse/Armored Bed that should not be susceptible to erosion due to the underlying hard rock (Bledsoe, 2010). In addition, for the County of

3934 Murphy Canyon Road, Suite B205 San Diego, CA 92123-4425 858.292.8030 Fax 858.292.0771 www.leightongeo.com

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10618.002

2

San Diego Critical Shear Stress Flow Calculator, the d50 will be indeterminate, and in any case larger than 24 inches, as the permissible shear stress will be in excess of 10 pounds per cubic feet. The recommendations contained in this letter report are based on available project information. Changes made during design development and construction, should be reviewed by Leighton to determine if recommendations are still applicable. We appreciate this opportunity to be service to you. If you have any questions regarding our letter, please contact this office. We appreciate this opportunity to be of service. Respectfully submitted, LEIGHTON AND ASSOCIATES, INC. Robert C. Stroh, CEG 2099 Roy N. Butz, PG 8942 Associate Geologist Project Geologist Extension: 4090, [email protected] Extension: 8489, [email protected] Distribution: (1) Addressee via electronic PDF

(1) Fuscoe Engineering; Attention: Mr. Eric Armstrong

Attachments: Figure 1 – Site Location Map Newland Sierra Critical Coarse Sediment Yield Impact Exhibit

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10618.002

3

REFERENCES

Bledsoe, B.P et al, Hydromodification Screening Tools, Field Manual for Assessing Channel Susceptibility, Technical Report 606, March, 2010.

Fuscoe Engineering, Newland Sierra Critical Coarse Sediment Yield Impact Exhibit, dated February, 2016.

Leighton and Associates, Preliminary Geotechnical Investigation, Newland Sierra, San Diego County, California, Project No. 10618.002, dated June 26, 2015.

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Figure 1

Scale:

Leighton

Base Map: ESRI ArcGIS Online 2016

1 " = 3,000 '

Project: 10618.002 Eng/Geol: WDO/RCS

Map Saved as P:\Drafting\10618\002\Maps\10618-002_F01_SLM_2016-06-03.mxd on 6/3/2016 1:32:18 PM

Author: mmurphy (mmurphy)

Date: June 2016SITE LOCATION MAP

Newland SierraSan Diego, California

ApproximateProject Boundary

³0 3,000 6,000

Feet


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