My WebLink
|
Help
|
About
|
Sign Out
RES 2026023
City of Pleasanton
>
CITY CLERK
>
RESOLUTIONS
>
2020-present
>
2026
>
RES 2026023
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
4/30/2026 9:30:47 AM
Creation date
4/28/2026 9:58:51 AM
Metadata
Fields
Template:
CITY CLERK
CITY CLERK - TYPE
RESOLUTIONS
DOCUMENT DATE
4/21/2026
DESTRUCT DATE
PERMANENT
DOCUMENT NO
RESO NO. 2026-023
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
285
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
<br />Sequoia Ecological Consulting, Inc. <br />CalVTP Project-Specific Analysis and Addendum <br />Augustin Bernal Community Park Fuel Reduction <br />November 2025 <br />4-50 <br /> <br /> <br />4.6.1. Discussion <br />The project area is located in Alameda County, within the Coast Ranges Geomorphic Province, which is <br />characterized by northwest-trending mountain ranges and valleys (California Geological Survey [CGS] <br />2002). The Coast Ranges are primarily composed of Jurassic- to Cretaceous-age (about 65–150 million <br />years old) marine sedimentary and volcanic rocks of the Franciscan assemblage. The Franciscan <br />assemblage consists of partially metamorphosed greenstone, basalt, chert, and graywacke that originated <br />as sea floor sediments. <br />The California Department of Conservation CGS Landslide Inventory (beta) map (CGS 2015) and the CGS <br />Earthquake Zones of Required Investigation Dublin Quadrangle (CGS 2008) were reviewed to identify <br />unstable areas within or in proximity to the treatment areas. The treatment areas are located on and <br />surrounded by land that has been and currently is subject to landslide, both weather-induced and <br />seismically induced. <br />Soils within the treatment areas are dominated by Los Gatos–Los Osos complex, 30 to 75 percent slopes, <br />eroded (65.3 percent), and Millsholm silt loam, 30 to 45 percent slopes (20.0 percent). Other soils make <br />up smaller percentages of the project footprint, such as Los Osos and Millsholm soils, 7 to 30 percent <br />slopes (8.1 percent), and Millsholm silt loam, 45 to 75 percent slopes, eroded (6.5 percent; Natural <br />Resources Conservation Service [NRCS] 2025). Table 8 below shows all soil types present within the <br />footprint of the treatment areas. The parent material for these soils consists of sandstone and shale, and <br />these soils are well drained to somewhat excessively well drained (NRCS 2025). The erosion hazard for the <br />soils ranges from moderately low to moderately high (NRCS 2025). As stated in the project description, <br />mechanical treatments would occur but would occur predominantly on slopes below 40 percent grade, <br />along ridges, and on slopes greater than 40 percent grade with equipment that can reach target vegetation <br />from existing road infrastructure. No mechanical treatment would occur on slopes greater than 50 <br />percent. <br />Table 7. Soil types and percentages within the project area. <br />Soil Type Acres Percent of Total <br />Footprint <br />Los Gatos-Los Osos complex, 30 to 75 percent slopes, eroded, Major Land <br />Resource Area 15 105.8 65.3% <br />Los Osos and Millsholm soils, 7 to 30 percent slopes 13.2 8.1% <br />Millsholm silt loam, 30 to 45 percent slopes, eroded 32.3 20% <br />Millsholm silt loam, 45 to 75 percent slopes, eroded 32.3 20% <br />Totals 161.9 100.0% <br />Source: NRCS 2025.
The URL can be used to link to this page
Your browser does not support the video tag.