My WebLink
|
Help
|
About
|
Sign Out
PC-2025-16
City of Pleasanton
>
BOARDS AND COMMISSIONS
>
PLANNING
>
RESOLUTIONS
>
2020 - PRESENT
>
2025
>
PC-2025-16
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
12/23/2025 10:30:44 AM
Creation date
12/23/2025 10:28:35 AM
Metadata
Fields
Template:
CITY CLERK
CITY CLERK - TYPE
RESOLUTIONS
DOCUMENT DATE
7/23/2025
DESTRUCT DATE
PERMANENT
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.
/
277
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).
Show annotations
View images
View plain text
ENGEO <br /> INCORPORATED <br /> <br /> <br />5150.100.101 <br />March 31, 2008 2 <br />The site is located on the west side of Foothill Road and the south side of Dublin Canyon Road in <br />Pleasanton, California, as shown on the Vicinity Map, Figure 1. The property is situated on a <br />north-facing slope that has been partially graded as a cut slope adjacent to Dublin Canyon Road. <br /> <br />The site is currently open space and vegetation consists of open grass land. Existing improvements <br />are limited to an asphalt-paved road that services existing residences upslope of the site and a <br />concrete-lined V-ditch. <br /> <br />Proposed Development <br /> <br />Conceptual development plans indicate that the site will be developed with a restaurant building and <br />associated parking areas. The location of the proposed building and parking areas are shown on the <br />attached Figure 2. The project will include a substantial amount of grading and construction of <br />retaining walls. <br /> <br />Regional Geology <br /> <br />The site is located in the Coast Ranges geomorphic province of California. In this part of the <br />province, bedrock is mapped as Miocene marine sedimentary sandstone by Dibblee (1980) and <br />Graymer (1996). The geologic setting of the site is depicted on the attached Regional Geologic Map, <br />Figure 3. <br /> <br />Regional bedrock structure is mapped by Dibblee (1980) striking to the northwest and dipping at <br />inclinations of about 65 to 75 degrees to the southwest. <br /> <br />Mapped Faulting <br />
The URL can be used to link to this page
Your browser does not support the video tag.