Southwest San Timoteo GSA - 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO
Southwest San Timoteo GSA - 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO
A. Applicant Information
Requesting Agency Information
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Agency Name: | Southwest San Timoteo GSA | ||
Address: | 2270 Trumble Road | ||
City: | Perris | Zip: | 92572-8300 |
Work Phone: | 951-9283777 | Cell Phone: | |
Email: | grayr@emwd.org | Fax: |
Revision Request Manager Information
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Person Name: | Rachel Gray | ||
Address: | 2270 Trumble Road | ||
City: | Perris | Zip: | 92572-8300 |
Work Phone: | 951-928-3777 | Cell Phone: | |
Email: | grayr@emwd.org | Fax: |
B. Description of Proposed Boundary Modification
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EMWD requests a basin boundary modification of the DWR Bulletin 118 Subbasin No. 8-002.08, the San Timoteo Groundwater Subbasin (Basin), based on scientific (external) justification to better represent the local groundwater aquifer conditions.
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- Scientific External
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The modification request is to eliminate areas of the existing Basin that lack viability and/or contribution to the local groundwater aquifer system. This boundary modification addresses areas of permeable materials capable of providing significant quantities of groundwater to wells and areas comprised of well-consolidated, Tertiary bedrock that should be excluded from the groundwater basin based on DWR's definition of a Quaternary groundwater basin. The proposed Basin boundary will coincide with the surface extent of unconsolidated young alluvium, old alluvium, alluvial fan, valley fill deposits, and other geologic formations having well understood and documented groundwater significance as mapped by the California Geological Survey (CGS). The proposed modification will not impact the sustainable management of the Basin because the areas identified for removal do not provide a significant source of water nor significant volumes of groundwater and there is no current or planned use for these areas that would constitute a significant contribution to water resources (Attachment B1). The Basin is the source of water supply for multiple purveyors (Attachment B2). The main production area is the adjudicated portion of the Basin identified by DWR in the basin prioritization released in 2018. The Beaumont Basin Watermaster actively manages the adjudicated portion of the Basin. The northeastern portion of the Basin (unadjudicated area) was previously managed under the San Timoteo Watershed Management Program implemented in 2005 prior to the passing of SGMA in 2014. This portion of the Basin is currently managed by the San Timoteo GSA and was classified as a very low priority basin (DWR, 2018).
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- 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO
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There are no new proposed basins. After proposed boundary revisions, a single Subbasin name 8-002.08 San Timoteo will remain.
C. Initial Notification and Combination of Requests
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Yes
Local Agency Potential Basin(s)/Subbasin(s) Yucaipa Valley Water District 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO Beaumont-Cherry Valley Water District 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO Eastern Municipal Water District 8-002.08 UPPER SANTA ANA VALLEY - SAN TIMOTEO -
No
D. Required Documents for All Modifications






This request is not a project as defined in the California Environmental Quality Act Code of Regulations, Title 14, Chapter 3, Section 15378.
E. General Information

The Basin underlies Cherry Valley and the City of Beaumont in southwestern San Bernardino and northwestern Riverside Counties. It is bounded to the north and northeast by the Banning fault and impermeable rocks of the San Bernardino Mountains, Crafton Hills, and Yucaipa Hills, on the south by the San Jacinto fault, on the west by the San Jacinto Mountains, and on the east by a topographic drainage divide with the Colorado River Hydrologic Region. The surface is drained by Little San Gorgonio Creek and San Timoteo Canyon to the Santa Ana River.
Holocene age alluvium, which consists of unconsolidated clay, silt, sand, and gravel, is the principal water-bearing unit in this Basin. The alluvium, which is probably thickest near the City of Beaumont, thins toward the southwest and is not present in the central part of the Basin (DWR, 2003). The San Timoteo Formation, located in the southwest portion of the Basin, consists primarily of well-consolidated, Tertiary sandstone and conglomerate. The geologic description of the San Timoteo formation is as follows:
Dominant lithology is light-gray, pebbly to cobbly, moderately to well-indurated, medium- to coarse-grained sandstone containing conglomerate beds up to 9 meters in thickness. Pale brown- to light-gray fine-grained sandstone; pebbly sandstone is subordinate. Overall, member consists of about 70 percent sandstone and 30 percent conglomerate; conglomerate more abundant in upper part. Includes numerous reddish-brown stratigraphic intervals consisting of oxidized sandstone, which are not paleosols, and reddish brown clay-rich intervals, which may be paleosols. Erodes to form sharp-ridged badlands topography. In eastern part of quadrangle, forms hogbacks on south side of San Timoteo Canyon. Included within the San Timoteo Formation (Tstm) is highly deformed, fault-bounded sandstone, pebbly sandstone, and conglomerate (Tstd) located along western part of badlands adjacent to Claremont Fault (Morton, 1999).
F. Notice and Consultation

San Gorgonio Pass Water Agency
Yucaipa Valley Water District
Beaumont-Cherry Valley Water District
South Mesa Water Company
Banning Water District
City of Redlands Water
City of Beaumont Water
Beaumont Basin Watermaster
City of Calimesa
City of Beaumont
City of Banning
City of Redlands

On May 14, 2018, the San Timoteo Sustainable Groundwater Management Agency held a meeting at San Gorgonio Pass Water Agency during which the basin boundary modification for the San Timoteo Groundwater Basin was discussed. On May 23, 2018, EMWD discussed technical comments with the members of the San Timoteo GSA for the San Timoteo Groundwater Basin boundary modification.

EMWD informed the San Timoteo GSA of the San Timoteo Groundwater Basin boundary modification request (southwestern portion of the Basin). Several technical discussions were held to resolve comments regarding the boundary modification. A consultation was held with the California Department of Water Resources, Southern Section on May 29, 2018.

The San Timoteo Groundwater Basin boundary modification was discussed at the EMWD's Board of Directors meeting on June 20, 2018.

No comments were received apart from the comments discussed during the technical meetings with members of the San Timoteo GSA.
H. Local Support
All requests for boundary modification must include the following:

On May 14, 2018, the San Timoteo Sustainable Groundwater Management Agency held a meeting at San Gorgonio Pass Water Agency during which the basin boundary modification for the San Timoteo Groundwater Basin was discussed. On May 23, 2018, EMWD discussed technical issues with the members of the San Timoteo GSA for the San Timoteo Groundwater Basin boundary modification request.

EMWD's Board of Directors adopted a Resolution (2018-083) initiating the San Timoteo Groundwater Basin boundary modification.

None submitted.
I. Hydrogeologic Conceptual Model
Requests for boundary modification, must include a document or text to a clearly defined hydrogeologic conceptual model demonstrating each of the following:

The San Timoteo Formation is composed primarily of sandstone, conglomerate, siltstone, and mudstone (Rewis, et al., 2007). The igneous and metamorphic rocks form the crystalline basement rocks in the area (Bloyd, 1971). The unconsolidated Quaternary alluvium, and the upper portion of the underlying San Timoteo Formation, constitutes the water-bearing aquifer of the Beaumont Basin (Rewis, et al., 2007). The San Timoteo barrier separates the lower San Timoteo Canyon area from the main part of the San Timoteo-Beaumont basin (USGS, 1972). There are three significant drainage systems that overlie the Beaumont Basin: the San Timoteo Creek drainage which is tributary to the Santa Ana River; the Potrero Creek drainage system in the San Jacinto watershed; and the Smith Creek drainage system tributary to the White Water River which is part of the Salton Sea drainage basin. Surface water flows originate in the San Bernardino Mountains to the north of the Basin (ALDA, 2013).
Attachment I1 - Ground-Water Outflow, San Timoteo-Smiley Heights Area Upper Santa Ana Valley, Southern California 1927 through 1968. February 9, 1972.
Attachment I2 - DWR Bulletin 118 Upper Santa Ana Valley Groundwater Basin, San Timoteo Subbain
Attachment I3 - Existing San Timoteo Subbasin Geologic Map
Attachment I4 - Engineer's Report No. 3 2008-2011
Attachment I5 - Second Report Of Recharge Parties Pursuant To RWQCB Resolution No. R8-2008-0019 Cooperative Agreement To Protect Water Quality And Encourage The Conjunctive Uses Of Imported Water In The Santa Ana River Basin, Yucaipa And San Timoteo Management Zones
J. Technical Studies for External Scientific Modifications
Requests for a scientific modification must include a document containing information that demonstrates the extent of the aquifer. Provide the following:

Attachment J1 - San Timoteo Basin 8-002.08 Geologic Map
Attachment J2 - Proposed New San Timoteo Basin 8-002.08 Boundary Geologic Map

The hydrogeology of the Basin was analyzed by reviewing data presented in the technical documents listed below and included in Section I. Justification for the modification is presented in Attachments J3 and J4.
Attachment J3 - San Timoteo Groundwater Basin Boundary Modification Justification
Attachment J4 - San Timoteo Groundwater Basin Boundary Modification Justification Maps
Attachment J5 - Conceptual Understanding and Groundwater Quality of Selected Basin-Fill Aquifers
Attachment J6 - 2013 Reevaluation of the Beaumont Basin Safe Yield