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Pájaro River Watershed Flood Protection Plan - The Pajaro River ...

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parkway system that can be implemented with no or minimal outside funding.<br />

Graniterock has already demonstrated a willingness to propose such action<br />

and assisted our study through their generous sharing of their aerial survey<br />

data. If conservation easements or land trust arrangements can be<br />

implemented for parts of the upper <strong>Pájaro</strong> watershed in conjunction with<br />

these major landholders, this may facilitate faster completion of potential<br />

storage volumes. We can help to facilitate such planning and<br />

implementation.<br />

Suggested Enhancement Options for Upper <strong>Pájaro</strong> <strong>River</strong>:<br />

<strong>The</strong> Upper <strong>Pájaro</strong> <strong>River</strong>, along the Santa Clara-San Benito County line is<br />

fundamentally different than the San Benito <strong>River</strong>. Here a channel is incised<br />

up to 25 feet below the Lake San Benito lakebed, but because the riverbed<br />

has historically carried a reliable supply of influent groundwater, a dense<br />

finger of riparian forest characterizes most of the channel. This mature<br />

riparian forest of cottonwood, alder, maple, and willow has a dense woody<br />

instream fabric of logs and mid-channel growth, with a diverse pool structure.<br />

Although only 100 m wide in places, this riparian corridor provides high<br />

quality wildlife habitat and, apparently, allows anadromous fish passage into<br />

Llagas and Uvas creeks.<br />

Because the riparian forest is so dense and woody debris so prevalent, flood<br />

stages rise rapidly and go overbank onto the old San Benito lakebed. Local<br />

landowners report that flooding reaches the old lakebed level at a frequency<br />

of 10 years or less. Because of the high regional groundwater levels that<br />

seasonally saturate up to the lakebed silt cap, the soils of the area are<br />

classed as hydric and, unless cropped continually, revert to wetland<br />

conditions with emergent wetland plants. Farmers have constructed drainage<br />

channels across these lands to carry shallow groundwater and rainfall into<br />

the <strong>Pájaro</strong>.<br />

We were able to meet with local landowners and/or farm leaseholders. We<br />

learned that this Soap Lake area, just south of Gilroy, and situated along<br />

Highway 25 between Gilroy and Hollister, may be a target for extensive<br />

development. An ongoing effort sponsored through the <strong>Pájaro</strong> <strong>River</strong><br />

<strong>Watershed</strong> <strong>Flood</strong> Prevention Authority and AMBAG seeks to establish flood<br />

or conservation easements for the Soap Lake basin. Our sources suggest<br />

that the opportunity costs for development are so great that contiguous<br />

easements may be very difficult to obtain. While the site looks like marginal<br />

agricultural land used for little more than growing hay or grazing with small<br />

areas of row crops, it is in fact being leased back to local farmers and kept in<br />

agriculture as an interim holding pattern while development options are<br />

considered. If some of these lands would be wetlands were it not for<br />

continual agricultural use, then federal regulations will make it necessary to<br />

maintain agricultural uses or raise the lands or protect them with dikes and<br />

levees to permit non-agricultural uses. Should this be the case, a need for<br />

local fill may provide an opportunity to encourage landowners to excavate the<br />

3-foot deep lake-silt cap immediately adjacent to the river. This could<br />

increase the flood storage.<br />

DRAFT 7/22/03<br />

44<br />

<strong>Pajaro</strong> <strong>Watershed</strong> <strong>Flood</strong> Management

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