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