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About the Tujunga Watershed
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Overview
The Tujunga is the largest subwatershed of the upper Los Angeles River
Watershed. The 225-square mile area comprises both remote open space of
the Angeles National Forest, and the highly urbanized lands of the cities
of Los Angeles & San Fernando. The watershed has a very steep slope
- the high elevations of the San Gabriel Mtns. (above 7100 ft.) in the
upper watershed drop rapidly to the valley floor at an average rate of
41 ft/mile. Dozens of blue line streams feed the three main tributaries
– the Big Tujunga, Little Tujunga, and Pacoima Washes. Since the
mountains are geologically young and highly dynamic, its waterbodies are
a “young” stream system. Big and Little Tujunga Wash come
together in the Hansen Dam Reservoir. Below Hansen Dam, Pacoima Wash joins
the channelized concrete box Tujunga Wash as it flows to its confluence
with the Los Angeles River in Studio City.
Geomorphology
The mountains of the upper watershed are historically prone to episodic
fires, common to the chaparral plant communities that dominate the southern
slopes, with fire frequency intervals estimated between 20-100 years.
A fire history computed for the Tujunga watershed estimated that 95 percent
of the watershed may have burned during the period 1878-1975. In the post-fire
scenario, runoff and erosion increase significantly. Additionally, frequent
activity along the numerous fault lines within the San Gabriel range can
increase the amount of fractured bedrock available for sediment transport
by large storms. Prior to the engineering and channelization of the regions
rivers and streams, these washes formed a network of as many as five wide,
alluvial channels across the eastern valley. What this meant to the history
of the Valley in real terms was that nutrient-rich soils were being deposited
across the valley, making it ideal for agriculture.
Water
Historically, the Tujunga Wash was a major contributor of groundwater
supply. The Valley sits atop the San Fernando Groundwater Basin - a huge
aquifer that has become depleted over the years as we have made the valley
floor impervious. Rain that used to soak into the ground now runs off
of concrete and asphalt and directly into the stormdrains, and our channellized
washes and river.
Although Los Angeles averages only 15 inches of annual rainfall, the
higher elevations of this watershed receive some of the most concentrated
rainfall in the United States. The depleted basin currently provides nearly
15% of local drinking water supplies to Los Angeles. Prior to the channelization
of our river systems and the subsequent intense development, roughly 80%
of stormwater percolated to groundwater. Current estimates are that around
8% percolates, the rest being lost to the ocean via the channelized river
system carrying contaminants from urbanized land use. Approached from
a watershed context, the Tujunga Watershed provides significant opportunities
to maximize recharge, optimize reuse, improve water quality, and reduce
reliance on imported water.
Habitat
Habitats include alluvial fan scrub, riparian woodland, willow thicket,
mulefat scrub, coastal sage scrub, oak woodland and conifer woodland forests.
These habitats currently provide critical cover, forage, nesting and breeding
sites for many bird, mammal, reptile, amphibian and invertebrate species.
The area supports several threatened and endangered species listed for
Los Angeles County, including California Condor, spotted owl, Least Bell’s
Vireo, southern willow flycatcher, American peregrine falcon, arroyo toad,
slender-horned spineflower, California red-legged frog, Santa Ana sucker,
unarmored threespine stickleback, and arroyo chub.
Communities
The watershed includes the City of San Fernando as well as the communities
of Pacoima, Arleta, Sylmar, Sunland, Tujunga, Panorama City, Van Nuys,
North Hollywood, Valley Glen, Valley Village & Studio City within
the City of Los Angeles. The watershed has a population of nearly 500,000,
is roughly 62% Latino with 32% of the population under the age of 17 and
19% living in poverty.
Infrastructure
The watershed contains numerous facilities, including Big Tujunga &
Hansen Dams; Pacoima & Tujunga Reservoirs; Hansen & Lopez Flood
Control Basins; Tujunga Gallery, Tujunga, Pacoima, Hansen, Branford, Spreading
Grounds; numerous small debris basins and sediment retention sites. In
addition, four gravel mining operation areas and a power generating station
occur within the watershed boundary. Transportation corridors include
Interstates 5, 405 & 210, and Highways 170, 101,118 and 14. Metrolink
and Amtrak lines and the Metro Rapidway dedicated bus corridor cross the
lower watershed. The Metrolink corridor is heavily industrialized.
Open Space
The upper watershed encompasses more than 100 square miles of the Angeles
National Forest and a large regional recreation area behind Hansen Dam.
The lower watershed is extremely park-poor but includes vacant lots that
could support opportunities to provide much-needed open space to economically
disadvantaged minority communities that have been adversely impacted by
past resource management decisions. Along the easement adjacent to the
box channel sections, good opportunities exist for green corridors that
could include bike paths, walking areas, small pocket parks and stormwater
retention areas. In addition, with some minor modifications to Dam and
Spreading Grounds operations, along with utilization of some measure of
storage at one of the gravel pits, the possibility exists to remove the
concrete armoring of the mainstem channels of Tujunga and Pacoima Washes,
thereby restoring natural processes and functions while providing for
habitat restoration all along both washes.
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For More Information
You can learn more about the Tujunga Watershed and watershed processes,
like flooding, in two ways:
Select places on a map
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