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Chapter 3 - Natural Resources - Marine Corps Base Camp Pendleton

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MCB <strong>Camp</strong> <strong>Pendleton</strong>, California<br />

3.1.4.1. Watersheds<br />

Mountain ranges divide the <strong>Base</strong> into seven watersheds or drainage areas (Figure 3-2) and<br />

(Table 3-1): San Mateo, San Onofre, Coastal Drainage, Las Flores, Aliso, Santa Margarita,<br />

and San Luis Rey. The Las Flores watershed is often divided into two sub-watersheds, the<br />

Las Pulgas Canyon and Piedra de Lumbre Creek. The Coastal Drainage is located north<br />

and south of Las Flores Creek watershed. The San Luis Rey River drains the southern<br />

portion of the <strong>Base</strong> into the ocean just south of the <strong>Base</strong>.<br />

The largest drainage, the Santa Margarita, is 742 square miles (474,880 ac). Over 90% of<br />

this watershed is located off <strong>Base</strong>. De Luz Creek is an important tributary to the Santa<br />

Margarita, and provides a significant quantity of water from off <strong>Base</strong>. Aliso Creek, Coastal<br />

Drainage (Horno Creek, French Creek, Cocklebur Creek, Hidden Creek), Las Flores (with<br />

tributaries Las Pulgas and Piedra de Lumbre), and San Onofre (with its Jardine Canyon<br />

tributary) are watersheds that are completely on <strong>Camp</strong> <strong>Pendleton</strong> and drain into the Pacific<br />

Ocean. San Mateo Creek drainage (with tributaries Cristianitos and Talega), includes areas<br />

of the Cleveland National Forest, San Onofre State Park, the City of San Clemente, and<br />

other private lands.<br />

The two largest watersheds on <strong>Base</strong>, Santa Margarita and San Mateo, form broad alluvial<br />

plains as they approach the Pacific Ocean. As the streams reach the sea, sloughs or<br />

estuarine lagoons form due to sand bars or narrow tidal barriers. These impound low<br />

stream flows, but are breached during high-flows caused by storm events and normal tidal<br />

fluctuation. <strong>Base</strong>d on water quality data, measurements, and observations for the Santa<br />

Margarita River Estuary, incoming tides are generally able to top the sandbar once or twice<br />

a day, while a small natural channel in the sandbar allows water to drain back out when the<br />

water level of the outgoing tide falls below the elevation of sand accumulated on the<br />

sandbar (Entingh pers. comm. 2009). The sandbar blockages subsequently reform by<br />

sedimentation and normal wave action. Gage height data for the SMR estuary indicates that<br />

the sandbar at the mouth of the estuary only isolates the estuary from the Ocean for<br />

approximately 25% of the time annually (Leedshill-Herkenhoff 1989).<br />

The three largest estuaries on the <strong>Base</strong> are situated at the mouths of the Santa Margarita,<br />

Las Flores, and San Mateo streams. Review of USGS data for the period October 2007 –<br />

September 2008, indicates that the Santa Margarita River, Aliso Creek, and Hidden Creek<br />

estuaries are tidally influenced while the San Onofre and San Mateo estuaries are<br />

predominately isolated from the Ocean. The Cockleburrr and Las Flores estuaries are<br />

somewhere in-between (Entingh pers. comm. 2009).<br />

3-4 <strong>Chapter</strong> 3 – <strong>Natural</strong> <strong>Resources</strong>

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