Lake Elsinore

The Lake Elsinore is a natural freshwater lake in Riverside County in the U.S. state of California, on the edge of the Santa Ana Mountains. Its most important tributary is the San Jacinto River.

The lake was originally named by the Spanish conquistadors Laguna Grande, before he was named after the town of Elsinore bank as Lake Elsinore. The city, in turn, is today named as Lake Elsinore even after the lake.

Geography

The Lake Elsinore is the largest freshwater lake in Southern California. It is the lowest place in the 1900 km ² large catchment area of ​​the San Jacinto River, which flows into Lake Elsinore.

Politically, the Lake Elsinore is part of the Riverside County, California. The lake with the same name City Lake Elsinore and Lakeland Village two shore towns.

Limnology

Located at an altitude of 379 m, the lake usually fills of 12.1 km ². However, due to floods and droughts, the level can vary significantly; as the Lake Elsinore may also cover 14 km ² under given conditions. Normally, the lake measures 9.7 km in length and 2.4 km in width. The circumference is 23 km. On average, the lake holds 51.4 million square meters of water. Its maximum depth is 13 m.

Out of the lake of Temescal Creek runs. At higher water level of the lake leads him off excess water. The Temescal Creek flows into the Santa Ana River.

The lake lies in a basin that is bounded on the west and south-west of the Elsinore Mountains, so make the lake a endorheisches waters dar. the northwest its shores bordered by the foothills of the Elsinore Mountains. From here hills continue until the West Bank where the elevations are less. At the mouth of the San Jacinto River, the Lake Elsinore Basin opens. From the lake itself, this pool is completely cut off by a seawall, which may only be opened at extreme high water to discharge to the lake. The Lake Elsinore Basin is the furthest northwest end of the wine region Temecula Valley AVA. The Santa Margarita River is flowing there cut off a small survey south of the lake from this.

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