San Elijo Lagoon is formed in a drowned river mouth. Approximately 150 feet of alluvial clay and silts underlay the lagoon basin. Steep bluffs border the lagoon basin and lower reaches of Escondido Creek. These bluffs are composed of tertiary marine sediment deposits of sand, shale and sandstone. The marine sediment formations are predominately Del Mar and Torrey sandstone (from the Mid-Eocene period - 47 million years ago) topped by Linda Vista red sandstone (from the Pliocene-Pleistocene period- 1.6 million years ago). Between 5,000 and 18,000 years ago a period of glacial extremes created ocean level approximately 400 feet below current levels. During the past 1,500 years, the sea level has been relatively stable, although regional studies on the effects of global warming indicate that sea level can be expected to rise by 2-3 ft. during the next 100 years. Highway 101, the San Diego Northern Railway (SDNR) and
Interstate 5 divide the lagoon into three basins connected by narrow channels.
The west basin, the area between the Pacific Coast Highway (101) and the
railroad, contains 45acres of wetlands that form a series of four to five ponds.
The central |
• Created by:
Maider Veschembes & Amy Slater
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