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Physical Science Though a relatively small area, Cabrillo National Monument is geologically and topographically diverse. The monument rises 400 feet above sea level. Three predominant formations comprise the monument and are sedimentary in nature. The Cretaceous Point Loma Formation is the oldest and extends from northern Baja California to Carlsbad, California. Rich in marine fossils, it is an excellent example of a late-Cretaceous marine environment. Superimposed on the Point Loma Formation, the Cabrillo Formation is composed of terrestrial deposits ranging from sandstone to boulder conglomerates indicative of braded river deposits. The younger Pleistocene Bay Point Formation is a poorly cemented sandstone structure that is indicative of a near shore marine environment. This formation forms the coastal marine terraces on both sides of the peninsula. The Pleistocene Bay Point Formation offers opportunities for geomorphologic studies because of its slope instability. Cabrillo National Monument offers many opportunities to study the effects of human populations on Mediterranean climate, water, air quality, soils, erosion, storm runoff, and other physical science related issues that impact park management. and visitation because of its proximity to San Diego. Additionally, the Mediterranean Climate and the unique physiography of the monument allows for the study of interactions between the ocean, and tidal environments, San Diego bay, and the surrounding terrestrial environments.
Current Research
Impacts on rocky intertidal communities
Effects of habitat fragmentation on the Greater Roadrunner
Monitoring turf trampling of coastal invertebrates
Research Opportunities
Baseline geologic and geomorphic inventories and mapping
Synthesis of existing data to assess trends in air or water quality and changes in hydrology
Tactical or long-term monitoring studies
Evaluation and prediction of geologic hazards
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