Riparian

Riparian zones are the outliers in the mostly dry Burton Mesa Ecological Reserve. Burton Mesa is a marine terrace topped by giant sand dunes.

A short geological digression:

The Santa Ynez block has been pushing northwards for the 20 million years, carried by the Pacific Plate. It contains the the Santa Ynez Mountains and its northern boundary is the hills just south of Lompoc. Northward pressure in the last few million years cause the land to fold and raise the Purisima Hills, just to the north of BMER, above the ocean floor. During a lull in this elevation a flat marine terrace formed by erosion. Prevailng north and west winds carried fine sand that dropped in the lee of the Purisima Hills, forming Burton Mesa. Little grains of quartz don't hold moisture, so most rainfall trickles down until stopped by the impermeable rocks of the oilfield. The dry dunes encouraged the development of chaparral and scrub plant communities. It also creates a perched water table that slowly leaks through canyons to reach the Santa Ynez River a few miles away.

I see three distinct riparian types:

The indigenous Chumash probably treasured these fresh water sources. But the plants were crucial to their culture.

Lake

overlook of the Hidden Lake from a hillside
Hidden Lake sits in a large bowl

Stream

TBD
Davis Creek flows south of Burton Mesa Road

Marsh

TBD
Cattails and arroyo willow in marsh at junction of Burton Mesa & Clubhouse Roads

Vernal Pool

tarweed in lateral ditch
Winter rains collect in this ditch just north of Oakhill Ave.