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Natural History

Bordered on the east by the high Sierra Nevada and separated from the Pacific Ocean by the Coast Range mountains, the San Joaquin Valley is 250 miles long and 50 miles wide, and the flat, open landscape includes parts of eight counties.

The San Joaquin River, the Valley’s namesake, runs the length of the region north from the Tulare Lake Basin. This river is fed by the Merced, Tuolumne, Stanislaus, Mokelumne and Cosumnes rivers. Dams and reservoirs for agricultural irrigation and domestic drinking water suppplies have dramatically reduced the natural flow of the San Joaquin River and its tributaries.

As of 2011, 3.9 million people and more than 100 ethnic groups live in the San Joaquin Valley. According to the California Department of Finance, the population will increase 131 percent by 2050 – the fastest increase in the state. Much of the Valley’s population is clustered in major cities, many dating from the late 1800s when they sprang up during construction of the Central Pacific Railroad. Those communities — Stockton, Modesto, Merced, Fresno and Bakersfield — are part of a string of urbanization along Highway 99, the region’s major intercity corridor. The population here is 5 percent younger than the state average.

The Merced Vernal Pools & Grassland Reserve sits at the edge of urbanization and agricultural fields, about five miles from downtown Merced.

Eastern Merced County includes a remarkably intact section of an alluvial terrace landscape formed along the western base of the Sierra Nevada. At first glance, the region and the site appear to consist of a relatively homogeneous mix of annual grasslands and vernal pools distributed across undulating slopes and occasional low hills. However, on more careful study, one finds this landscape to be quite varied in its soils, geology, and biology. Taken as a whole, this region can provide us with insight into the physical genesis and evolutionary history of a large region of California, including areas well beyond the boundaries of eastern Merced County.

 

Climate

The grasslands of eastern Merced County occur within a region where only about 13 inches of rain falls during the cool part of the year (November through May).

 

Geology

Eastern Merced County includes a remarkably intact section of an alluvial terrace landscape formed along the western base of the Sierra Nevada. Vernal pools are still found in widely-scattered areas throughout California, but they reach their greatest density and development on the alluvial terraces formed along the base of the Sierra Nevada foothills. Here, the landscape and weather are ideal for their development. Other uniquely characteristic habitats within this terrace landscape region include volcanic and sandstone rock outcrops, seasonally inundated clay flats, and certain geologically influenced microhabitats within the annual grasslands. The Vernal Pools & Grassland Reserve is characterized by unique globally-significant habitats that create important opportunities for teaching and research.

References on geological history of the Merced Fan, the Cherokee Terrace, & the eastern Great Valley (courtesy of Bob Holland)

 

Hydrology

The site lies within the watersheds of the Black Rascal, Fahrens, and Cottonwood creeks, which flow generally southwest to Bear Creek and the San Joaquin River. The San Joaquin River, the Valley’s namesake, runs the length of the region north from the Tulare Lake Basin. This river is fed by the Merced, Tuolumne, Stanislaus, Mokelumne and Cosumnes rivers. Dams and reservoirs for agricultural irrigation and domestic drinking water supplies have dramatically reduced the natural flow of the San Joaquin River and its tributaries.

 

Soils

Some of the oldest soils in North America (the China Hat soil formation) are found in the high regions to the northeast.

 

Ecosystems

The most striking habitats within the Reserve are the vernal pools. As seasonally inundated wetlands, the vernal pools require specific combinations of geology, soils, slope, and climate to exist. The entire area encompasses one of the largest, least fragmented vernal-pool-grassland environments in the state, and possibly the nation. Some of the largest and most diverse sets of vernal pools found anywhere in California occur in this area. The area is defined by hundreds of small watersheds that support and create a dense vernal-pool complex, including the habitat for the extremely rare Conservancy Fairy Shrimp (Branchinecta conservatio).

Past and Present Distribution, and Physical and Biological Considerations Characterization and Global Distribution of Vernal Pools

The Plants, Animals, and Ecosystems – Ecology and Systematics, Status and Trends

Conservation and Management

 

Ecology, Conservation, and Management of Vernal Pool Ecosystems

Proceedings from a 1996 Conference

Table of Contents

Foreword

By Michael G. Barbour

Introduction

By Carol W. Witham