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Glaciers in sunny California? Many people will be surprised to learn that there are several hundred in this state, ranging in size from the impressive Whitney Glacier on Mt. Shasta and the Palisade Glacier in the Sierra Nevada to tiny glacierets. While California's glaciers are small compared to those in the northern Rockies or the European Alps, each one is interesting and some are suitable for exploring. Also of note is the fact that Ice Age glaciers carved California's most spectacular mountain scenery—the High Sierra was glaciated several times and glacial landforms are prominent features of the Sierran landscape today. Bill Guyton summarizes the history of the discovery of Ice Age glaciation and modern-day glaciers in California, as well as the development of modern ideas about the state's glacial history. He describes the controversy about the origin of Yosemite Valley and quotes from the colorful accounts of early mountain explorers such as John Muir, Josiah Whitney, and François Matthes. His book provides a primer on glaciers and glacial landforms, a glossary of technical terms, helpful illustrations, and a 100-mile Sierra field trip guide for readers who want to see glaciers and glacial features for themselves. Glaciers of California will make any visit to the mountains more interesting, whether one is carrying a camera, crampons, or a fishing pole.
This book reviews advances in understanding of the past ca. two million years of Earth history - the Quaternary Period - in the United States. It begins with sections on ice and water - as glaciers, permafrost, oceans, rivers, lakes, and aquifers. Six chapters are devoted to the high-latitude Pleistocene ice sheets, to mountain glaciations of the western United States, and to permafrost studies. Other chapters discuss ice-age lakes, caves, sea-level fluctuations, and riverine landscapes. With a chapter on landscape evolution models, the book turns to essays on geologic processes. Two chapters discuss soils and their responses to climate, and wind-blown sediments. Two more describe volcanoes and earthquakes, and the use of Quaternary geology to understand the hazards they pose. The next part of the book is on plants and animals. Five chapters consider the Quaternary history of vegetation in the United States. Other chapters treat forcing functions and vegetation response at different spatial and temporal scales, the role of fire as a catalyst of vegetation change during rapid climate shifts, and the use of tree rings in inferring age and past hydroclimatic conditions. Three chapters address vertebrate paleontology and the extinctions of large mammals at the end of the last glaciation, beetle assemblages and the inferences they permit about past conditions, and the peopling of North America. A final chapter addresses the numerical modeling of Quaternary climates, and the role paleoclimatic studies and climatic modeling has in predicting future response of the Earth's climate system to the changes we have wrought.
Paleoecological research was undertaken in the central Sierra Nevada to determine the postglacial environmental history of regions which today support montane mixed conifer forests. Six lake sites were selected for study. The sites are ecologically similar to one another, and are situated near the maximum extent of Tioga glaciation at elevations between 1800-2000 meters. Pollen, macrofossils, and microscopic charcoal were analyzed to develop a regional environmental history based on comparison of the local records.