THE LAB
The mission of the laboratory is to conduct environmental research to further our understanding of past and present physical landscapes and to promote student education and research. The lab emphasizes sediment research and tree-ring research.
LAB EQUIPMENT
Sedimentology Equipment
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Livingstone-type piston corer with 50of extension rods |
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1.6 cubic ft lab oven |
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127.5 cubic in muffle furnace |
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Analytical balance with 0.1 mg readability |
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10-45X stereo microscope |
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Compound microscope with 10X, 40X, and 100X objectives |
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Bartington MS2 magnetic susceptiblity meter |
Dendrochronology Equipment
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10", 14”, 16”, and 20” Haglof tree increment borers |
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24” Travel Velmex Measurement System with 0.001 mm Accu-Rite readout |
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10-40X Stereozoom binocular microscope with boom-arm and fiber optic illuminator |
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Voortech Measurement Software |
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16" Solo chain saw and accessories |
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Bosch 3" X 21" belt sander |
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Bosch oscillating sander |
ABOUT SEDIMENTOLOGY
Sedimentology is concerned with the use of lake and marsh deposits in reconstructing past environments. Layers of lake sediment can accumulate undisturbed over long periods of time, forming a repository of information about changing environmental conditions. When carefully collected and examined, these layers can be read like pages in a book describing the environmental history of a region. Sediment characteristics such as grain size, organic content, magnetic susceptiblity, and elemental composition give insight into past climate and erosion in a watershed. The study of microfossils in lake sediments, such as pollen and charcoal, allows for the reconstruction of regional vegetation patterns and fire frequencies. Continuous sediment records spanning time periods from decades to hundreds of thousands of years have been used to study changing environments around the world.
CURRENT SEDIMENT RESEARCH PROJECTS
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Klamath Mountains |
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Western Basin and Range |
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California Coast Ranges |
ABOUT DENDROCHRONOLOGY
The science of dendrochronology is based on the doctrine that the "the past is the key to the future." By evaluating annual growth rings of suitable tree species we are given a glimpse of past environmental conditions. Knowledge of past environments helps us to better understand the environments in which we currently live and how these environments may change in the future. By evaluating changes in annual growth rings dendrochronologists are able to create records of environmental change that may extend back hundreds or even thousands of years. Tree rings have been used to study population dynamics of forests, volcanic eruptions, the rise and fall of ancient cultures, changes in insect and fish populations, earthquakes, tsunamis, river flow, atmospheric and soil pollution, deception in art masterpieces, radiocarbon dating, sunspots, and more. To learn more about the intriguing art and science of dendrochronology go to the Ultimate Tree Ring Pages . CURRENT TREE-RING RESEARCH PROJECTS
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Tehachapi Mountains |
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Sierra Nevada Mountains |
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Northern Nevada |
Lab Directors:
Bruce Gervais
James Wanket
Department of Geography
California State University, Sacramento
6000 J Street
Sacramento , California 95819-6003
916 .278.6109; fax 916.278.7584 |