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Explore effects of mass movements on tree growth, dating impact scars, and analyzing geomorphic processes. Witness reactions like reaction wood in hardwoods and conifers. Discover consequences of global cooling post-volcanic eruptions and tree-ring dating in glaciology.
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Applications in Geomorphology:Mass Movements Mudflow causing trees to fall and lean. Effects of geomorphic processes on tree growth Digging out a tree buried by adjacent hillside erosion, Milledgeville, central Georgia.
Applications in Geomorphology:Mass Movements Impact Scars can be dated.
Applications in Geomorphology:Mass Movements Impact Scars can be dated. Impact scars from ice flows/jams. Effects of a snow avalanche on a white spruce.
Applications in Geomorphology:Mass Movements Impact Scars can be dated.
Applications in Geomorphology:Mass Movements Reaction wood: Conifers form compression wood in response to leaning and flagging. Deciduous trees form tension wood in response to leaning.
Applications in Geomorphology:Mass Movements Hardwoods PUSH Conifers PULL
Applications in Geomorphology: Volcanology Effects of global-scale cooling caused by a volcanic eruption in AD 536, as seen in a Siberian pine from Mongolia. Which is the frost ring?
Applications in Geomorphology: Volcanology Effects of global-scale cooling caused by a volcanic eruption ca. 1627 BC, as seen in a bristlecone pine. Which is the frost ring?
Applications in Geomorphology: Hydrology Effects of a 1945 flood on growth of a ponderosa pine, Pine Canyon, Chiricahua Mountains, Arizona.
Applications in Geomorphology: Hydrology Changes in hydrologic properties of an area.
Bank erosion causing conifer trees to lean along the Sheepscot River in Maine.
Applications in Geomorphology: Glaciology A. Radiocarbon dates
B. Tree-ring datesof glacial advances Applications in Geomorphology: Glaciology
Applications in Geomorphology: Glaciology Tree-ring dated moraines