TY - JOUR
T1 - Fire and alluvial chronology in Yellowstone National Park
T2 - climatic and intrinsic controls on Holocene geomorphic processes
AU - Meyer, G. A.
AU - Wells, S. G.
AU - Jull, A. J.T.
PY - 1995
Y1 - 1995
N2 - Fifty 14 C ages on fire-related events cluster within the intervals of 3300-2900, 2600-2400, 2200-1800, and 1400-800 yr BP and suggest earlier episodes of large fires and fan aggradation around 7500, 5500, and 4600-4000 yr BP. A major pulse of fire-related debris-flow activity between 950 and 800 yr BP coincided with the height of the widely recognized Medieval Warm Period (ca. AD 1050-1200). Instrumental climate records over the last ~100 yr in Yellowstone imply that the intensity and interannual variability of summer precipitation are greater during warmer periods, enhancing the potential for severe short-term drought, major forest fires, and storm-generated fan deposition. -from Authors
AB - Fifty 14 C ages on fire-related events cluster within the intervals of 3300-2900, 2600-2400, 2200-1800, and 1400-800 yr BP and suggest earlier episodes of large fires and fan aggradation around 7500, 5500, and 4600-4000 yr BP. A major pulse of fire-related debris-flow activity between 950 and 800 yr BP coincided with the height of the widely recognized Medieval Warm Period (ca. AD 1050-1200). Instrumental climate records over the last ~100 yr in Yellowstone imply that the intensity and interannual variability of summer precipitation are greater during warmer periods, enhancing the potential for severe short-term drought, major forest fires, and storm-generated fan deposition. -from Authors
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U2 - 10.1130/0016-7606(1995)107<1211:FAACIY>2.3.CO;2
DO - 10.1130/0016-7606(1995)107<1211:FAACIY>2.3.CO;2
M3 - Article
AN - SCOPUS:84879879220
SN - 0016-7606
VL - 107
SP - 1211
EP - 1230
JO - Geological Society of America Bulletin
JF - Geological Society of America Bulletin
IS - 10
ER -