Yellowstone River Wetland/riparian Change Detection Pilot Study / Prepared By Gregory M. Kudray And Thomas Schemm 2006
Yellowstone River Wetland/riparian Change Detection Pilot Study / Prepared By Gregory M. Kudray And Thomas Schemm 2006
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High flows can also destroy wetlands by filling them with new sediment. River ice scour has also been recognized as an important factor in structuring woody vegetation in Montana's riparian areas (Smith and Pearce 2000) and probably affects other wetland types too.
Created structures affect wetlands but off-site impacts downstream were impossible to determine with our limited sample. The reduction of sediment with extensive rip-rap may affect wetlands as would streamlining channels for bridges ...or blocking river migration with levees.
Peak stream flow in the Yellowstone River has shown a pattern of relatively little alteration near Billings (Figure 4) compared to a steady decline in peak discharge over time downstream at Sidney (Figure 5). All photo series had fairly substantial peak flow events within five years of the photo year (Table 2). Large flows and ice movement likely scour vegetation and create Riverine bank and other wetlands.
USGS USGS 06214500 Yellowstone River at Billings MT L -P 0) u ■H 88866 78866 68866 ■^ o 58866 c U L •P to u 48866 38866 28866 o o o o o ' o
What to read after Yellowstone River Wetland/riparian Change Detection Pilot Study / Prepared By Gregory M. Kudray And Thomas Schemm 2006?
You can find similar books in the "Read Also" column, or choose other free books by Montana Natural Heritage Program to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
High flows can also destroy wetlands by filling them with new sediment. River ice scour has also been recognized as an important factor in structuring woody vegetation in Montana's riparian areas (Smith and Pearce 2000) and probably affects other wetland types too.
Created structures affect wetlands but off-site impacts downstream were impossible to determine with our limited sample. The reduction of sediment with extensive rip-rap may affect wetlands as would streamlining channels for bridges ...or blocking river migration with levees.
Peak stream flow in the Yellowstone River has shown a pattern of relatively little alteration near Billings (Figure 4) compared to a steady decline in peak discharge over time downstream at Sidney (Figure 5). All photo series had fairly substantial peak flow events within five years of the photo year (Table 2). Large flows and ice movement likely scour vegetation and create Riverine bank and other wetlands.
USGS USGS 06214500 Yellowstone River at Billings MT L -P 0) u ■H 88866 78866 68866 ■^ o 58866 c U L •P to u 48866 38866 28866 o o o o o ' o
What to read after Yellowstone River Wetland/riparian Change Detection Pilot Study / Prepared By Gregory M. Kudray And Thomas Schemm 2006?
You can find similar books in the "Read Also" column, or choose other free books by Montana Natural Heritage Program to read onlineMoreLess
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