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Wetland Classification and Mapping of the Kenai Lowland, Alaska
Map Unit Descriptions Ecosystem: Riparian Map Unit: Rea; Reac
Extent: 237 wetland polygons; 1936.9 ha; 1.37% of wetland area; 1.44% of wetland polygons. |
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![]() A short-run Rea stream in the City of Kenai (polygon 8602). |
Wetland Indicators Type: Stream Average depth to water table: 25.4 cm; n=9 Organic layer thickness: 67.2 cm; n=9 Average depth to redoximorphic features: 20.0 cm; n=2 Common Soils: STARICHKOF, TRUULI, SLIKOK, TLIKAKILA, NIKOLAI Common Plant communities: Barclay's willow / Bluejoint - Field horsetail Barclay's willow / Bluejoint / Marsh fivefinger
NWI: Stream: R2US3,4. Valley wetlands: PSS1J HGM: Stream: Low Gradient Natural Stream-single thread. Valley wetlands: Lotic Slope groundwater-dominated Throughflow/Bidirectional-nontidal. |
| Accuracy assessment: 34 polygons interpreted as Rea on aerial photographs were field checked. 24 remained Rea; 3 were revised to RB; 1 each was revised to: DW2-4, DW35A, DW4, DW53, DWR, RA, Reb and upland. | |
Rea units are in Rosgen's (1996) E stream category. E streams are slightly entrenched, sluggish pool-dominated streams with thickly vegetated banks. They occur on surfaces deposited by larger processes. On the Kenai Lowlands those larger processes occurred when glaciers occupied more of the landscape, leaving behind lakebed, drainageway and kettle surfaces.
Rea units are E streams with channels that cannot be discerned on 1:25,000 aerial photography. Vegetation bands on the photography provide the clue that a stream with a bed and banks is present. E streams are common streams on the lowlands; Rea units often occur as first order, short-run streams originating in peatlands on relict glacial lakebeds.
After the floods that occurred during October and November of 2002, many E streams' character changed. Their beds were scoured, creating more riffles, and exposing cobbles and gravels. Beaver dams breached, so E streams that were dammed became free-flowing and now exhibit some B and C stream characters.
E streams are considered "evolutionary" (Rosgen, 1996). Many of these steams should probably be re-examined to observe whether or not they: 1) changed during the floods, 2) return to their former character, or 3) begin to evolve into a different stream type. The floods may have been one of the first big episodes in the long term evolution of these streams. The glacial till these streams now flow across will eventually be left as a terrace as the stream valley becomes entrenched into underlying bedrock over time. Then the till terrace will erode into the stream, a deep V-shaped valley will form, then perhaps glaciers will return and reset the process.
Fifty foot habitat protection area
Fourteen streams in the project area are covered under Kenai Peninsula Borough's Anadromous Streams Habitat Protection Ordinance. Many activities require a permit, or are prohibited within 50 feet of these streams. For a list of the streams, rationale for the ordinance, and details on obtaining a permit, visit the link highlighted above.
Floodplain regulation
From The Kenai Borough website:
"The Kenai Peninsula Borough manages a Floodplain Ordinance that addresses proper development to reduce flood risks and lessen the economic losses caused by flood events. The ordinance provides building standards for construction projects within the floodplain to ensure the availability of flood insurance through the National Flood Insurance Program. These building requirements also are intended to minimize or prevent damage when flood events occur. The ordinance requires floodplain development permits for all projects in floodplains."
In Homer, the name Reac refers to a human-created Rea wetland.
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Introduction and Key to Plant Communities |
| Contact: Mike Gracz Kenai Watershed Forum Homer Field Office Old Town Professional Center 3430 Main Street Suite B1 Homer, AK 99603 907-235-2218 |
15 November 2005 15:04 |
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