Cook Inlet Wetlands
LEFT: An idealized cross-section of an Re stream valley showing key characteristics and typical plants of local underfit streams. Drawing by Conrad Field. RIGHT: Range of wetlands mapped as Riverine.
Riverine wetlands lie adjacent to rivers and streams. The Cook Inlet Classification uses a modified version of Rosgen & Silvey's classification (1996) to name these wetlands. We use a modification of Level I, which has seven classes, four of which are common on the lowlands: Types B, C, D, and E (Fig. 1):
A fifth type, DA, is used to describe a small, multiple channel stream reach and associated wetlands as the reach fans out onto a glacial terrace, usually in a peatland.Steep, entrenched 'A' stream reaches, with rapids, waterfalls, and narrow associated wetland margins, occur along a few streams flowing into Kachemak Bay, such as McNeil and Falls Creek.
Many streams originate as moderately entrenched B reaches. The dominant B types at level II in Rosgen's classification are B4, with moderately steep valley walls and beds dominated by gravels, and B3 where cobbles dominate the bed material. B reaches have very narrow wetland fringes, if at all.
Type B reaches frequently flow into Type E reaches (E for “evolutionary”). E reaches are slightly entrenched, stable, low-gradient, pool-dominated reaches with low width/depth ratios, densely vegetated banks, and low sinuosity (although the typical Rosgen E reach has high sinuosity). E reaches have narrow active floodplains even though steep valley walls may be distant from the modern channel. Occasionally, abandoned channels and oxbows are evident.E reaches occur on relict glacial lakebeds or within wide valley bottoms that were eroded by large amounts of glacial meltwater at the last glacial maximum. A good example of an E reach is the upper portion of the Ninilchik River, which flows along a glacial terrace. The unnamed creek between Palmer and Wasilla that orginates near Memory Lake and dissappears into gravel near Vine road is another good example of an E reach. The most common reach types are E3 and E4 at level II in Rosgen’s classification, with cobble or gravel beds, respectively.
E reaches often have wide wetland fringes, fed by overbank flooding, groundwater discharge along the valley walls, and discharge of hyporrheic flow. Hyporrheic flow is the shallow groundwater flowing immediately beneath and adjacent to the channel. It can extend many meters to the sides of the stream.
E reaches are classified into four sub-types based on channel sinuosity and form (Fig. 2):
C reaches are the probably the most familiar model of rivers, with cut banks eroding at the outside bends, point bars forming on inside bends, and wide active floodplains. Many C reaches in Cook Inlet Basin lie in underfit valleys, but still support wide active floodplains. Many portions of the floodplain do no meet wetland criteria today, but the stream will eventually meander to every part of the floodplain. Wetlands on the floodplain are abandoned oxbows, fed by hyporrheic discharge or overbank flooding, or they are fed by shallow groundwater discharge at the toeslopes of the valley walls. Uncommonly, some wetlands adjacent to C reaches are relict abandoned meander terraces, which were formed when the river drained a glacier at the end of the last glacial maximum and are now peatlands situated on terraces above the modern floodplain. The lower portion of Willow Creek has several such features.
D reaches are large braided systems fed by glacial discharge. These reaches form aggading braidplains, and are very different from the meandering C stream model of cut banks and point bars. Aggradation can be extreme, especially on the braidplain of the Ressurection and Salmon Rivers near Seward where single flood events can raise portions of the plain a meter or more above the previous base level. Braidplains are extremely active, and often are sparsely vegetated but they do support less active floodplain wetlands along their margins. A braided thread of the river channel can potentially shift its flow to any portion of the wide braidplain.
NWI and HGM
Riverine wetlands are the same as the Riverine classification in the US Fish and Wildlife Service's National Wetland Inventory (Cowardin et al 1979). Riverine 3, (upper perennial) is the most common NWI type on the lowlands, these reaches have fast velocity, gravel to boulder beds, and little floodplain development, corresponding to Rosgen's (1996) "B" streams. R2 (lower perennial) rivers and streams are also common. These are low gradient, slow velocity "E" and "RDA" streams, although, unlike typical NWI R2 streams, floodplains may be poorly developed and oxygen deficits probably never occur. Stream-adjacent wetlands are found near braided glacial rivers which in NWI these are intermittently flooded PSS/EMJ Palustrine shrub/scrub and emergent wetlands.
The LLWW hydrogeomorphic classification of Tiner (2003) would place lowland stream-adjacent wetlands in its Lotic Stream fringe category. Type B and C streams are "middle gradient streams"; while E and RDA streams are "low gradient streams". Rib's are Bidirectional-nontidal River Island wetlands.
Soils and Plant Communities
Cation chemistry by Geomorphic Component. Riverine wetlands (highlighted in blue) have generally low cation concentrations compared to other Geomorphic Components, indicating that precipitation and snowmelt strongly influence chemistry. Although calcium and silicon show the greatest concentrations, magnesium and iron concentrations in our area are high for natural waters. DW = Drainageway, K = Kettle; S = Discharge Slope; LB = Lakebed; SF = Spring Fen; RT = VLD Trough; R= Riparian; H = Headwater Fen; D = Depression.
Samples were collected from a surface pool where possible, otherwise from a separate shallow pit excavated to just below the water table. All samples were filtered through either a 0.2 micron filter using a disposable syringe, or pumped through a 0.45 micron filter using a peristaltic pump. Samples were acidified with ultra-pure nitric acid and kept cool until analysis on a direct current plasma spectrometer to about 5% accuracy (except K, 10-20% accuracy).
Riverine Wetland Types:
AMT- Abandoned meander terraces and channels (not strictly Riverine wetlands, but associated with a few rivers and streams)
Rel- Linear, sinuosity less than 1.3, low gradient, pool dominated, on glacial deposits.
Res- Sinuous, sinuosity greater than 1.3, low gradient, pool dominated, on glacial deposits.
Reb- Bank-full due to beaver dam, roads, logging debris or natural obstruction. Low gradient, on glacial deposits.
Rea- Stream surface not discernable on aerial photography. On glacial deposits.
Rib- Islands and bars in streams.
RA- Steeper, step and pool morphology
RB- Higher gradient (>2%); riffle dominated.
RC- Floodplain developed. Point bars. Riffle/pool morphology.
RDA- Multiple braided, low gradient, pool-dominated channels on glacial deposits.
RD3C- Glacier-fed braided channels dominated by cobbles. Fourth of July Creek near Seward
RD4C- Glacier-fed braided channels dominated by gravels. The Resurrection River in Seward
RDF1- Permanantly flooded ponds on the braidplains of glacier-fed reaches
RDF2- Stable water table near the surface in wetlands on the braidplains of glacier-fed reaches, usually sedge dominated
RDF3- Fluctuating water table on the braidplains of glacier-fed reaches, usually shrubby
RD4SC- Side channels on the braidplains of glacier-fed reaches
RD4T1- Low terraces on the braidplains of glacier-fed reaches, often does not meet wetland jurisdictional criteria
RD4T2- Higher terraces on the braidplains of glacier-fed reaches, often does not meet wetland jurisdictional criteria
Rt- Tidally influenced river or stream. Usually too small to map but extends about a mile on larger streams, and several miles on the Kasilof and Kenai Rivers.
PO Box 15301
Fritz Creek, AK 99603
26 October, 2011