Natural Resources
Conservation Service
Ecological site R222XY360AK
Alpine Herbaceous Wet Organic Depressions
Last updated: 8/16/2024
Accessed: 11/21/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 222X–Southern Alaska Coastal Mountains
This area is in the Southern Alaska Region and includes the higher elevations of the Coast, St. Elias, Chugach, and Kenai Mountains. The area makes up about 26,335 square miles. The terrain consists of steep, rugged, high-relief mountains. Glaciers and ice fields make up about 54 percent of the area. Unglaciated portions of the area are deeply incised with narrow to broad valleys. Flood plains and stream terraces on valley floors rapidly give rise to steep alluvial fans and mountain footslopes. Elevation ranges from sea level at the base of tidewater glaciers and ice fields to 18,008 feet at the summit of Mt. St. Elias (USDA 2006).
During the Pleistocene epoch, the area was covered with glacial ice. As the glacial ice melted, sediments were deposited by the melting ice. However, most of the original glacial deposits have eroded away or have been buried by colluvium and slope alluvium, which covers more than 90 percent of the present unglaciated landscape. The remaining glacial and glaciofluvial deposits and recent fluvial deposits are generally restricted to the bottoms of the larger valleys. Paleozoic, Mesozoic, and Lower Tertiary stratified sedimentary rocks, and occasionally Paleozoic intrusive rocks, underlie much of the area and are exposed on steep mountain slopes and ridges (USDA 2006).
Miscellaneous (non-soil) areas make up more than 90 percent of this MLRA. The most common miscellaneous areas are rock outcrop, rubble land, avalanche chutes, and glaciers. The dominant soil orders in this area are Spodosols and Histosols. The soils in the area have a cryic soil temperature regime or a subgelic soil temperature class, a udic or aquic soil moisture regime, and mixed or amorphic mineralogy (USDA 2006).
Alpine plant communities characterize the vegetation in this area. Alpine vegetation consists of a variety of dwarf scrub and herbaceous communities. Low willow scrub is common in drainages. Lichens, scattered herbs, and dwarf shrubs dominate bedrock exposures and very shallow soils. In general, there is little or no plant growth at elevations above about 7,500 feet (USDA 2006). At lower elevations, subalpine vegetation consists of a variety of mountain hemlock and tall scrub communities. These subalpine plant communities typically occur at elevations between 1500 to 3000 feet (Boggs et al. 2010, Carstensen 2007, Jaques 1983; Martin et al. 1995) and are associated with the Alexander Archipelago-Gulf of Alaska Coast area (MLRA 220X).
The area is almost entirely undeveloped wild land. Remote wild-land recreation is the principal land use in this area. The rugged, high mountains, extensive glaciers and ice fields, and wilderness qualities of the area attract visitors from around the world. Small rural communities along the road system are the only permanent settlements. Part of the Wrangell-St. Elias Bay National Park and Preserve, the Glacier Bay National Park and Preserve, the Misty Fjords National Monument, the Chugach National Forest, and the Tongass National Forest are in this MLRA.
Classification relationships
Biophysical Settings: Alaskan Pacific Maritime Alpine Wet Meadow (BpS 7816730) (LANDFIRE 2009)
Ecological site concept
This high-elevation site has wet and shallow soils and a harsh alpine climate. The alpine is characterized as having very short growing seasons, cold temperatures, and high winds. Associated soils are very wet, organic-rich, and bedrock controlled. The harsh alpine climate and shallow, wet soils combine to prevent the growth and dominance of common subalpine species like mountain hemlock.
The reference plant community is wet graminoid herbaceous meadow that is primarily composed of dwarf sedges. Common species include tufted bulrush, grassy slope arctic sedge, black alpine sedge, Merten’s rush, white marsh marigold, and deer cabbage (Jaques 1983, Landfire 2009, and Flagstad and Boucher 2015). The primary disturbance processes that maintain this plant community are exposure to cold temperatures, ponding, wind, and avalanches (NatureServe 2018).
Associated sites
| R222XY352AK |
Alpine Dwarf Scrub Dry Organic Slopes Both sites occur in the alpine where organic matter accumulates, however, site 352 is dry organic matter over bedrock. |
|---|---|
| R222XY356AK |
Alpine Dwarf Scrub Dry Gravelly Slopes Occurs in the alpine on exposed slopes with drier soils. |
| R222XY357AK |
Alpine Dwarf Scrub Moist Gravelly Slopes Occurs in the alpine on drier soils where snow accumulates. |
Similar sites
| R222XY352AK |
Alpine Dwarf Scrub Dry Organic Slopes Both sites occur in the alpine where organic matter accumulates. However, site 352 is dry organic matter over bedrock. |
|---|---|
| R220XY362AK |
Subalpine Sedge Wet Flood Plain Sites 360 and 362 both have wet graminoid herbaceous meadow communities. However, site 362 occurs in subalpine flood plain, while site 360 occurs in wet depressions on mountains which do not flood. |
Table 1. Dominant plant species
| Tree |
Not specified |
|---|---|
| Shrub |
Not specified |
| Herbaceous |
(1) Trichophorum cespitosum |
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