Natural Resources
Conservation Service
Ecological site F220XY455AK
Maritime Forest Sandy Coastal Plain
Last updated: 6/05/2025
Accessed: 10/21/2025
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): 220X–Alexander Archipelago-Gulf of Alaska Coast
The Alexander Archipelago-Gulf of Alaska Coast area consists of a narrow arc of islands and lower elevation coastal mountains in the Southern Alaska Region. This area spans from the Alexander Archipelago in southeastern Alaska, north and west along the coast of the Gulf of Alaska and Prince William Sound, and further west to the southern tip of the Kenai Peninsula and the northeastern islands of the Kodiak Archipelago. The area makes up about 27,435 square miles (USDA 2006). The terrain primarily consists of low to moderate relief mountains that are deeply incised. Throughout the area glaciers, rivers, and streams have cut deep, narrow to broad valleys. The broader valleys have nearly level to strongly sloping flood plains and stream terraces. Alluvial and colluvial fans and short footslopes are common in the valleys along the base of the mountains. Rocky headlands, sea cliffs, estuaries, and beaches are common along the coast.
This area includes the Municipality of Juneau, Alaska's capital, and a number of smaller coastal towns and villages. Federally administered lands within this MLRA include Admiralty Island National Monument and part of Misty Fjords National Monument, Tongass National Forest, Chugach National Forest, and Glacier Bay, Wrangell-St. Elias, and Kenai Fjords National Parks and Preserves. The southern terminus of the Trans-Alaska Pipeline is in Valdez.
During the late Pleistocene epoch, the entire area was covered with glacial ice. The numerous fjords of the Alexander Archipelago and Prince William Sound were formed chiefly as a result of glacial scouring and deepening of preglacial river valleys. Most glacial deposits have been eroded away or buried by mountain colluvium and alluvium, which cover about 90 percent of the present landscape. The remaining glacial and glaciofluvial deposits are generally restricted to coastal areas. During the Holocene epoch, volcanic activity within and adjacent to this area deposited a layer of volcanic ash of varying thickness on much of the landscape in the southeastern and northwestern parts of the area. Paleozoic, Mesozoic, and Lower Tertiary stratified sedimentary rocks and Cretaceous and Tertiary intrusive rocks underlie much of the area and are exposed on steep mountain
slopes and ridges (USDA 2006).
The dominant soil orders in this MLRA are Spodosols, Histosols, and Entisols. Soils in the area typically have a cryic soil temperature regime, an udic moisture regime, and have mixed minerology. Spodosols are common on mountains and hills having been formed in gravelly or cobbly colluvium, glacial till, and varying amounts of silty volcanic ash. These Spodosols commonly range from shallow to deep, are well to somewhat poorly drained, and typically classify as Humicryods or Haplocryods. Histosols that are poorly to very poorly drained occur on footslopes, discharge slopes, and valley floors. These wet histosols commonly classify as Cryosaprists, Cryohemists, and Cryofibrists. Histosols that are well drained occur on steep mountainsides. These dry Histosols commonly classify as Cryofolists. Entisols are common on flood plains, stream terraces, and outwash plains having been formed in silty, sandy, and gravelly to cobbly alluvium. These Entisols are generally deep, range from well to somewhat poorly drained, and commonly classify as Cryaquents and Cryofluvents. Miscellaneous (non-soil) areas make up about 23 percent of the MLRA. The most common miscellaneous areas are avalanche chutes, rock outcrop, rubble land, beaches, river wash, and water.
This area represents the northern extent of the Pacific temperate rainforest and is characterized by productive stands of conifers. Western hemlock and Sitka spruce are the dominant trees on mountains and hills at the lower elevations. Due to warmer temperatures, western red cedar and Alaska cedar are more prevalent in the southern part of the area. Black cottonwood and mixed forest types occur on flood plains. Areas of peat and other sites that are too wet for forest growth support sedge-grass meadows and low scrub. The transition to subalpine and alpine communities typically occurs at elevations between 1500 to 3000 feet (Boggs et al. 2010, Carstensen 2007, Martin et al. 1995), which characterize the vegetation of the Southern Alaska Coastal Mountains area.
For many decades, logging, commercial fishing, and mining have been the primary industrial land uses throughout much of the area. In recent years, changes in public interests, land use policies, and timber economics have contributed to a significant decline in the timber industry. Commercial fishing continues to be an important industry and most communities support a fleet of boats and fishing related facilities. A number of mines operate in the area and others have been prospected and proposed. Tourism and wildland recreation are becoming increasingly important. Subsistence hunting, fishing, and gathering provide food and a variety of other resources to local residents and remain the principal economy for residents of remote villages.
Ecological site concept
This site occurs on coastal plains and glacial outwash plains and deltas with slopes not typically exceeding 5%. Soils are sandy and somewhat poorly- to poorly-drained. A shallow water table persists throughout the growing season and ponding occasionally occurs. This site supports a reference state comprised of three community phases driven by isostatic rebound. Over time, the emergence of landmasses, or isostatic rebound, in this are reduces ponding and leads to primary succession of plant communities. A second state has been identified on this site and results from anthropogenic ditching. This management practice increases soil drainage and aeration, causing shifts in plant community dynamics and composition.
The reference community phase is characterized as an open needleleaf spruce forest. It is composed primarily of mature Sitka spruce and lodgepole pine. Western hemlock is common, although the cover is low. The understory is variable. Some areas have minimal shrub and forb cover and a ground cover that is dominantly moss. Other areas have a mixed shrub-forb-moss understory with a higher diversity of species. Common shrub species include Sitka alder, oval-leaf blueberry, and crowberry.
Associated sites
| F220XY432AK |
Maritime Forest Gravelly Plain Ecological site F220XY432AK also occurs on glaciated outwash plains, but is associated with higher and drier positions as compared to F220XY455AK. While site F220XY432AK is not subject to high water table influences, the site does experience windthrow, logging, and ditching disturbance. |
|---|
Similar sites
| F220XY466AK |
Maritime Forest Sandy Plains Eolian Ecological site F220XY466AK supports a similar plant community on sandy soils but occurs on dunes and eolian hills and ridges. |
|---|
Figure 1. Typical area of associated ecological site F220XY432AK. This site is adjacent to site F220XY455AK and is not subject to ponding because of isostatic rebound. With continued isostatic rebound, site F220XY455AK may transition to site F220XY432AK.
Table 1. Dominant plant species
| Tree |
(1) Picea sitchensis |
|---|---|
| Shrub |
(1) Alnus viridis ssp. sinuata |
| Herbaceous |
(1) Hylocomium splendens |
Click on box and path labels to scroll to the respective text.
Ecosystem states
| T1A | - | Ditching |
|---|---|---|
| R2A | - | Return to reference state site hydrology |
State 1 submodel, plant communities
| 1.1a | - | Increased ponding and/or higher water table |
|---|---|---|
| 1.2b | - | decreased ponding and drier soils as a result of isostatic rebound. |
| 1.2a | - | Increased ponding and/or higher water table |
| 1.3a | - | decreased ponding and drier soils as a result of isostatic rebound. |