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Natural Resources
Conservation Service
Ecological site F145XY013CT
Well Drained Till Uplands
Accessed: 08/17/2024
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): 145X–Connecticut Valley
The nearly level floor of the Connecticut River Valley makes up most of the area. Nearly level to sloping lowlands are at the outer edges of the river valley. These lowlands are broken by isolated, north- to south-trending trap-rock ridges that are hilly and steep. Elevation ranges from sea level to 330 feet in the lowlands and from 650 to 1,000 feet on ridges.
Recent alluvium has been deposited on the nearly level flood plain along the Connecticut River since the glacial retreat about 10,000 to 12,000 years ago. These deposits created some of the most productive agricultural soils in New England. Glacial lake deposits, outwash, and recent alluvial deposits dominate.
The area primarily supports central hardwoods. Habitat loss and fragmentation are widespread throughout the lower part of the Connecticut River Valley. The major tree species in the rest of the forested areas are sugar maple, birch,beech, oaks, and hickory. White pine and hemlock are the dominant conifers, but pitch pine and red pine are more common on sandy soils. Red maple grows on the wetter sites.
The most common understory plants are moosewood and hobblebush in the northern part of the area and dogwood in the southern part. Abandoned agricultural land is dominated by white pine and paper birch in the northern part and red cedar and gray birch in the southern part. The important upland habitats include trap-rock ridges and sand plains. Oak woodlands and cedar glades are common on the ridges. Black oak savannas mixed with pitch pine and varying amounts of little bluestem are common on the sand plains. Other habitats of significance include wetlands associated with the Connecticut River freshwater marshes, swamps, flood plains, and lowlands. The dominant trees on the flood plains are black willow, cottonwood, and sycamore.
Classification relationships
LRR: Northeastern Forage and Forest Region
MLRA 145 Connecticut Valley
USDA USFS:
Province221: Eastern Broadleaf Forest
Section 221A: Lower New England
Subsection 221Af: Lower Connecticut River Valley
EPA Ecoregions:
Level III: 59 Northeast Coastal Zone
Level IV: 59a Connecticut Valley
Ecological site concept
The site consists of well drained, loamy soils formed in ablation till derived mostly from reddish sandstone, shale, and conglomerate with some basalt. The soils are moderately deep and deep to bedrock. They are nearly level to moderately steep soils on hills and ridges. Representative soils are Yalesville and Cheshire.
The reference plant community coincides with the northern red oak/mapleleaf viburnum forests (Metzler and Barrett 2006). Red oak is often the dominant tree species but other species can co-occur such as black oak, chestnut oak, American beech, sugar maple, white ash, red maple and shagbark hickory. Flowering dogwood, ironwood, and hop-hornbeam are common in the sub-canopy. Common shrubs include mapleleaf viburnum, American witch hazel, lowbush blueberry, and beaked hazelnut. Common herbaceous plants include fragrant bedstraw, spotted geranium, Christmas fern, and Pennsylvania sedge. In openings following tree falls or other natural disturbances warm season grasses such as little bluestem and big bluestem may occur along with early successional trees such as eastern red cedar and black birch. Invasive exotic plants such as Japanese barberry, multiflora rose, winged euonymus, and shrub honeysuckles can occur in disturbed sites. Overbrowsing by white-tailed deer can significantly alter the structure of this community.
The site is very similar to the Well Drained Till Uplands within MLRA 144A, however the growing season is longer within MLRA 145 relative to the surrounding MLRA 144A. Additionally, the unique red soil mineralogy which characteristic of the Connecticut River Valley (MLRA 145) provides a relatively richer substrate for vegetative growth.
Table 1. Dominant plant species
Tree |
(1) Quercus rubra |
---|---|
Shrub |
(1) Cornus florida |
Herbaceous |
Not specified |
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