Natural Resources
Conservation Service
Ecological site R144AY050RI
Subaqueous Haline Flats
Last updated: 10/04/2024
Accessed: 12/03/2024
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): 144A–New England and Eastern New York Upland, Southern Part
MLRA 144A: New England and Eastern New York Upland, Southern Part
The eastern half of the eastern part of this MLRA is in the Seaboard Lowland Section of the New England Province of the Appalachian Highlands. The western half of the eastern part and the southeastern half of the western part are in the New England Upland Section of the same province and division. The northwestern half of the western part is in the Hudson Valley Section of the Valley and Ridge Province of the Appalachian Highlands. This MLRA is a very scenic area of rolling to hilly uplands that are broken by many gently sloping to level valleys that terminate in coastal lowlands. Elevation ranges from sea level to 1,000 feet (0 to 305 meters) in much of the area, but it is 2,000 feet (610 meters) on some hills. Relief is mostly about 6 to 65 feet (2 to 20 meters) in the valleys and about 80 to 330 feet (25 to 100 meters) in the uplands.
This area has been glaciated and consists almost entirely of till hills, drumlins, and bedrock-controlled uplands with a mantle of till. It is dissected by narrow glacio-fluvial valleys. The southernmost boundary of the area marks the farthest southward extent of Wisconsinian glaciation on the eastern seaboard. The river valleys and coastal plains are filled with glacial lake sediments, marine sediments, and glacial outwash. The bedrock in the eastern half of the area consists primarily of igneous and metamorphic rocks of early Paleozoic age. Granite is the most common igneous rock, and gneiss, schist, and slate are the most common metamorphic rocks. In the parts of the MLRA in eastern and southeastern New York, Devonian- to Pennsylvanian-age sandstone, shale, and limestone are dominant. Carbonate rocks, primarily dolomite and limestone, are the dominant kinds of bedrock in the part of this MLRA in northwestern Connecticut.
Ecological site concept
The Subaqueous Haline Flats ecological site consists of very deep, subaqueous soils permanently submerged beneath 10 through 150 cm of tidal estuarine water on flood tidal delta flats, washover fan flats in coastal lagoons and bays. Slope ranges from 0 through 2 percent. Representative soils are Massapog, Nagunt, and Rhodesfolly 0-1 meter depth.
Massapog soils are formed in sandy marine and estuarine sediments transported by flood tidal currents. Nagunt soils are formed in sandy marine deposits as a result of washover events, eolian deposition, and tidal flooding. Buried surface horizons and stratification are often identified. The Rhodesfolly soils are formed in sandy marine deposits. Some areas are vegetated with native macroalgae, eelgrass (Zostera marina) and/or widgeonweed (Ruppia maritima). Vegetative cover ranges from 0 to 35 percent. The site is used for recreation and support benthic aquatic habitat. Fishing is commonplace and the species found in the area are smelt, small cod, flounder, scup, menhaden, and white perch. Shellfish farming and recreational harvesting are common.
Associated sites
R144AY047RI |
Subaqueous Haline Glacial Deposits |
---|---|
R144AY048RI |
Subaqueous Haline Low Energy Basins |
R144AY049RI |
Subaqueous Haline Slopes |
Similar sites
R144AY047RI |
Subaqueous Haline Glacial Deposits |
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R144AY048RI |
Subaqueous Haline Low Energy Basins |
R144AY049RI |
Subaqueous Haline Slopes |
Table 1. Dominant plant species
Tree |
Not specified |
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Shrub |
Not specified |
Herbaceous |
(1) Zostera marina |
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