Natural Resources
Conservation Service
Ecological site F111XE204OH
Dry Alluvium Forest
Last updated: 9/11/2024
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): 111X–Indiana and Ohio Till Plain
111E – Indiana and Ohio Till Plain, Eastern Part. Most of this area is in the Till Plains Section of the Central Lowlands Province of the Interior Plains. The northeast tip of the area is in the Southern New York Section of the Appalachian Highlands. The entire area has been glaciated. It is dominated by ground moraines that are broken in places by kames, lake plains, outwash plains, terraces, and stream valleys. Narrow, shallow valleys commonly are along the few large streams in the area. Elevation ranges from 580 to 1,400 feet (175 to 425 meters), increasing gradually from west to east. Relief is mainly a few meters, but in some areas hills rise as much as 100 feet (30 meters) above the adjoining plain.
The extent of the major Hydrologic Unit Areas (identified by four-digit numbers) that make up this MLRA is as follows: Scioto (0506), 33 percent; Muskingum (0504), 31 percent; and Western Lake Erie (0410), 28 percent; Upper Ohio (0503), 5 percent; and Southern Lake Erie (0411), 3 percent. The headwaters of many rivers in central Ohio, including the Vermillion, Black Fork, Sandusky, Little Scioto, and Olentangy Rivers, are in this MLRA.
This MLRA is underlain by late Devonian shale and sandstone. Surficial materials include glacial deposits of till, glaciolacustrine sediments, and outwash from Wisconsin and older glacial periods.
Classification relationships
Major Land Resource Area (USDA-Natural Resources Conservation Service, 2006)
USFS Ecological Regions (USDA, 2007):
Sections –Central Till Plains, Beech Maple (222H), Western Glaciated Allegheny Plateau (221F)
Subsections – Allegheny Plateau (221Fa), Bluffton Till Plains (222Ha), Miami-Scioto Plain – Tipton Till Plain (222Hb)
NatureServe Systems anticipated (NatureServe, 2011): Agriculture - Cultivated Crops and Irrigated Agriculture, Agriculture – Pasture/Hay, North-Central Interior Floodplain
LANDFIRE Biophysical Settings anticipated (USGS, 2010): Central Interior and Appalachian Floodplain Systems
Ecological site concept
This site is a wetland/riparian site formed on soils with alluvial parent materials that are moderately well to well drained that a have a light (lighter than 3/2 Munsell) surface color. It is located along the floodplain, often on steps, natural levees, and terraces, of lotic systems in sandy alluvial deposits overlaying coarser materials. The site is generally constrained to a narrow landscape position that is influenced by the adjacent uplands and riparian areas. Flooding can be very rare to frequent, depending on the riparian system with durations up to 7 days. Landscape position and internal drainage preclude ponding from occurring on this site.
The characteristic vegetation of the site is that of a riparian forest dominated principally by sugar maple and basswood. Additional canopy level species include black walnut, silver maple, and elm. Active hydrologic and geomorphic process, along with windthrow of established trees, drive the long interval disturbance regime of this tree dominated site. These macro and micro scale disturbance events creates mixed-aged forests that contains both late and early seral species. These dynamics have been drastically changed due to the installation of levees, dams, and channelization of the system. Establishment woody non-native, invasive species, followed by no management to control them, can alter the state of the site. The invasive species can persist in the understory as a component and then spread rapidly with an opening in the canopy. They can come to dominate the understory of the site, while the canopy level species remain, relatively, unchanged. Removal of the woody species, installation of tile, and agricultural practices move this site to a new state. Much of the historic acres of this site have been transitioned to agriculture with the bulk of those acres being in corn and soybean rotations.
Associated sites
| F111XE202OH |
Dry Alluvium Floodplain Soils are moderately well to well drained; surface dark in color (mollic) |
|---|---|
| F111XE201OH |
Wet Alluvium Floodplain Soils are very poorly drained; surface dark in color (mollic) |
| F111XE203OH |
Wet Alluvium Forest Soils are poorly to somewhat poorly drained |
Similar sites
| F111XE102OH |
Lacustrine Forest Located on lacustrine parent materials; soils are somewhat poorly drained or drier. |
|---|---|
| F111XE301OH |
Wet Restricted Located on residuum parent materials; soils are somewhat poorly drained; soils have a restrictive layer within 36 inches of the surface. |
| F111XE403OH |
Outwash Upland Located on outwash parent materials; soils are very poorly to somewhat poorly drained. |
| F111XE503OH |
Till Ridge Located on glacial till parent materials; site located on a convex landscape position; soils are moderately well to well drained. |
| F111XE502OH |
Wet Till Ridge Located on glacial till parent materials; site located on a convex landscape position; soils are somewhat poorly drained. |
Table 1. Dominant plant species
| Tree |
(1) Acer saccharum |
|---|---|
| Shrub |
Not specified |
| Herbaceous |
Not specified |
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