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Rome Sand Plains is a pine barrens about west of the city center of Rome, New York, which is in Oneida County in central New York. It consists of a mosaic of sand dunes extending about above low peat bogs that lie between the dunes. The barrens are covered with mixed northern hardwood forests, meadows, and wetlands. About are protected in conservation preserves. Pine barrens are typical of seacoasts; the Rome Sand Plains is one of only a handful of inland pine barrens remaining in the United States.〔(【引用サイトリンク】title=Rome Sand Plains Resource Management Area )〕 The Albany Pine Bush is located north and west of the capital city of the state. E. W. Russell has described the Sand Plains as follows, "The landscape today forms a sharp contrast with the surrounding flat, fertile farmland, which is almost all cleared of trees and planted in crops. Uplands, including some dunes, support forest vegetation of American beech, white oak (''Quercus alba''), red and sugar maples, white and pitch pine (''Pinus strobus'' and ''P. rigida''), gray birch (''Betula populifolia''), hemlock, aspen (''Populus'' spp.), American elm, and other northern hardwood species. Some uplands are also characterized as pitch pine heaths, dominated by pitch pines with an understory of blueberries (''Vaccinium'' spp.) and other related (ericaceous) shrubs. Pitch pine is the characteristic tree of the wetlands, along with aspen, gray birch, and red maple, along with an ericaceous shrub layer." Among the several rare species in the Sand Plains are the purple pitcher plant and a sundew (both of which are carnivorous plants), red-shouldered hawks, martens, and the frosted elfin butterfly, which is a threatened species in New York State.〔(【引用サイトリンク】url=http://www.dec.ny.gov/animals/7494.html )〕 Other species to be found include wild blue lupine (also rare, and the food for the frosted elfin), barrens buckmoth (''Hemileuca maia''), whippoorwill, pine warbler and pitch pine, normally indigenous to coastal areas. The Rome Sand Plains were owned privately through about 1980. The sand was mined to make molds and cores for metal casting. An application for a permit to mine sand around 1980 triggered a regional effort to protect the area. The New York State Department of Environmental Conservation began purchasing lands, working with The Nature Conservancy and other organizations. of the Sand Plains have been purchased by the DEC, and are designated as the Rome Sand Plains Unique Area.〔(【引用サイトリンク】url=http://www.dec.ny.gov/outdoor/7795.html )〕 The Nature Conservancy holds another .〔(【引用サイトリンク】title=Rome Sand Plains )〕 The Izaak Walton League holds about , Oneida County holds an additional as a County Forest, and a few acres are held by the City of Rome. A map showing these holdings was released by the DEC in 2008; the map shows the location of three foot trails maintained by the DEC and one by the Izaak Walton League.〔(【引用サイトリンク】url=http://www.dec.ny.gov/docs/regions_pdf/rspmap.pdf )〕 A consolidated management plan involving all five preserves, and addressing the entire Sand Plains area, was published in 2006.〔(【引用サイトリンク】date=March 3, 2006 )〕 The sand plains are considered by geologists to be a relic of Lake Iroquois, which was a somewhat larger version of the present Lake Ontario that existed near the end of the last ice age about twelve thousand years ago. The level of Lake Iroquois was about higher than Lake Ontario's present level. Lake Iroquois drained to the Atlantic Ocean via the Mohawk and Hudson rivers, and its outlet was near the present Sand Plains.〔 The work of Anderson and Lewis (1985) is the basis for these authors' views on the history of the post-glacial water levels.〕 Lake Ontario's outlet is near the Thousand Islands, and the lake drains through the Saint Lawrence River; this outlet was dammed by ice in the period when Lake Iroquois existed. ==See also== *List of pine barrens 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Rome Sand Plains」の詳細全文を読む スポンサード リンク
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