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A Guide to over 70 Cultural Landscapes in New York City

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Solange Knowles and Mickalene Thomas. In size, New York ranks 27th compared with the other 50 states. Major rivers include the Hudson, the Mohawk and the Genessee.

Major lakes include Ontario, Erie, Champlain and George. The eastern part of New York state is dominated by the Great Appalachian Valley, while the northern part of the state includes Lake Champlain. This part also features the Hudson River. The western part of the valley features the Adirondack Mountains.

The Adirondacks are located in the northern part of the state. They are the highest and most rugged mountains. They are located between Lake Champlain in the east and Lake Ontario in the west. Most of the Adirondacks region consists of an ancient dome of Precambrian rock, similar geologically to the Canadian Shield, but also includes the Tug Hill Upland, which is more similar geologically to the Allegheny Plateau.

Landforms include high Appalachian peaks roughly 90 peaks surpass m , as well as a broad zone of lower mountains and foothills ranging down to m in elevation. The area is dominated by a combination of maple-beech-birch and red spruce-balsam fir forest, but also includes numerous glacial lakes and bogs, as well as alpine communities. Roughly 2. The most pervasive human influence on the natural landscape has been through commercial timber harvest and production, resulting in early removal of dominant white pine, hemlock, and old-growth spruce, and a gradual shift towards greater dominance by northern hardwoods.

Harvest today is primarily by means of selective cutting of single trees; therefore age structure and species composition of the forest will continue to be affected without creating additional areas of early seasonal vegetation.

The Catskills rise considerably higher than the neighboring parts of the upland. Summit elevations exceed ft. The mountainous character of the Catskills is due to the action of glaciation and streams carving deep valleys in the flat-lying rocks.

The glaciated Allegheny Plateau, which includes about one-third of the State, is the most extensive province in the State. On the east, the plateau is separated from the Hudson-Mohawk lowlands by the Helderberg escarpment and, to the south, grades into the Catskill Mountains. A series of escarpments form the boundary between the plateau and the lowlands to the north.

The province continues beyond the southern boundary of the State with the exception of the small unglaciated portion of the plateau in the southwest. It is the northeastern part of the great Appalachian Plateau which lies along the western side of the Appalachian Mountains and extends southward into Tennessee. This upland is underlain by great thicknesses of sedimentary rocks which lie almost horizontal, except for a slight dip to the southwest and a kind of sagging in the middle of the Finger Lakes District.

Severe dissection by both water and ice erosion has given the upland a somewhat rugged relief. It varies in elevation from to ft. The plateau is thought to represent ancient erosion surfaces and gives a rather flat-topped appearance when viewed from a distance. This small segment of the plateau, between the arc of the Allegheny River and the southern border of the State, is a rugged area with steep-sided valleys and high upland areas.

Maximum relief is about 1, ft. The central mass of the province displays the normal erosion of water-cut features rather than the ice erosion features of the rest of the plateau in New York State.

The fringes of the province on the east, north, and west do display features of glaciation and glacial deposition. A wild bleak upland which is truly plateau-like in the "text book" sense.

It is an outlier of the Appalachians, entirely separated from this and other provinces. The plateau drops off from flat swampy heights of ft.

On the east the boundary is a steep scarp face but the steepness disappears on the other side. Relief on the plateau surface is gentle except where easterly-flowing streams have cut "gulf" in the scarp resulting in a series of distinct terraces as it descends ft.

This province, extending across the Hudson River in a northeast-southwest direction, covers southern Orange and northern Rockland Counties and the area from southern Dutchess County southward across Putnam County and into Westchester County.




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