About: New England Uplands     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : owl:Thing, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon
http://dbpedia.demo.openlinksw.com/c/3zjrYsazeW

The topography of the New England Uplands section is that of a maturely-dissected plateau with narrow valleys, and the entire area is greatly modified by glaciation. It is the most widespread of the geomorphic sections in the New England Province, extending from Canada through New England down to the Seaboard section and extending southwestward through New York and New Jersey as two narrow upland projections, the Reading Prong and the Manhattan Prong. Numerous hills and mountains rise above the general level of the upland; except in the presence of mountains, the horizon of the regional landscape is fairly level. Glaciation has resulted in the erosion and rounding off of the bedrock topography and numerous rock basin lakes. Glacial drift is thin, patchy, and stony, and ice-contact features

AttributesValues
rdfs:label
  • New England Uplands (en)
rdfs:comment
  • The topography of the New England Uplands section is that of a maturely-dissected plateau with narrow valleys, and the entire area is greatly modified by glaciation. It is the most widespread of the geomorphic sections in the New England Province, extending from Canada through New England down to the Seaboard section and extending southwestward through New York and New Jersey as two narrow upland projections, the Reading Prong and the Manhattan Prong. Numerous hills and mountains rise above the general level of the upland; except in the presence of mountains, the horizon of the regional landscape is fairly level. Glaciation has resulted in the erosion and rounding off of the bedrock topography and numerous rock basin lakes. Glacial drift is thin, patchy, and stony, and ice-contact features (en)
dct:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
Link from a Wikipage to an external page
sameAs
dbp:wikiPageUsesTemplate
article
  • Geomorphic Provinces and Sections of the New York Bight Watershed (en)
url
has abstract
  • The topography of the New England Uplands section is that of a maturely-dissected plateau with narrow valleys, and the entire area is greatly modified by glaciation. It is the most widespread of the geomorphic sections in the New England Province, extending from Canada through New England down to the Seaboard section and extending southwestward through New York and New Jersey as two narrow upland projections, the Reading Prong and the Manhattan Prong. Numerous hills and mountains rise above the general level of the upland; except in the presence of mountains, the horizon of the regional landscape is fairly level. Glaciation has resulted in the erosion and rounding off of the bedrock topography and numerous rock basin lakes. Glacial drift is thin, patchy, and stony, and ice-contact features such as kames, kame terraces, and eskers are abundant. The surface of the New England Uplands slopes southeast from maximum inland altitudes around 670 meters (2,200 feet), excluding the other mountainous sections of the province, to about 122 to 152 meters (400 to 499 ft) along its seaward edge at the narrow coastal Seaboard section, which goes down to sea level. In the New York Bight watershed, the New England Uplands section is represented by a portion of the Taconic Mountains and its foothills, and by the Reading and Manhattan Prongs that extend southwestward from the New England states. Although geologists refer to the larger of these extensions as the Reading Prong, in this region it is more commonly known as the New York - New Jersey Highlands, and locally as the Hudson Highlands, the New Jersey Highlands, the Ramapo Mountains, or simply the Highlands. The Highlands are bounded on the southeast and on the northwest by the lowlands of the Piedmont and Great Valley provinces, respectively. The mountains and valleys that make up the Highlands are part of a relatively long, linear, and narrow regional geological feature that averages 16 to 32 kilometers (9.9 to 19.9 miles) in width, with a maximum width of 40 kilometers (25 miles), and extends in a southwest–northeast trending direction for nearly 225 kilometers (140 miles), from southeastern Pennsylvania near Reading to southwestern Connecticut near Danbury, where it joins the Taconic Mountains and Housatonic Highlands of the New England Uplands plateau. The Hudson River cuts a deep gorge through the Highlands in New York in the stretch of river between Peekskill on the south and Newburgh on the north. (en)
prov:wasDerivedFrom
page length (characters) of wiki page
foaf:isPrimaryTopicOf
is Link from a Wikipage to another Wikipage of
is Wikipage redirect of
is foaf:primaryTopic of
Faceted Search & Find service v1.17_git147 as of Sep 06 2024


Alternative Linked Data Documents: ODE     Content Formats:   [cxml] [csv]     RDF   [text] [turtle] [ld+json] [rdf+json] [rdf+xml]     ODATA   [atom+xml] [odata+json]     Microdata   [microdata+json] [html]    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 08.03.3331 as of Sep 2 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 65 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software