About: Kinsman Notch

An Entity of Type: mountain pass, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

Kinsman Notch (elev. 1,870 feet (570 m)) is a mountain pass located in the White Mountains of New Hampshire, United States. It is the westernmost of the major notches through the White Mountains (the others being Franconia Notch, Crawford Notch, and Pinkham Notch). To the southeast, the valley of the notch is drained by the Lost River, leading to the Pemigewasset River, and ultimately the Merrimack, flowing into the Gulf of Maine. The northwest half of the notch is drained by Beaver Brook and the Wild Ammonoosuc River, part of the Connecticut River watershed leading to Long Island Sound.

Property Value
dbo:abstract
  • Kinsman Notch (elev. 1,870 feet (570 m)) is a mountain pass located in the White Mountains of New Hampshire, United States. It is the westernmost of the major notches through the White Mountains (the others being Franconia Notch, Crawford Notch, and Pinkham Notch). To the southeast, the valley of the notch is drained by the Lost River, leading to the Pemigewasset River, and ultimately the Merrimack, flowing into the Gulf of Maine. The northwest half of the notch is drained by Beaver Brook and the Wild Ammonoosuc River, part of the Connecticut River watershed leading to Long Island Sound. The notch lies between Mount Moosilauke to the southwest and Kinsman Ridge to the northeast. The Appalachian Trail crosses the height of land in the notch on its route between Moosilauke and Kinsman Ridge. The trail descends Moosilauke along Beaver Brook Cascades, a long set of waterfalls descending a total of 1,200 feet (370 m). The Lost River Reservation, a wild gorge filled with enormous boulders, is found in the floor of the notch to the southeast of the height of land. New Hampshire Route 112 traverses the notch on its route from North Woodstock to Woodsville, New Hampshire. (en)
  • Kinsman Notch est un col de montagne situé à 570 mètres d'altitude dans les montagnes Blanches du New Hampshire, États-Unis. C'est le plus occidental des cols majeurs à travers les montagnes Blanches (les autres étant Franconia Notch, Crawford Notch, et ). Au sud-est, la vallée est drainée par la rivière Lost, menant à la rivière Pemigewasset, et finalement au fleuve Merrimack, coulant vers le golfe du Maine. Le versant nord-ouest du col est drainé par le ruisseau Beaver et la rivière Wild Ammonoosuc, un affluent de la rivière Ammonoosuc, une partie du bassin hydrographique du fleuve Connecticut menant à Long Island Sound. (fr)
dbo:location
dbo:name
  • Kinsman Notch (en)
dbo:thumbnail
dbo:wikiPageExternalLink
dbo:wikiPageID
  • 7424063 (xsd:integer)
dbo:wikiPageLength
  • 5429 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1113876541 (xsd:integer)
dbo:wikiPageWikiLink
dbp:1a
  • Parsons (en)
  • Watson (en)
dbp:1pp
  • 211 (xsd:integer)
  • 151190 (xsd:integer)
dbp:1y
  • 2010 (xsd:integer)
dbp:2a
  • Smith (en)
  • Heald (en)
  • Daniell (en)
dbp:2p
  • 76 (xsd:integer)
  • 273 (xsd:integer)
dbp:2y
  • 2002 (xsd:integer)
  • 2003 (xsd:integer)
dbp:elevationFt
  • 1870 (xsd:integer)
dbp:location
dbp:name
  • Kinsman Notch (en)
dbp:photo
  • Beaver Pond Kinsman Notch NH.jpg (en)
dbp:photoCaption
  • Beaver Pond near height of land in Kinsman Notch (en)
dbp:range
dbp:topo
  • USGS Mount Moosilauke (en)
dbp:traversed
  • 20 (xsd:integer)
dbp:wikiPageUsesTemplate
dbp:wordnet_type
dcterms:subject
gold:hypernym
georss:point
  • 44.0392 -71.7925
rdf:type
rdfs:comment
  • Kinsman Notch est un col de montagne situé à 570 mètres d'altitude dans les montagnes Blanches du New Hampshire, États-Unis. C'est le plus occidental des cols majeurs à travers les montagnes Blanches (les autres étant Franconia Notch, Crawford Notch, et ). Au sud-est, la vallée est drainée par la rivière Lost, menant à la rivière Pemigewasset, et finalement au fleuve Merrimack, coulant vers le golfe du Maine. Le versant nord-ouest du col est drainé par le ruisseau Beaver et la rivière Wild Ammonoosuc, un affluent de la rivière Ammonoosuc, une partie du bassin hydrographique du fleuve Connecticut menant à Long Island Sound. (fr)
  • Kinsman Notch (elev. 1,870 feet (570 m)) is a mountain pass located in the White Mountains of New Hampshire, United States. It is the westernmost of the major notches through the White Mountains (the others being Franconia Notch, Crawford Notch, and Pinkham Notch). To the southeast, the valley of the notch is drained by the Lost River, leading to the Pemigewasset River, and ultimately the Merrimack, flowing into the Gulf of Maine. The northwest half of the notch is drained by Beaver Brook and the Wild Ammonoosuc River, part of the Connecticut River watershed leading to Long Island Sound. (en)
rdfs:label
  • Kinsman Notch (fr)
  • Kinsman Notch (en)
owl:sameAs
geo:geometry
  • POINT(-71.792503356934 44.039199829102)
geo:lat
  • 44.039200 (xsd:float)
geo:long
  • -71.792503 (xsd:float)
prov:wasDerivedFrom
foaf:depiction
foaf:isPrimaryTopicOf
is dbo:wikiPageDisambiguates of
is dbo:wikiPageWikiLink of
is dbp:source1Location of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License