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- Champlain_Thrust abstract "The Champlain Thrust is a fault extending southward from southern Quebec, though western Vermont in the Champlain Valley, and into eastern New York in the Hudson Valley. This east dipping thrust fault transports Cambrian-Ordovician passive margin shelf rocks westerward by about 30–50 miles (48–80 km) and places them on top of Middle Ordovician rocks. The Middle Ordivician accretion of the one or more island arcs terranes drove the initial thrusting during the Taconic Orogeny, though reactivation of the fault may have occurred during the middle Devonian Acadian Orogeny.The thrust fault is exposed to the north of the city of Burlington, Vermont on the shores of Lake Champlain at Lone Rock Point. Here the Lower Cambrian Dunham dolostone can be seen thrust on top of the Middle Ordovician Iberville shales. The Champlain Thrust marks the most westerly thrust of the Taconic Orogeny.".
- Champlain_Thrust thumbnail Champlain_Thrust_Lone_Rock_.jpg?width=300.
- Champlain_Thrust wikiPageExternalLink chthrust.htm.
- Champlain_Thrust wikiPageExternalLink champlainthrust.html.
- Champlain_Thrust wikiPageID "14414168".
- Champlain_Thrust wikiPageRevisionID "595055614".
- Champlain_Thrust age "Ordovician".
- Champlain_Thrust formedBy "Taconic Orogeny".
- Champlain_Thrust hasPhotoCollection Champlain_Thrust.
- Champlain_Thrust name "Champlain Thrust".
- Champlain_Thrust photo "Champlain_Thrust_Lone_Rock_.jpg".
- Champlain_Thrust photoCaption "Champlain Thrust Fault, Lone Rock Point, Burlington Vermont".
- Champlain_Thrust subject Category:Geology_of_Vermont.
- Champlain_Thrust type GeologicalFormation109287968.
- Champlain_Thrust type Mountain109359803.
- Champlain_Thrust type NaturalElevation109366317.
- Champlain_Thrust type Object100002684.
- Champlain_Thrust type PhysicalEntity100001930.
- Champlain_Thrust type YagoGeoEntity.
- Champlain_Thrust type YagoPermanentlyLocatedEntity.
- Champlain_Thrust type Mountain.
- Champlain_Thrust type NaturalPlace.
- Champlain_Thrust type Place.
- Champlain_Thrust type Wikidata:Q532.
- Champlain_Thrust type Mountain.
- Champlain_Thrust type Place.
- Champlain_Thrust type Location.
- Champlain_Thrust comment "The Champlain Thrust is a fault extending southward from southern Quebec, though western Vermont in the Champlain Valley, and into eastern New York in the Hudson Valley. This east dipping thrust fault transports Cambrian-Ordovician passive margin shelf rocks westerward by about 30–50 miles (48–80 km) and places them on top of Middle Ordovician rocks.".
- Champlain_Thrust label "Champlain Thrust".
- Champlain_Thrust sameAs m.03d2sh1.
- Champlain_Thrust sameAs Q5070180.
- Champlain_Thrust sameAs Q5070180.
- Champlain_Thrust sameAs Champlain_Thrust.
- Champlain_Thrust wasDerivedFrom Champlain_Thrust?oldid=595055614.
- Champlain_Thrust depiction Champlain_Thrust_Lone_Rock_.jpg.
- Champlain_Thrust isPrimaryTopicOf Champlain_Thrust.
- Champlain_Thrust name "Champlain Thrust".