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The Ecstall Greenstone Belt is a north-northwest trending greenstone belt in northwestern British Columbia, Canada. It is located in the Kitimat Ranges of the Coast Mountains between the communities of Prince Rupert and Kitimat, in the vicinity of the Ecstall River. This 80 km (50 mi) long and 3 to 20 km (1.9 to 12.4 mi) wide geologic feature forms a small portion of the 2,000 km (1,200 mi) long , which ranges from Proterozoic-to-Paleozoic age. Metavolcanic and metasedimentary rocks as well as quartzite and layered gneiss comprise the Ecstall Greenstone Belt.

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  • The Ecstall Greenstone Belt is a north-northwest trending greenstone belt in northwestern British Columbia, Canada. It is located in the Kitimat Ranges of the Coast Mountains between the communities of Prince Rupert and Kitimat, in the vicinity of the Ecstall River. This 80 km (50 mi) long and 3 to 20 km (1.9 to 12.4 mi) wide geologic feature forms a small portion of the 2,000 km (1,200 mi) long , which ranges from Proterozoic-to-Paleozoic age. Metavolcanic and metasedimentary rocks as well as quartzite and layered gneiss comprise the Ecstall Greenstone Belt. (en)
  • La cintura di rocce verdi Ecstall è una cintura di rocce verdi ad andamento nord-nordovest, situata nella parte nordoccidentale della Columbia Britannica, in Canada. La cintura è situata nella catena montuosa Kitimat Ranges, che fa parte delle Montagne Costiere, tra le municipalità di Prince Rupert e Kitimat. Ha una lunghezza di 80 km e una larghezza compresa tra 3 e 20 km; rappresenta una piccola porzione del che è lungo quasi 2.000 km. Le rocce della cintura Ecstall risalgono al Precambriano e al Paleozoico. (it)
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  • The Ecstall Greenstone Belt is a north-northwest trending greenstone belt in northwestern British Columbia, Canada. It is located in the Kitimat Ranges of the Coast Mountains between the communities of Prince Rupert and Kitimat, in the vicinity of the Ecstall River. This 80 km (50 mi) long and 3 to 20 km (1.9 to 12.4 mi) wide geologic feature forms a small portion of the 2,000 km (1,200 mi) long , which ranges from Proterozoic-to-Paleozoic age. Metavolcanic and metasedimentary rocks as well as quartzite and layered gneiss comprise the Ecstall Greenstone Belt. (en)
  • La cintura di rocce verdi Ecstall è una cintura di rocce verdi ad andamento nord-nordovest, situata nella parte nordoccidentale della Columbia Britannica, in Canada. La cintura è situata nella catena montuosa Kitimat Ranges, che fa parte delle Montagne Costiere, tra le municipalità di Prince Rupert e Kitimat. Ha una lunghezza di 80 km e una larghezza compresa tra 3 e 20 km; rappresenta una piccola porzione del che è lungo quasi 2.000 km. Le rocce della cintura Ecstall risalgono al Precambriano e al Paleozoico. (it)
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  • Ecstall Greenstone Belt (en)
  • Cintura di rocce verdi Ecstall (it)
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