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- Q126153 subject Q8665776.
- Q126153 subject Q8690298.
- Q126153 abstract "The Arnaud River (formerly known as the Payne River) is a river in Nunavik, Quebec, Canada, flowing from the low plateaux of the Ungava Peninsula through a series of glacial lakes to Ungava Bay. Its mean discharge is approximately 15 km³ per year, but the river flows only in the summer as it is frozen to several metres for the rest of the year. The total length of the river is about 377 kilometres, but there are several main channels in the upper reaches of the river, most of them unnamed and hardly sighted even by the native Inuit.The Inuit village of Kangirsuk lies near the mouth of the Arnaud River on the north shore of Payne Bay, 13 kilometres (8.1 mi) inland from the western coast of Ungava Bay. About 22 kilometres (14 mi) upstream from Kangirsuk is the Hammer of Thor archaeological site.Most of the basin is almost totally barren owing to the harsh climate - the mean temperature is only about 7 °C (45 °F) even at the height of summer and continuous permafrost extends deep from only half a metre below the surface. The only vegetation is low shrubs at the lower levels, for no trees grow within the Arnaud basin even in the most sheltered sites, and the river freezes for too long to make hydroelectric development feasible.The basin of the Arnaud River, though intensely glaciated for almost the whole of the Quaternary - ice sheets are known to have been thicker over the basin at the Last Glacial Maximum than they are over Antarctica today - is the site of a major meteorite impact about a million years ago that has been surprisingly well preserved, probablyREDIRECT Template:Weasel inlineThis is a redirect from a page that has been moved (renamed). This page was kept as a redirect to avoid breaking links, both internal and external, that may have been made to the old page name. For more information follow the bold category link. because the exposed surface rocks are exceedingly old and the meteorite might have been deposited in such a way as to ensure preservation during the long glaciations.".
- Q126153 country Q16.
- Q126153 discharge "670.0".
- Q126153 region Q1074865.
- Q126153 riverMouth Q1165951.
- Q126153 state Q176.
- Q126153 synonym "Payne River".
- Q126153 synonym "Rivière Arnaud".
- Q126153 thumbnail Payne_Bay_QC.JPG?width=300.
- Q126153 wikiPageWikiLink Q1074865.
- Q126153 wikiPageWikiLink Q1165951.
- Q126153 wikiPageWikiLink Q12599.
- Q126153 wikiPageWikiLink Q16.
- Q126153 wikiPageWikiLink Q176.
- Q126153 wikiPageWikiLink Q1862522.
- Q126153 wikiPageWikiLink Q189975.
- Q126153 wikiPageWikiLink Q1979625.
- Q126153 wikiPageWikiLink Q23397.
- Q126153 wikiPageWikiLink Q26185.
- Q126153 wikiPageWikiLink Q3849991.
- Q126153 wikiPageWikiLink Q602963.
- Q126153 wikiPageWikiLink Q75520.
- Q126153 wikiPageWikiLink Q7937.
- Q126153 wikiPageWikiLink Q80638.
- Q126153 wikiPageWikiLink Q84127.
- Q126153 wikiPageWikiLink Q8665776.
- Q126153 wikiPageWikiLink Q8690298.
- Q126153 wikiPageWikiLink Q991147.
- Q126153 country "Canada".
- Q126153 discharge "670".
- Q126153 mouth "Ungava Bay".
- Q126153 name "Arnaud River".
- Q126153 otherName "Payne River".
- Q126153 otherName "Rivière Arnaud".
- Q126153 region "Nunavik".
- Q126153 state "Quebec".
- Q126153 type BodyOfWater.
- Q126153 type Place.
- Q126153 type RiverBodyOfWater.
- Q126153 type BodyOfWater.
- Q126153 type Location.
- Q126153 type NaturalPlace.
- Q126153 type Place.
- Q126153 type River.
- Q126153 type Stream.
- Q126153 type Thing.
- Q126153 type Q4022.
- Q126153 type Q47521.
- Q126153 comment "The Arnaud River (formerly known as the Payne River) is a river in Nunavik, Quebec, Canada, flowing from the low plateaux of the Ungava Peninsula through a series of glacial lakes to Ungava Bay. Its mean discharge is approximately 15 km³ per year, but the river flows only in the summer as it is frozen to several metres for the rest of the year.".
- Q126153 label "Arnaud River".
- Q126153 depiction Payne_Bay_QC.JPG.
- Q126153 name "Arnaud River".