{{Infobox river | name = Anuy | image = Kalmytsky brod.jpg | image_caption = | source1 = | source1_elevation = | mouth = Ob | mouth_location = | mouth_coordinates = {{coord|52|24|10|N|84|44|40|E|source:kolossus-ruwiki|display=it}} | progression = {{ROb}} | subdivision_type1 = Country | subdivision_name1 = Russia |length_km=327 | discharge1_avg = |basin_size_km2=6930 }}
The '''Anuy''' ({{langx|ru|река́ Ану́й}}) is a left tributary of the Ob originating in the Altai Mountains of Siberia, Russia.<ref>[http://bse.sci-lib.com/article064170.html Ануй (река в Алтайском кр.)], Great Soviet Encyclopedia</ref> It is {{convert|327|km}} long, and has a drainage basin of {{convert|6930|km2}}.<ref name=gvr>{{GVR|187978|Река АНУЙ}}</ref>
The Chyorny Anuy and the smaller Bely Anuy join to form the Anuy. The Chyorny Anuy starts at an elevation of {{convert|1220|m|ft}} at the southeastern end of the Anuy mountain range in the Altai Republic. Flowing in a northwestern direction, it enters Altai Krai after about {{convert|40|km|mi}}. The two rivers join near Soloneshensky District.
The Anuy exits the Altai mountains at an elevation of {{convert|250|m|ft}} and flows in a northeastern to eastern direction. Near the village of Anuyskoye, the river takes a northern direction and joins the Ob west of Biysk at an elevation of about {{convert|150|m|ft}}.
The average flow at Staro-Tirishkino, about {{convert|10|km|mi|0}} near the river's end, is about {{convert|36.1|m3/s|cuft/s}} with a minimum of {{convert|6.9|m3/s|cuft/s}} in February and a maximum of {{convert|123|m3/s|cuft/s}} in April.<ref>[http://www.r-arcticnet.sr.unh.edu/v4.0/ViewPoint.pl?Point=6709 Flow Gauge at Staro-Tirishkino]</ref>
The Anuy is frozen between November and April. It is not navigable.
The Denisova Cave is approximately {{convert|28|m|ft}} above the right bank of the Anuy.
==References== {{Reflist}} This article is based on a partial translation of the corresponding German web site from March 29, 2010.
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Category:Rivers of Altai Krai Category:Rivers of the Altai Republic