Mons Kronokiensis
mons ignifer Russiae
Mons Kronokiensis[1] (Russice Kronockaja sopka, Кроноцкая сопка[2]) est mons ignifer in Camtschatka, in reservato Kronokiensi, inter Oceanum Pacificum et lacum Kronokiensem, prope Vallem scaturiginum geyzerianarum, quae aquis calidis salientibus abundat, situs.
Res apud Vicidata repertae:
Altitudo: 3 527 metrum, 3 521 metrum
Locus: 54°45′0″N 160°31′0″E, 54°45′9″N 160°31′55″E
Civitas: Russia
Typus: Eastern Range
Locus: 54°45′0″N 160°31′0″E, 54°45′9″N 160°31′55″E
Civitas: Russia
Typus: Eastern Range
![](http://upload.wikimedia.org/wikipedia/commons/thumb/6/64/Kronotsky_volcano.jpg/220px-Kronotsky_volcano.jpg)
Pars circuli ignis Pacifici est. Altitudo montis 3482 metra est. Crateres multos habet. Eruptiones nunc rarae sunt, sed fumus et vapores perpetuo emittuntur.
![](http://upload.wikimedia.org/wikipedia/commons/thumb/c/c5/%D0%9A%D1%80%D0%BE%D0%BD%D0%BE%D1%86%D0%BA%D0%B0%D1%8F_%D1%81%D0%BE%D0%BF%D0%BA%D0%B0_%D1%81_%D0%B7%D0%B0%D0%BB%D0%B8%D0%B2%D0%B0_%D1%83_%D0%BD%D0%B8%D0%B7%D0%BE%D0%B2%D0%B8%D0%B9_%D0%A3%D0%BD%D0%B0%D0%BD%D1%8B.jpg/220px-%D0%9A%D1%80%D0%BE%D0%BD%D0%BE%D1%86%D0%BA%D0%B0%D1%8F_%D1%81%D0%BE%D0%BF%D0%BA%D0%B0_%D1%81_%D0%B7%D0%B0%D0%BB%D0%B8%D0%B2%D0%B0_%D1%83_%D0%BD%D0%B8%D0%B7%D0%BE%D0%B2%D0%B8%D0%B9_%D0%A3%D0%BD%D0%B0%D0%BD%D1%8B.jpg)
Notae
recensere- ↑ Norae Zabinkovae et Moysis Kirpicznikov Nomina physico-geographica principalia URSS s.v. Кроноцкая Сопка.
- ↑ Sopka est nomen montis seiuncti in Russia meridionali et in Oriente Extremo Russiae; cf. S. Ivaškovskij, Lexicon Rossico-Latinum, s.v. сопка.
Nexus externi
recensereSitus geographici et historici: Locus: 54°45′0″N 160°31′0″E, 54°45′9″N 160°31′55″E • GeoNames • Peakbagger • Global Volcanism Program • Большая российская энциклопедия |
Vicimedia Communia plura habent quae ad montem Kronokiensem spectant. |