Kulduk-Too (original) (raw)

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Kulduk-Too (Kyrgyz: Кулдук-Тоо) is a northern offspur of the Alay Range in the Batken Region of Kyrgyzstan. It is located between the valley of the river Sokh and that of its tributary Kojashkan. It stretches from west to east, south of the Aydarken depression, and is connected in the east with the range. The length of the range is 31 km (19 mi), its width is 7–8 km (4.3–5.0 mi). Its average height is 4,100–4,300 m (13,500–14,100 ft), and its highest point is 5,016 m (16,457 ft). The northern slope, long and gentle, gradually descends to Sokh river and Khaidarkan depression. The southern slope, short and steep, features great variations in altitudes. Both slopes are deeply dissected by tributaries of Sokh river. The range is composed of Silurian and Carboniferous rocks: (shale, limestone,

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dbo:abstract Kulduk-Too (Kyrgyz: Кулдук-Тоо) is a northern offspur of the Alay Range in the Batken Region of Kyrgyzstan. It is located between the valley of the river Sokh and that of its tributary Kojashkan. It stretches from west to east, south of the Aydarken depression, and is connected in the east with the range. The length of the range is 31 km (19 mi), its width is 7–8 km (4.3–5.0 mi). Its average height is 4,100–4,300 m (13,500–14,100 ft), and its highest point is 5,016 m (16,457 ft). The northern slope, long and gentle, gradually descends to Sokh river and Khaidarkan depression. The southern slope, short and steep, features great variations in altitudes. Both slopes are deeply dissected by tributaries of Sokh river. The range is composed of Silurian and Carboniferous rocks: (shale, limestone, and conglomerate) and more rarely by intrusive rock such as granite and granodiorite. (en)
dbo:country dbr:Kyrgyzstan
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dbo:width 7000.000000 (xsd:double)
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dbo:wikiPageWikiLink dbr:Carboniferous dbr:Batken_District dbr:Batken_Region dbr:Intrusive_rock dbr:Limestone dbr:Granodiorite dbr:Conglomerate_(geology) dbr:Silurian dbr:Alay_Range dbr:Granite dbc:Batken_Region dbc:Mountain_ranges_of_Kyrgyzstan dbr:Sokh_(river) dbr:Kyrgyzstan dbr:Shale dbr:Kojashkan dbr:Kuruksay
dbp:country dbr:Kyrgyzstan
dbp:elevationM 5016 (xsd:integer)
dbp:formedBy shale, limestone, and conglomerate of Silurian and Carboniferous, and more rarely by granite and granodiorite (en)
dbp:lengthKm 31 (xsd:integer)
dbp:name Kulduk-Too (en)
dbp:subdivision dbr:Batken_District dbr:Batken_Region
dbp:subdivision2Type Regions (en)
dbp:subdivision3Type Districts (en)
dbp:widthKm 7 (xsd:integer)
dbp:wikiPageUsesTemplate dbt:Convert dbt:Coord dbt:Infobox_mountain dbt:Reflist dbt:Native_name dbt:Kyrgyzstan-geo-stub
dcterms:subject dbc:Batken_Region dbc:Mountain_ranges_of_Kyrgyzstan
georss:point 39.68333333333333 71.11666666666666
rdf:type owl:Thing dbo:Place dbo:Location schema:Mountain schema:Place dbo:NaturalPlace wikidata:Q8502 geo:SpatialThing dbo:Mountain
rdfs:comment Kulduk-Too (Kyrgyz: Кулдук-Тоо) is a northern offspur of the Alay Range in the Batken Region of Kyrgyzstan. It is located between the valley of the river Sokh and that of its tributary Kojashkan. It stretches from west to east, south of the Aydarken depression, and is connected in the east with the range. The length of the range is 31 km (19 mi), its width is 7–8 km (4.3–5.0 mi). Its average height is 4,100–4,300 m (13,500–14,100 ft), and its highest point is 5,016 m (16,457 ft). The northern slope, long and gentle, gradually descends to Sokh river and Khaidarkan depression. The southern slope, short and steep, features great variations in altitudes. Both slopes are deeply dissected by tributaries of Sokh river. The range is composed of Silurian and Carboniferous rocks: (shale, limestone, (en)
rdfs:label Kulduk-Too (en)
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geo:geometry POINT(71.116668701172 39.683334350586)
geo:lat 39.683334 (xsd:float)
geo:long 71.116669 (xsd:float)
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foaf:name Kulduk-Too (en)
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