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Kaltat Creek, Targhasa massif, Krasnoyarsk Krai, Russiai
| Regional Level Types | |
|---|---|
| Kaltat Creek | Creek |
| Targhasa massif | Massif |
| Krasnoyarsk Krai | Krai |
| Russia | Country |
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Latitude & Longitude (WGS84):
55° 56' 40'' North , 92° 51' 11'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Krasnoyarsk | 927,200 (2017) | 8.2km |
| Ovsyanka | 3,722 (2012) | 17.6km |
| Berëzovka | 20,913 (2018) | 18.7km |
| Zykovo | 5,365 (2013) | 19.2km |
| Solnechnyy | 10,641 (2012) | 19.5km |
The Kaltat (Russian: Калтат) is a river in Russia. It is located in the province of Krasnoyarskiy Kray, in the central part of the country, 3,400 km east of Moscow, the capital of the country. Kaltat is part of the Yenisei River watershed.
Limestones.
Fe–Si alloys (iron silicides): (unnamed) FeSi9, (unnamed) Fe3Si2, and (unnamed) Fe4Si9.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
13 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Barringerite Formula: (Fe,Ni)2P |
| ⓘ Cohenite Formula: Fe3C |
| ⓘ Hapkeite Formula: Fe2Si |
| ⓘ Linzhiite Formula: FeSi2 Description: Originally described as Ferdisilicite, renamed and redefined as linzhiite References: |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Moissanite Formula: SiC References: |
| ⓘ Naquite Formula: FeSi References: |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ Native Sulphur Formula: S8 |
| ⓘ Schreibersite Formula: (Fe,Ni)3P |
| ⓘ Silicon Formula: Si |
| ⓘ Wüstite Formula: FeO |
| ⓘ Xifengite Formula: Fe5Si3 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Cohenite | 1.BA.05 | Fe3C |
| ⓘ | Naquite | 1.BB.15 | FeSi |
| ⓘ | Linzhiite | 1.BB.20 | FeSi2 |
| ⓘ | Hapkeite | 1.BB.35 | Fe2Si |
| ⓘ | Xifengite | 1.BB.40 | Fe5Si3 |
| ⓘ | Schreibersite | 1.BD.05 | (Fe,Ni)3P |
| ⓘ | Barringerite | 1.BD.10 | (Fe,Ni)2P |
| ⓘ | Silicon | 1.CB.15 | Si |
| ⓘ | Native Sulphur | 1.CC.05 | S8 |
| ⓘ | Moissanite | 1.DA. | SiC |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Wüstite | 4.AB.25 | FeO |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Cohenite | Fe3C |
| C | ⓘ Moissanite | SiC |
| O | Oxygen | |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Wüstite | FeO |
| Si | Silicon | |
| Si | ⓘ Moissanite | SiC |
| Si | ⓘ Silicon | Si |
| Si | ⓘ Xifengite | Fe5Si3 |
| Si | ⓘ Hapkeite | Fe2Si |
| Si | ⓘ Naquite | FeSi |
| Si | ⓘ Linzhiite | FeSi2 |
| P | Phosphorus | |
| P | ⓘ Barringerite | (Fe,Ni)2P |
| P | ⓘ Schreibersite | (Fe,Ni)3P |
| S | Sulfur | |
| S | ⓘ Native Sulphur | S8 |
| Fe | Iron | |
| Fe | ⓘ Barringerite | (Fe,Ni)2P |
| Fe | ⓘ Cohenite | Fe3C |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Schreibersite | (Fe,Ni)3P |
| Fe | ⓘ Wüstite | FeO |
| Fe | ⓘ Xifengite | Fe5Si3 |
| Fe | ⓘ Hapkeite | Fe2Si |
| Fe | ⓘ Naquite | FeSi |
| Fe | ⓘ Linzhiite | FeSi2 |
| Ni | Nickel | |
| Ni | ⓘ Barringerite | (Fe,Ni)2P |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Schreibersite | (Fe,Ni)3P |
Other Databases
| Wikipedia: | https://ceb.wikipedia.org/wiki/Kaltat |
|---|---|
| Wikidata ID: | Q36184958 |
Other Regions, Features and Areas containing this locality
AsiaContinent
Eurasian PlateTectonic Plate
- Zavhan BasinVolcanic Arc
Russia
- ⭔SiberiaTraditional Region
- ⭔Siberian Federal DistrictDistrict
Soviet Union (1922-1991)Country
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
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