Shindong-ri, Kilju County, North Hamgyong Province, North Koreai
| Regional Level Types | |
|---|---|
| Shindong-ri | Outcrop (Uncertain) |
| Kilju County | County |
| North Hamgyong Province | Province |
| North Korea | Country |
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Latitude & Longitude (WGS84):
41° 5' 36'' North , 129° 11' 30'' East
Latitude & Longitude (decimal):
Type:
Outcrop (Uncertain) - last checked 2026
Deposit first discovered:
1932
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Kilju | 63,652 (2012) | 18.4km |
| Hau-ri | 13,581 (2012) | 26.2km |
| Sŭngjibaegam | 11,786 (2012) | 36.8km |
| Hoemul-li | 11,681 (2012) | 55.0km |
| Kyŏngsŏng | 35,604 (2012) | 64.9km |
Other Languages:
Korean:
조선민주주의인민공화국 함경북도 길주군 신동리, 길주군, 함경북도, 조선민주주의인민공화국
Outcrop of the Hakmusan intrusive which intruded into the proterozoic Namdaechon series (Machonryong system)
The Hakmusan intrusive is a part of the tertiary Hakmusan complex, an alkaline granitoids which intruded during the opening of the rift which formed the Sea of Japan.
List of minerals for each chemical element
Other Regions, Features and Areas containing this locality
Amur PlateTectonic Plate
AsiaContinent
China
- North China OrogenOrogen
Eurasian Plate
- North China Craton
- Longgang BlockShield
Korean PeninsulaPeninsula
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