Ciomadul
Sign in to saveCiomadul () is a dormant volcano in Romania. It is in the Eastern Carpathians, between the spa towns of Băile Tușnad and Balvanyos. Ciomadul lies at the southeastern end of the Carpathian volcanic chain and it is the youngest volcano of the Carpatho-Pannonian region. Ciomadul consists of several lava domes with two embedded explosion craters known as Mohoș and Sfânta Ana, the latter of which contains a crater lake, Lake Sfânta Ana. The dominant volcanic rock at Ciomadul is potassium-rich dacite.
Key facts
- Mountain.name
- Ciomadul
- Mountain.other_name
- Csomád (hu)
- Mountain.photo
- Lacul Sfanta Ana - Relief.jpg
- Mountain.photo_caption
- 3D model of Ciomadul's central sector seen from the south
- Mountain.map
- Romania
- Mountain.location
- Romania, Harghita County
- Mountain.elevation_m
- 1289
- Mountain.range
- Carpathian Mountains
- Mountain.type
- Lava domes
- Mountain.age
- Pleistocene
- Mountain.volcanic_belt
- Carpathian volcanic arc
via Wikipedia infobox
Article
13 sectionsContents
- Geography and geology
- Regional setting
- Volcano
- Composition
- Eruptive history
- Tephras
- Recent explosive activity
- Current status
- Future activity
- Climate and vegetation
- References
- Bibliography
- External links
Ciomadul () is a dormant volcano in Romania. It is in the Eastern Carpathians, between the spa towns of Băile Tușnad and Balvanyos. Ciomadul lies at the southeastern end of the Carpathian volcanic chain and it is the youngest volcano of the Carpatho-Pannonian region. Ciomadul consists of several lava domes with two embedded explosion craters known as Mohoș and Sfânta Ana, the latter of which contains a crater lake, Lake Sfânta Ana. The dominant volcanic rock at Ciomadul is potassium-rich dacite.
Volcanic activity at Ciomadul commenced with effusive activity about one million years ago. Most of the volcano was constructed between 650,000 – 500,000 years ago.