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Karasu Rift Volcano

Updated: 19 abr. 2024 10:50 GMT -
Volcanic field 486 m / 1594 ft
Turkey, 36.77°N / 36.6°E
Current status: (probably) extinct (0 out of 5)

[smaller] [larger]
Typical eruption style: unspecified
Erupciones del volcán Karasu Rift: None during the past 10,000 years
Less than few million years ago (Pleistocene)

Latest nearby earthquakes

Fecha / HoraRevista / Prof.Distancia / Ubicación
14 abr 23:51 (Istanbul)
2.5

7 km
14 km al sur Turkey: Kırıkhan (Hatay)
Más
sábado, 13 abril 2024 GMT (1 sismo)
13 abr 14:40 (Istanbul)
2.3

7 km
20 km al norte Turkey: İslahiye (Gaziantep)
Más
domingo, 7 abril 2024 GMT (1 sismo)
7 abr 08:36 (Istanbul)
1.9

7 km
28 km al suroeste Turkey: KARAAGAC-ARSUZ (HATAY)
Más
viernes, 5 abril 2024 GMT (1 sismo)
5 abr 15:46 (Istanbul)
2.3

10.4 km
17 km al norte Gaziantep, 31 km al sureste de Osmaniye, Osmaniye, Turquía
Más
lunes, 8 abril 2024 GMT (1 sismo)
8 abr 18:15 (Istanbul)
1.8

7.3 km
25 km al suroeste Turkey: Kırıkhan (Hatay)
Más
miércoles, 17 abril 2024 GMT (1 sismo)
17 abr 09:53 (Istanbul)
1.7

1.5 km
23 km al suroeste Turkey: TASOLUK-KIRIKHAN (HATAY)
Más

Background

The Quaternary basalts of the Karasu Rift form a belt covering an area 94 km long and 12-25 km wide (as revealed by boreholes) between Fevzipasa and north of Revhanli in the northern section of the rift (Rojay et al., 2001). Located near the far NE corner of the Mediterranean Sea, some of the lava field extends into Syria. One especially dark fresh-looking are of lava flows just east of the city of Hassa covers an area of about 140 km2 over a N-S distance of 20 km, and includes the low Küçükak Tepesi crater. Those flows almost surrounded the older lavas of Büyükak Tepe. K-Ar age dating by Rojay et al. (2001) on new samples showed five preiods of volcanism between 1.6 and 0.05 Ma.
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Source: Smithsonian / GVP volcano information

Latest satellite images

karasurift satellite image sat1karasurift satellite image sat2
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