Lewati ke konten utama
← Kembali ke peta
⇄ Bandingkan

Gunung Kawi

Kawi-Butak

Stratovolkan · Indonesia · 2651 m

The broad Kawi-Butak volcanic massif rises above rice paddies below its SW flank. The forested volcano lies immediately east of Kelud volcano and south of Arjuno-Welirang volcano. The high point of the complex is flat-topped Gunung Butak on the right horizon. Gunung Kawi (left-center) was constructed to the NW of Butak. Both are primarily of Holocene age.
The broad Kawi-Butak volcanic massif rises above rice paddies below its SW flank. The forested volcano lies immediately east of Kelud volcano and south of Arjuno-Welirang volcano. The high point of the complex is flat-topped Gunung Butak on the right horizon. Gunung Kawi (left-center) was constructed to the NW of Butak. Both are primarily of Holocene age. · Foto: Photo by Lee Siebert, 2000 (Smithsonian Institution). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Indonesia
Wilayah
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Ketinggian
2651 m
Koordinat
-7.920, 112.450
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
No Data (checked)
Ringkasan geologi

The broad Kawi-Butak volcanic massif lies immediately E of Kelut volcano and S of Arjuno-Welirang volcano. Gunung Kawi was constructed to the NW of Gunung Butak. No historical eruptions are known from either volcano, but both are primarily of Holocene age.

Ringkasan Wikipedia

Gunung Kawi adalah sebuah gunung berapi yang sudah lama tidak aktif, berada sebelah barat daya di Kabupaten Malang, berbatasan langsung dengan Kabupaten Blitar Jawa Timur, Indonesia, Tidak ada catatan sejarah mengenai letusan gunung berapi ini. Gunung ini cukup dikenal karena adanya tempat ziarah Pesarean Gunung Kawi.

Wikipedia · CC BY-SA · Baca artikel lengkap →

Riwayat letusan

Garis waktu rinci

Tidak ada catatan letusan.

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.