The official name for this volcano complex is still a debate, due to Bur ni Geureudong and Bur ni Telong’s adjacent positions. Two volcanic cones are ‘Salah Nama’ and ‘Pepanji’ which is a hill of sediment.
The Mount Bur ni Geureudong volcano has been landslide since Pleitosin, but has Fumaroles and Hot springs on the slopes. While Bur ni Telong is located south of Bur ni Geureundong. Bur ni Telong has an active crater that still has lava on the southern slopes of the mountain.
Mount Geureudong is a mountain for the Aceh Tribe, while Bur ni Telong is called by the Gayo tribe. This mountain by local people is also often referred to as Bur ni Cempege which in Gayo language means the mountain full of sulfur.
Nanggroe Aceh Darussalam;
Kabupaten Bener Meriah
Kecamatan Timang Gajah
Kecamatan Pintu Rime Gayo
a volcano/ active
Pleistosen (Mt. Bur ni Geureudong)
Desember 7,1924 (Mt. Bur ni Telong)
last erruption …?1937 (Mt. Bur ni Telong)
Elevation (meters above sea level);
Mt. Burni Telong 2.600 (…?ft)
Mt. Burni Geureudong …?
The morphology of Bur Ni Telong mountains flourishes south, southeast and southwest, while the south is slightly blocked by small hills on the slopes. This is due to the north and east growth of Bur Ni Telong’s body obstructed by the complex of Mount Geurodong, Gunung Leui Kucak and Gunung Panji.
The pattern of the river flow is also strongly influenced by the morphology that formed it, part of the river flow around the peak showed a catchment area patterned radier and semi dendritic flow, but downstream turned into parallel.
The peak area of Bur Ni Telong has a coarse-grained morphology composed of cone remnants and lava domes that are partially destroyed by eruptions in the past so that when seen from a distance it appears jagged. The top and upper slopes have a steep slopes angle, and based on the current point of activity towards Mount Bur Ni Telong open westwards. The former crater located in the southeast at this time does not show its activity.
Potensi Panas Bumi Indonesia, Jilid I 2017, halaman 3; Ditjen EBTKE dan Badan Geologi, Kementerian ESDM (link: drive.google.com)
Geological Structure Causes of the Rise in Burni Telong Manifestations, Bener Meriah, Central Aceh, Indonesia; Gartika Setiya Nugraha (Lecturer, Department of Geology Engineering, Faculty of Engineering, Syiah Kuala University, Banda Aceh, Indonesia); Marwan Ebubakar (Lecturer, Geophysics Section, Department of Physics, Faculty of Mathematics and Natural Sciences, Syiah Kuala University, Banda Aceh, Indonesia-Lecturer, Department of Geophysics Engineering. Faculty of Engineering, Syiah Kuala University, Banda Aceh, Indonesia); Dr. Susanti Alawiyah (Lecturer, Department of Physics Engineering, Faculty of Mining and Petroleum Engineering Institut Teknologi Bandung, Bandung, Indonesia); Dr. Sutopo (Lecturer, Department of Petroleum Engineering, Faculty of Mining and Petroleum Engineering Institut Teknologi Bandung, Bandung, Indonesia); EJGE 2016 (link: drive.google.com)
Kerapatan Edelweis (Anaphalis javanica) Di Gunung Burni Telong Bener Meriah, Density Edelweis (Anaphalis javanica) In Mountain Burni Telong Bener Meriah; Milda Gemasih (Mahasiswa), Djufri (Pembimbing I), Supriatno (Pembimbing II), Jurusan Pendidikan Biologi, Fkip Universitas Syiah Kuala, Jurnal Ilmiah Mahasiswa Fakultas Keguruan dan Ilmu Pendidikan Unsyiah Vol 2, No 1 (2017); Pebruari 2017 (link: drive.google.com)
Klasifikasi Tanah Di Lereng Selatan Gunung Burni Telong Kecamatan Bukit Kabupaten Bener Meriah Provinsi Aceh; Thasniema Putri (Corresponding author), Purba Marpaung, Razali (Program Studi Agroteknologi, Fakultas Pertanian, USU, Medan), Jurnal Online Agroekoteknologi . ISSN No. 2337- 6597
Vol.3, No.1 : 264 – 275 Desember 2015 (link: drive.google.com)