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Mount Lewotobi in Indonesia East Nusa Tenggara erupted spewing a 3,500 metre ash column & prompting orange-level aviation alerts, evacuation advisories & safety warnings for residents near active volcano.
| 
 Feature  | 
 Details  | 
| 
 Location  | 
 Flores Island, East Nusa Tenggara province, Indonesia  | 
| 
 Coordinates  | 
 Approximately 8.5° S, 122.8° E  | 
| 
 Type  | 
 Stratovolcano (composite volcano)  | 
| 
 Composition  | 
 Andesitic to basaltic andesite  | 
| 
 Part of  | 
 Pacific Ring of Fire  | 
| 
 Peaks  | 
 Two main peaks Lewotobi Lakilaki (1584 m) & Lewotobi Perempuan (1703 m)  | 
| 
 Separation  | 
 2 km separated by a saddle of 1232 m elevation  | 
| 
 Crater Features  | 
 Lakilaki 400 m wide open to north; Perempuan 700 m wide  | 
| 
 Flank Cone  | 
 Iliwokar on east flank of Lewotobi Perempuan  | 
| 
 Historical Eruptions  | 
 Lakilaki Frequent activity in 19th–20th century; Perempuan Only two historical eruptions  | 
| 
 2024 Activity  | 
 Major eruption with ash plumes up to 8,000 m; aviation warning issued (Orange Level)  | 
| 
 Volcanic Hazards  | 
 Ashfall, hot clouds, lava flows, lahars during rainfall  | 
| 
 Local Response  | 
 6 km exclusion zone; facemask advisory; aviation rerouting below 5,000 m  | 
| 
 Nearby Settlement Risk  | 
 High due to proximity of human habitation & farming communities  | 
| 
 Feature  | 
 Details  | 
| 
 Type  | 
 Major tectonic plate  | 
| 
 Boundaries  | 
 Converges with Indian, Arabian & Philippine Sea plates  | 
| 
 Interaction with Indo-Australian Plate  | 
 Subduction of Indo-Australian Plate beneath Eurasian Plate creates volcanic arcs  | 
| 
 Relevance to Indonesia  | 
 Forms northern boundary; causes volcanism & earthquakes  | 
| 
 Geological Significance  | 
 Part of complex Sunda Arc tectonic interaction  | 
| 
 Feature  | 
 Details  | 
| 
 Type  | 
 Major tectonic plate  | 
| 
 Boundary Type  | 
 Convergent (subducts under Eurasian Plate)  | 
| 
 Motion Direction  | 
 Northward at ~7 cm/year  | 
| 
 Interaction with Indonesia  | 
 Responsible for Sunda Trench & volcanic arc in Java-Sumatra chain  | 
| 
 Importance  | 
 Drives seismicity in southern Indonesian region  | 
| 
 Feature  | 
 Details  | 
| 
 Type  | 
 Largest tectonic plate  | 
| 
 Motion Direction  | 
 Westward movement  | 
| 
 Plate Boundaries  | 
 Interacts with Philippine Sea, North American & Indo-Australian plates  | 
| 
 Indonesia Relevance  | 
 Less direct than Eurasian/Australian but contributes to broader Pacific seismicity  | 
| 
 Key Feature  | 
 Dominates Ring of Fire encircling Pacific Basin  | 
| 
 Feature  | 
 Details  | 
| 
 Location  | 
 Extends from northern Sumatra through Java, Bali, Lombok, Sumbawa, Flores, to Banda Sea  | 
| 
 Tectonic Setting  | 
 Formed by subduction of Indo-Australian Plate beneath Eurasian Plate  | 
| 
 Arc Type  | 
 Continental volcanic arc  | 
| 
 Length  | 
 Over 3,000 km  | 
| 
 Key Islands  | 
 Sumatra, Java, Bali, Lombok, Sumbawa, Flores, Wetar  | 
| 
 Oceanic Feature  | 
 Lies above Sunda Trench a major subduction zone  | 
| 
 Major Volcanoes  | 
 Mount Merapi, Mount Agung, Mount Bromo, Mount Rinjani, Mount Tambora, Mount Lewotobi  | 
| 
 Plate Interaction  | 
 Indo-Australian Plate (subducting) & Eurasian Plate (overriding)  | 
| 
 Volcanic Activity  | 
 High includes several of world’s most explosive & active volcanoes  | 
| 
 Hazards  | 
 Earthquakes, tsunamis, pyroclastic flows, lahars, ashfall, volcanic lightning  | 
| 
 Most Famous Eruption  | 
 Mount Tambora (1815) largest eruption in recorded history; caused “Year Without a Summer”  | 
| 
 Modern Monitoring  | 
 Managed by Indonesia PVMBG (Volcanology & Geological Hazard Mitigation Centre)  | 
| 
 Geological Importance  | 
 Vital for understanding plate tectonics, subduction volcanism & hazard mitigation  | 
| 
 Aspect  | 
 Details  | 
| 
 Subduction Zone  | 
 Indo-Australian Plate descends below Eurasian Plate  | 
| 
 Trench System  | 
 Sunda Trench (a deep oceanic trench parallel to arc)  | 
| 
 Magma Generation  | 
 Caused by water-rich oceanic crust melting in mantle wedge forming andesitic magma  | 
| 
 Seismicity  | 
 Frequent earthquakes due to plate movement; includes megathrust & deep-focus quakes  | 
| 
 Tsunami Potential  | 
 High especially where underwater quakes rupture sea floor (e.g., 2004 Indian Ocean Tsunami)  | 
| 
 Banda Arc Connection  | 
 The eastern end transitions into complex Banda Arc involving multiple microplates  | 
| 
 Economic Impact  | 
 Affects agriculture, infrastructure & human settlement due to fertile soils but high risk  | 
| 
 Volcano  | 
 Island  | 
 Elevation (m)  | 
 Last Major Eruption  | 
 Notes  | 
| 
 Mount Merapi  | 
 Java  | 
 2,963  | 
 2023  | 
 Most active volcano in Indonesia  | 
| 
 Mount Tambora  | 
 Sumbawa  | 
 2,850 (after 1815)  | 
 1815  | 
 Deadliest eruption in history  | 
| 
 Mount Agung  | 
 Bali  | 
 3,031  | 
 2019  | 
 Known for 1963 catastrophic eruption  | 
| 
 Mount Rinjani  | 
 Lombok  | 
 3,726  | 
 2016  | 
 Second highest in Indonesia  | 
| 
 Mount Lewotobi  | 
 Flores  | 
 1,703 / 1,584  | 
 2024  | 
 Twin volcano, recent aviation alerts issued  | 
For more such articles, please refer to IAS GYAN
Sources:
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 PRACTICE QUESTION Q. Sunda Arc exemplifies dynamic interaction of tectonic plates shaping Southeast Asian geography & hazards. Examine geological significance & implications of volcanic activity along Sunda Arc for regional disaster preparedness.  | 
								
								
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