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[LIVE] Ngaji Bakda Shubuh | Dr. Ir. Amien Widodo,. M.Si. | Inspirasi Al-Quran | Rabu, 30 Sept 2026

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Science and Nature

Summary of scientific concepts, discoveries, and nature phenomena

1) Earthquakes as part of a divinely governed system (Qur’anic framing)

  • The speaker links earthquakes to Qur’anic ideas that all creations have precise “measurements” (size/proportion) and operate within a structured system of natural laws.
  • Emphasis is placed on research and reflection on natural phenomena (heavens/earth, alternation of day/night) to avoid fatalism.

2) Plate tectonics and earthquake mechanisms (geoscience explanation)

  • Earth heat drives mantle convection
    • Earth’s interior heat (compared to energy from a “hot sun” in the talk) heats the mantle.
    • The mantle becomes softer and produces convection currents.
  • Convection currents move tectonic plates.
  • Earthquakes occur when plates shift and break
    • Breaking of the lithosphere / tectonic faults leads to shaking.
  • Volcanoes form from collisions and subduction-related processes
    • Collision can generate magma and lead to volcanic activity.

3) Volcanic outputs and global impacts

  • Volcanoes emit:
    • Gas, which influences atmospheric composition.
    • Ash/soil, which can contribute to fertile soils.
  • Historical examples mentioned:
    • Mount Kelud (1901): ash covered parts of Java.
    • Mount Tambora (1814): ash spread to Europe and contributed to cold conditions for months.

4) Earth as a “closed system” and human-caused climate change

  • The Earth is described as four interacting components:
    • Lithosphere, hydrosphere, atmosphere, anthroposphere
  • Atmospheric composition (as stated in the talk):
    • ~78.9% nitrogen, ~20% oxygen
  • CO₂ is described as rising, with an approximate increase from ~0.039% to ~0.415%.
  • Consequences described:
    • Global warming → climate shifts, unpredictable rain, stronger winds, higher temperatures
    • Indonesia noted as experiencing >1°C increase.

5) Disaster risk vs “destiny”: risk concepts and mitigation

  • Disasters are differentiated from ordinary hazards:
    • A disaster requires exposure and vulnerability (people/community/structures).
  • The talk stresses proactive education and adaptation:
    • Identify local earthquake hazards rather than ignoring them.
    • Adapt building styles and behaviors before events occur.
  • Example of community resilience:
    • Tsunami adaptation in Aceh using mosque architecture with hollow understructures (water passes through) and elevated evacuation spaces.

6) Earthquake impacts can be cascading (secondary disasters)

  • Earthquakes are described as more than “shaking,” including triggers such as:
    • Infrastructure damage
    • Clean water system damage
    • Fires followed by economic/social disruption
    • Health impacts
  • Soil response mentioned:
    • Liquefaction (soil loses strength and behaves like a liquid).
  • “Non-single event” framing:
    • Shaking can continue, and multiple structures may fail—including vulnerable buildings.

7) Indonesia’s tectonic setting: multiple plate pressures and megathrust risk

  • Indonesia is described as being pressured by three plates:
    • Indian Ocean plate (south)
    • Pacific Ocean plate (east)
    • Eurasian plate (north)
  • This is asserted to create earthquake-generating faults across regions.
  • Megathrust
    • A locked subduction interface that can hold strain for >200 years
    • When it releases → megathrust earthquake, potentially generating a tsunami
  • Tsunami risk emphasized for parts of southern East Java, connected to historical events, including a referenced event in 1994.

8) Seismic hazard mapping and engineering scale concepts

  • Hazard is linked to:
    • Fault locations, depth ranges, and regional geology
  • Fault depth range referenced:
    • 0 km to ~600 km (as stated)
  • Engineering analogy:
    • Testing rock strength by compressing at controlled conditions and observing crack progression.
  • Magnitude vs intensity:
    • The talk discusses magnitude scales and newer, more detailed intensity approaches that consider additional factors (including ground/land conditions), not only wave amplitude and distance.
    • The speaker claims older approaches remain broadly valid internationally.

9) Earthquake history and trend monitoring

  • The talk emphasizes studying past earthquakes to improve adaptation:
    • Recurrence and cumulative hazard.
  • Claims/trends mentioned for East Java:
    • Increasing earthquake activity across periods leading up to a major event (analogized to Japan’s March 11 sequence).
  • Data sources mentioned:
    • A national earthquake research center provides fault-line overviews.
  • Example locality detail:
    • Tremors intensify in some areas due to sediment geology (East Surabaya described as sediment-based).

10) Public beliefs and fatalism survey results (as stated)

  • A survey (Kompas cited) is described:
    • 48.5%: disasters are God’s will that cannot be avoided.
    • Another group believes disasters are natural mechanisms but “cannot be migrated.”
    • Only ~8.4% believe natural mechanisms can be mitigated.
  • The talk uses this to argue for education to increase preparedness.

Methodologies / frameworks outlined

  • Religious-to-research framework

    • Use Qur’anic passages as motivation to investigate natural phenomena scientifically.
    • Argue that creation is not “vain,” encouraging empirical study (including earthquakes).
  • Earthquake/disaster risk framework

    • Hazard exists continuously (e.g., earthquakes, storms), but disaster happens when people and vulnerability are involved.
    • Disaster understanding path:
      • Identify threats (including local earthquake-prone zones)
      • Recognize vulnerability (building practices, lack of reinforcement)
      • Mitigate through preparedness and education before events
  • Engineering adaptation approach

    • If buildings are not designed for seismic forces:
      • reinforce foundations/structure
      • reduce collapse risk
    • Use local resilient architecture as models (e.g., traditional forms, tsunami-sheltering mosque layouts).
  • Hazard assessment approach (implied)

    • Map fault zones (active vs inactive)
    • Use earthquake history and geologic context (sediment, faults, soil liquefaction risk)
    • Translate hazard into building and land-use decisions at the district level

Researchers or sources featured (named at end)

  • Dr. Ir. Amien Widodo, M.Si.
  • Kompas (survey mentioned)
  • ITS (as an institution involved in education/media in the talk)
  • Pusgen (mentioned as a geological studies center from the Geological Agency)
  • Geological Agency (Indonesia) (as source context for Pusgen)

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