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The 2018 Sulawesi Earthquake and Tsunami: Geological Context and Disaster Response

At a Glance

Title: The 2018 Sulawesi Earthquake and Tsunami: Geological Context and Disaster Response

Total Categories: 7

Category Stats

  • Geological Dynamics of the Earthquake: 13 flashcards, 15 questions
  • Tsunami Dynamics and Coastal Impact: 5 flashcards, 6 questions
  • Secondary Hazards and Widespread Destruction: 3 flashcards, 2 questions
  • Humanitarian Consequences: 6 flashcards, 5 questions
  • Infrastructure Damage and Economic Toll: 8 flashcards, 6 questions
  • Disaster Response and Management: 10 flashcards, 10 questions
  • Chronological and Comparative Context: 4 flashcards, 9 questions

Total Stats

  • Total Flashcards: 49
  • True/False Questions: 26
  • Multiple Choice Questions: 27
  • Total Questions: 53

Instructions

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Welcome to Your Curriculum Command Center

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The Core Concept: What is a "Kit"?

Think of a Kit as your all-in-one digital lesson plan. It's a single, portable file that contains every piece of content for a topic: your subject categories, a central image, all your flashcards, and all your questions. The true power of the Studio is speed—once a kit is made (or you import one), you are just minutes away from printing an entire set of coursework.

Getting Started is Simple:

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Step 1: Laying the Foundation (The Authoring Tools)

This is where you build the core knowledge of your Kit. Use the left-side navigation panel to switch between these powerful authoring modules.

⚙️ Kit Manager: Your Kit's Identity

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  • Kit Name: Give your Kit a clear title. This will appear on all your printed materials.
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  • Topics: Create the structure for your lesson. Add topics like "Chapter 1," "Vocabulary," or "Key Formulas." All flashcards and questions will be organized under these topics.

🃏 Flashcard Author: Building the Knowledge Blocks

Flashcards are the fundamental concepts of your Kit. Create them here to define terms, list facts, or pose simple questions.

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Create a bank of questions to test knowledge. These questions are the engine for your worksheets and exams.

  • Click "➕ Add New Question".
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  • The Explanation field is a powerful tool: the text you enter here will automatically appear on the teacher's answer key and on the Smart Study Guide, providing instant feedback.

🔗 Intelligent Mapper: The Smart Connection

This is the secret sauce of the Studio. The Mapper transforms your content from a simple list into an interconnected web of knowledge, automating the creation of amazing study guides.

  • Step 1: Select a question from the list on the left.
  • Step 2: In the right panel, click on every flashcard that contains a concept required to answer that question. They will turn green, indicating a successful link.
  • The Payoff: When you generate a Smart Study Guide, these linked flashcards will automatically appear under each question as "Related Concepts."

Step 2: The Magic (The Generator Suite)

You've built your content. Now, with a few clicks, turn it into a full suite of professional, ready-to-use materials. What used to take hours of formatting and copying-and-pasting can now be done in seconds.

🎓 Smart Study Guide Maker

Instantly create the ultimate review document. It combines your questions, the correct answers, your detailed explanations, and all the "Related Concepts" you linked in the Mapper into one cohesive, printable guide.

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Step 3: Saving and Collaborating

  • 💾 Export & Save Kit: This is your primary save function. It downloads the entire Kit (content, images, and all) to your computer as a single .json file. Use this to create permanent backups and share your work with others.
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You're now ready to reclaim your time.

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Study Guide: The 2018 Sulawesi Earthquake and Tsunami: Geological Context and Disaster Response

Study Guide: The 2018 Sulawesi Earthquake and Tsunami: Geological Context and Disaster Response

Geological Dynamics of the Earthquake

The epicenter of the 2018 Sulawesi earthquake was located in Palu city.

Answer: False

The epicenter of the 2018 Sulawesi earthquake was located in the Donggala Regency of Central Sulawesi, approximately 70 kilometers north of Palu city.

Related Concepts:

  • When and where did the significant earthquake and tsunami event occur in 2018?: In 2018, a shallow, large earthquake struck on September 28th in the neck of the Minahasa Peninsula, Indonesia. The epicenter was located in the mountainous Donggala Regency of Central Sulawesi, impacting the region with both seismic activity and a subsequent tsunami.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.

The Palu-Koro fault is primarily a thrust fault responsible for vertical displacement.

Answer: False

The Palu-Koro fault is characterized as a left-lateral strike-slip fault, primarily accommodating horizontal movement between tectonic blocks in Sulawesi, rather than a thrust fault responsible for significant vertical displacement.

Related Concepts:

  • What specific type of geological fault is the Palu-Koro fault, and what is its estimated slip rate?: The Palu-Koro fault is characterized as a left-lateral strike-slip fault. Its estimated rate of slip is between 30 and 40 millimeters per year.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.
  • What was the role of the Palu-Koro fault in the seismic activity of the region?: The Palu-Koro fault is the main active geological structure in western Central Sulawesi. It is a significant left-lateral strike-slip fault that accommodates tectonic plate movement and has been linked to several major earthquakes in the past.

Initial magnitude estimates for the main earthquake varied between 7.5 Mw and 7.7 Mw.

Answer: True

Initial reports from agencies like the USGS and BMKG stated the mainshock magnitude as 7.7 Mw, with later revisions placing it at 7.5 Mw or 7.6 Mw by other sources.

Related Concepts:

  • What were the different magnitude estimates for the main Sulawesi earthquake from various agencies?: Initial reports from both the USGS and BMKG stated the mainshock magnitude as 7.7 Mw. The USGS later revised this to 7.5 Mw, while the International Seismological Centre (ISC) reported it as 7.6 Mw.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • How many aftershocks were recorded in the first 24 hours following the main Sulawesi earthquake?: Following the main magnitude 7.5-7.6 earthquake, there were 14 aftershocks recorded with a magnitude of 5.0 or greater within the first 24 hours.

The earthquake's rupture extended approximately 150 kilometers along the Palu-Koro fault.

Answer: True

Geodetic evidence suggests that approximately 150 kilometers of the Palu-Koro fault ruptured during the main earthquake event.

Related Concepts:

  • What was the estimated length of the fault rupture during the mainshock?: Geodetic evidence suggests that approximately 150 kilometers of the Palu-Koro fault ruptured during the main earthquake.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.

The Palu-Koro fault has a slow slip rate of less than 5 mm per year.

Answer: False

The Palu-Koro fault has an estimated slip rate of 30-40 mm per year, which is considered significant for a strike-slip fault.

Related Concepts:

  • What specific type of geological fault is the Palu-Koro fault, and what is its estimated slip rate?: The Palu-Koro fault is characterized as a left-lateral strike-slip fault. Its estimated rate of slip is between 30 and 40 millimeters per year.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.
  • What was the role of the Palu-Koro fault in the seismic activity of the region?: The Palu-Koro fault is the main active geological structure in western Central Sulawesi. It is a significant left-lateral strike-slip fault that accommodates tectonic plate movement and has been linked to several major earthquakes in the past.

The phenomenon of supershear rupture, where fault rupture exceeds shear wave speed, was definitively ruled out for this earthquake.

Answer: False

Seismic data analysis suggested the possibility of a supershear rupture, where the fault rupture propagates at speeds exceeding the shear wave velocity, indicating this phenomenon was not definitively ruled out.

Related Concepts:

  • What unusual rupture characteristic was suggested for the 2018 Sulawesi earthquake?: Analysis of seismic data indicated that the rupture propagated at speeds exceeding the S-wave velocity. This suggests the possibility of a supershear rupture, a phenomenon where fault rupture propagates faster than the shear wave speed.

Which of the following locations was identified as the epicenter of the 2018 Sulawesi earthquake?

Answer: Donggala Regency

The epicenter of the 2018 Sulawesi earthquake was located in the Donggala Regency of Central Sulawesi, approximately 70 kilometers north of Palu city.

Related Concepts:

  • When and where did the significant earthquake and tsunami event occur in 2018?: In 2018, a shallow, large earthquake struck on September 28th in the neck of the Minahasa Peninsula, Indonesia. The epicenter was located in the mountainous Donggala Regency of Central Sulawesi, impacting the region with both seismic activity and a subsequent tsunami.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.

What was the approximate magnitude of the main Sulawesi earthquake according to the USGS revised estimate?

Answer: 7.5 Mw

While initial estimates varied, the USGS later revised the magnitude of the main Sulawesi earthquake to 7.5 Mw. Other sources reported it as 7.6 Mw or initially as 7.7 Mw.

Related Concepts:

  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.

The Palu-Koro fault, associated with the earthquake, is characterized as what type of fault?

Answer: A left-lateral strike-slip fault.

The Palu-Koro fault is identified as a left-lateral strike-slip fault, which is characterized by predominantly horizontal movement along the fault line.

Related Concepts:

  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.
  • What was the role of the Palu-Koro fault in the seismic activity of the region?: The Palu-Koro fault is the main active geological structure in western Central Sulawesi. It is a significant left-lateral strike-slip fault that accommodates tectonic plate movement and has been linked to several major earthquakes in the past.
  • What specific type of geological fault is the Palu-Koro fault, and what is its estimated slip rate?: The Palu-Koro fault is characterized as a left-lateral strike-slip fault. Its estimated rate of slip is between 30 and 40 millimeters per year.

What was the estimated length of the fault rupture during the main Sulawesi earthquake?

Answer: Approximately 150 kilometers

Geodetic evidence indicates that the rupture during the main Sulawesi earthquake extended approximately 150 kilometers along the Palu-Koro fault.

Related Concepts:

  • What was the estimated length of the fault rupture during the mainshock?: Geodetic evidence suggests that approximately 150 kilometers of the Palu-Koro fault ruptured during the main earthquake.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.

What unusual characteristic of the rupture propagation was suggested by seismic data analysis?

Answer: Rupture propagation at speeds exceeding the S-wave velocity (supershear).

Seismic data analysis suggested that the rupture propagated at speeds exceeding the S-wave velocity, indicating the potential for a supershear rupture event.

Related Concepts:

  • What unusual rupture characteristic was suggested for the 2018 Sulawesi earthquake?: Analysis of seismic data indicated that the rupture propagated at speeds exceeding the S-wave velocity. This suggests the possibility of a supershear rupture, a phenomenon where fault rupture propagates faster than the shear wave speed.

How many aftershocks with a magnitude of 5.0 or greater were recorded within the first 24 hours after the main earthquake?

Answer: Exactly 14

Within the first 24 hours following the main Sulawesi earthquake, 14 aftershocks with a magnitude of 5.0 or greater were recorded.

Related Concepts:

  • How many aftershocks were recorded in the first 24 hours following the main Sulawesi earthquake?: Following the main magnitude 7.5-7.6 earthquake, there were 14 aftershocks recorded with a magnitude of 5.0 or greater within the first 24 hours.

What was the estimated slip rate of the Palu-Koro fault per year?

Answer: 30-40 mm/year

The Palu-Koro fault, a significant left-lateral strike-slip fault, has an estimated slip rate of 30 to 40 millimeters per year.

Related Concepts:

  • What specific type of geological fault is the Palu-Koro fault, and what is its estimated slip rate?: The Palu-Koro fault is characterized as a left-lateral strike-slip fault. Its estimated rate of slip is between 30 and 40 millimeters per year.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.
  • What was the estimated length of the fault rupture during the mainshock?: Geodetic evidence suggests that approximately 150 kilometers of the Palu-Koro fault ruptured during the main earthquake.

The earthquake occurred on September 28, 2018. What was the magnitude of the largest foreshock that occurred earlier on the same day?

Answer: 6.1 Mw

Earlier on September 28, 2018, a significant foreshock with a magnitude of 6.1 Mw (according to USGS) occurred, preceding the main earthquake.

Related Concepts:

  • What was the magnitude of the earthquake that struck near Palu, Indonesia, on September 28, 2018?: The earthquake that struck near Palu, Indonesia, on September 28, 2018, had a magnitude between 7.5 and 7.6 Mw (Moment Magnitude scale).
  • What was the timing and magnitude of the first significant foreshock before the main Sulawesi earthquake?: The first major foreshock occurred at 15:00 WITA (Indonesia Central Standard Time) on September 28, 2018. This earthquake had a magnitude of 5.9 Mw according to BMKG and 6.1 Mw according to the USGS, striking at a shallow depth and causing initial casualties and damage.

What was the primary function of the Palu-Koro fault mentioned in the source?

Answer: To accommodate tectonic plate movement between blocks in Sulawesi.

The Palu-Koro fault serves as a significant geological structure that accommodates the tectonic plate movement between different blocks within the island of Sulawesi.

Related Concepts:

  • What was the role of the Palu-Koro fault in the seismic activity of the region?: The Palu-Koro fault is the main active geological structure in western Central Sulawesi. It is a significant left-lateral strike-slip fault that accommodates tectonic plate movement and has been linked to several major earthquakes in the past.
  • How was the Palu-Koro fault described in terms of its geological characteristics and significance?: The Palu-Koro fault is a left-lateral strike-slip fault trending NNW-SSE, acting as a boundary between tectonic blocks in Sulawesi. It has an estimated slip rate of 30-40 mm per year and was identified in a 2017 study as representing the greatest seismic risk in eastern Indonesia.
  • What specific type of geological fault is the Palu-Koro fault, and what is its estimated slip rate?: The Palu-Koro fault is characterized as a left-lateral strike-slip fault. Its estimated rate of slip is between 30 and 40 millimeters per year.

Tsunami Dynamics and Coastal Impact

The tsunami waves that struck Palu were estimated to be consistently between 4 to 7 meters high.

Answer: False

While initial estimates by BMKG suggested wave heights between 4 to 7 meters in some areas, reports indicate that actual tsunami waves reached up to 10.7 meters in Donggala and over 2 meters in Palu, exceeding initial predictions.

Related Concepts:

  • How did Palu's geographical location potentially influence the tsunami's impact?: Palu is situated at the end of a narrow bay. This geographical feature likely intensified the tsunami's force as the waves funneled into the bay, increasing their destructive potential upon reaching the city.
  • What was the initial warning issued by Indonesian authorities after the earthquake, and how accurate were the predicted tsunami heights?: A tsunami warning was issued for the Makassar Strait and coastal areas like Palu and Donggala. While warnings predicted wave heights of less than 0.5 meters in Palu and 0.5-3 meters in Donggala, the actual tsunami waves were significantly higher, reaching over 2 meters in Palu and up to 7 meters in Donggala.
  • What natural disasters combined to cause the high casualty count in Sulawesi in September 2018?: The combined effects of the magnitude 7.5-7.6 earthquake and the subsequent tsunami led to a high number of fatalities. The tsunami struck Palu, causing widespread destruction as it swept inland.

Palu's geographical location at the end of a narrow bay helped mitigate the tsunami's impact.

Answer: False

Palu's location at the end of a narrow bay likely intensified the tsunami's impact by funneling the waves, amplifying their force and leading to more severe inundation rather than mitigating it.

Related Concepts:

  • How did Palu's geographical location potentially influence the tsunami's impact?: Palu is situated at the end of a narrow bay. This geographical feature likely intensified the tsunami's force as the waves funneled into the bay, increasing their destructive potential upon reaching the city.
  • How did the tsunami's interaction with Palu's bay shape its destructive power?: Palu's location at the end of a narrow bay acted like a funnel for the tsunami waves. This geographical feature amplified the force of the water as it entered the bay, leading to more severe inundation and destruction along the coastline.

The Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG) initially estimated tsunami wave heights to be potentially over 10 meters.

Answer: False

The BMKG initially estimated tsunami wave heights between 4 to 7 meters. Actual observed waves, particularly in Donggala, were reported to be higher, reaching up to 10.7 meters.

Related Concepts:

  • What were the estimated heights of the tsunami waves that struck the coast?: The Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG) initially estimated tsunami wave heights between 4 to 7 meters (13 to 23 feet). However, other reports indicated waves reaching up to 10.7 meters (35 feet) in Donggala Regency.
  • What was the initial warning issued by Indonesian authorities after the earthquake, and how accurate were the predicted tsunami heights?: A tsunami warning was issued for the Makassar Strait and coastal areas like Palu and Donggala. While warnings predicted wave heights of less than 0.5 meters in Palu and 0.5-3 meters in Donggala, the actual tsunami waves were significantly higher, reaching over 2 meters in Palu and up to 7 meters in Donggala.
  • What was the estimated number of people affected by the earthquake and tsunami in total?: According to Sutopo Purwo Nugroho of the Indonesian National Board for Disaster Management, approximately 2.4 million people were affected by the earthquake and tsunami.

Why did the tsunami cause particularly severe damage in Palu?

Answer: The city's location at the end of a narrow bay intensified the tsunami's force.

Palu's geographical position at the terminus of a narrow bay acted to funnel the tsunami waves, amplifying their destructive power as they reached the city.

Related Concepts:

  • How did Palu's geographical location potentially influence the tsunami's impact?: Palu is situated at the end of a narrow bay. This geographical feature likely intensified the tsunami's force as the waves funneled into the bay, increasing their destructive potential upon reaching the city.
  • How did the tsunami's interaction with Palu's bay shape its destructive power?: Palu's location at the end of a narrow bay acted like a funnel for the tsunami waves. This geographical feature amplified the force of the water as it entered the bay, leading to more severe inundation and destruction along the coastline.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.

What was the estimated height of the tallest tsunami waves reported in Donggala Regency?

Answer: 10.7 meters

Reports indicated that the tsunami waves reached an estimated height of up to 10.7 meters in the Donggala Regency.

Related Concepts:

  • What were the estimated heights of the tsunami waves that struck the coast?: The Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG) initially estimated tsunami wave heights between 4 to 7 meters (13 to 23 feet). However, other reports indicated waves reaching up to 10.7 meters (35 feet) in Donggala Regency.
  • What was the initial warning issued by Indonesian authorities after the earthquake, and how accurate were the predicted tsunami heights?: A tsunami warning was issued for the Makassar Strait and coastal areas like Palu and Donggala. While warnings predicted wave heights of less than 0.5 meters in Palu and 0.5-3 meters in Donggala, the actual tsunami waves were significantly higher, reaching over 2 meters in Palu and up to 7 meters in Donggala.

Which statement best describes the initial BMKG tsunami warning predictions compared to the actual waves?

Answer: Predictions were significantly lower than the actual waves observed.

The initial BMKG tsunami warning predictions for wave heights were significantly lower than the actual waves observed, particularly in areas like Donggala where heights exceeded 10 meters.

Related Concepts:

  • Why was the BMKG (Indonesian Agency for Meteorology, Climatology and Geophysics) criticized regarding the tsunami warning?: The BMKG faced criticism on social media because they lifted the tsunami warning after the waves had already struck. This timing led to confusion, with some believing the warning was lifted before the tsunami hit, partly due to time zone differences affecting perceptions of sunset times.

Secondary Hazards and Widespread Destruction

Soil liquefaction was a minor factor in the damage caused by the 2018 Sulawesi disaster.

Answer: False

Soil liquefaction was a major factor, causing significant destruction in areas like Petobo and Balaroa near Palu, where the ground lost strength and behaved like a liquid, leading to subsidence and engulfing structures.

Related Concepts:

  • What was the phenomenon of soil liquefaction, and where did it cause the most severe damage in the Sulawesi disaster?: Soil liquefaction is a process where saturated soil temporarily loses strength and behaves like a liquid during an earthquake. In the Sulawesi disaster, it caused immense destruction in areas like Petobo and Balaroa near Palu, where the ground essentially turned to mud, swallowing homes and structures.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.

What was the primary geological phenomenon responsible for the widespread destruction of homes in the Petobo and Balaroa areas near Palu?

Answer: Soil liquefaction causing the ground to behave like liquid mud.

The widespread destruction in Petobo and Balaroa was primarily attributed to soil liquefaction, a process where saturated ground loses its strength and behaves like a liquid during seismic events, causing subsidence and engulfing structures.

Related Concepts:

  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.
  • What was the phenomenon of soil liquefaction, and where did it cause the most severe damage in the Sulawesi disaster?: Soil liquefaction is a process where saturated soil temporarily loses strength and behaves like a liquid during an earthquake. In the Sulawesi disaster, it caused immense destruction in areas like Petobo and Balaroa near Palu, where the ground essentially turned to mud, swallowing homes and structures.
  • What was the role of the Palu-Koro fault in the seismic activity of the region?: The Palu-Koro fault is the main active geological structure in western Central Sulawesi. It is a significant left-lateral strike-slip fault that accommodates tectonic plate movement and has been linked to several major earthquakes in the past.

Humanitarian Consequences

The earthquake caused significant damage to agricultural land, affecting over 9,000 hectares.

Answer: True

The combined effects of the earthquake, tsunami, and liquefaction resulted in damage to approximately 9,718 hectares of agricultural land across Palu, Sigi, and Donggala.

Related Concepts:

  • What specific agricultural damage was reported, and what was its estimated cost?: The earthquake, tsunami, and subsequent soil liquefaction damaged 9,718 hectares of crops across Palu, Sigi, and Donggala. The estimated cost of this agricultural damage was 36 billion Indonesian rupiah.

The earthquake and tsunami caused damage to approximately 70,000 houses.

Answer: True

More than 70,000 houses were reported damaged or destroyed by the combined effects of the earthquake and tsunami, leading to widespread displacement.

Related Concepts:

  • How many houses were destroyed in total by the earthquake and tsunami?: More than 70,000 houses were reported to be damaged or destroyed as a result of the earthquake and the subsequent tsunami, displacing tens of thousands of people.
  • What was the estimated number of people affected by the earthquake and tsunami in total?: According to Sutopo Purwo Nugroho of the Indonesian National Board for Disaster Management, approximately 2.4 million people were affected by the earthquake and tsunami.
  • What was the total death toll reported for the 2018 Sulawesi earthquake and tsunami?: The combined effects of the earthquake and tsunami led to an estimated death toll of 4,340 people.

What was the estimated number of people affected in total by the earthquake and tsunami?

Answer: Approximately 2.4 million people

According to disaster management authorities, approximately 2.4 million people were affected by the combined earthquake and tsunami event.

Related Concepts:

  • What was the estimated number of people affected by the earthquake and tsunami in total?: According to Sutopo Purwo Nugroho of the Indonesian National Board for Disaster Management, approximately 2.4 million people were affected by the earthquake and tsunami.
  • What was the total death toll reported for the 2018 Sulawesi earthquake and tsunami?: The combined effects of the earthquake and tsunami led to an estimated death toll of 4,340 people.
  • How many houses were destroyed in total by the earthquake and tsunami?: More than 70,000 houses were reported to be damaged or destroyed as a result of the earthquake and the subsequent tsunami, displacing tens of thousands of people.

What was the estimated total number of deaths resulting from the earthquake and tsunami?

Answer: Around 4,340

The official estimated death toll from the combined earthquake and tsunami event is approximately 4,340 fatalities.

Related Concepts:

  • What was the total death toll reported for the 2018 Sulawesi earthquake and tsunami?: The combined effects of the earthquake and tsunami led to an estimated death toll of 4,340 people.
  • What was the estimated number of people affected by the earthquake and tsunami in total?: According to Sutopo Purwo Nugroho of the Indonesian National Board for Disaster Management, approximately 2.4 million people were affected by the earthquake and tsunami.
  • How many houses were destroyed in total by the earthquake and tsunami?: More than 70,000 houses were reported to be damaged or destroyed as a result of the earthquake and the subsequent tsunami, displacing tens of thousands of people.

How many houses were reported damaged or destroyed in total by the earthquake and tsunami?

Answer: More than 70,000

The combined earthquake and tsunami caused damage to over 70,000 houses, leading to significant displacement and a severe housing crisis in the affected regions.

Related Concepts:

  • How many houses were destroyed in total by the earthquake and tsunami?: More than 70,000 houses were reported to be damaged or destroyed as a result of the earthquake and the subsequent tsunami, displacing tens of thousands of people.
  • What was the estimated number of people affected by the earthquake and tsunami in total?: According to Sutopo Purwo Nugroho of the Indonesian National Board for Disaster Management, approximately 2.4 million people were affected by the earthquake and tsunami.
  • What was the total death toll reported for the 2018 Sulawesi earthquake and tsunami?: The combined effects of the earthquake and tsunami led to an estimated death toll of 4,340 people.

Infrastructure Damage and Economic Toll

Over 500 wireless communication towers were undamaged by the earthquake.

Answer: False

The earthquake caused significant disruption to communication infrastructure, with reports indicating that over 500 wireless communication towers were damaged, leading to widespread blackouts and communication failures.

Related Concepts:

  • What was the immediate aftermath of the main Sulawesi earthquake regarding infrastructure?: Following the mainshock, blackouts occurred throughout the affected area, and telecommunications were disrupted. More than 500 wireless communication towers were reported damaged by the earthquake, severely hindering communication efforts.

The Kuning Ponulele Bridge, destroyed in the disaster, was the second arch bridge built in Indonesia.

Answer: False

The Kuning Ponulele Bridge, also known as Palu IV Bridge, was destroyed in the disaster. It held the distinction of being the first arch bridge built in Indonesia, not the second.

Related Concepts:

  • Which iconic bridge in Palu was destroyed, and what was its significance?: Palu's iconic Kuning Ponulele Bridge, also known as Palu IV Bridge, was destroyed. This bridge held the distinction of being the first arch bridge built in Indonesia.

The disaster significantly impacted the prison system in Donggala, leading to the escape of nearly all inmates.

Answer: False

The Donggala Penitentiary's walls collapsed due to the earthquake, and over half of its inmates escaped. While significant, it was not 'nearly all' inmates, and the escape was a consequence of structural damage and subsequent chaos.

Related Concepts:

  • What was the reported impact on the prison system in Donggala?: The Donggala Penitentiary suffered severe damage, with its walls collapsing. In the chaos following the earthquake, over half of its 560 inmates escaped, and a riot broke out as prisoners demanded to see their families.

What was the estimated economic damage caused by the combined disasters of the earthquake, tsunami, and liquefaction?

Answer: Approximately Rp 24.6 trillion (US$1.71 billion)

The total estimated economic damage resulting from the earthquake, tsunami, and liquefaction was approximately Rp 24.6 trillion (US$1.71 billion), with Palu city accounting for the majority of this figure.

Related Concepts:

  • What specific agricultural damage was reported, and what was its estimated cost?: The earthquake, tsunami, and subsequent soil liquefaction damaged 9,718 hectares of crops across Palu, Sigi, and Donggala. The estimated cost of this agricultural damage was 36 billion Indonesian rupiah.
  • What was the estimated total economic damage caused by the earthquake, tsunami, and liquefaction?: The overall damage from the combined disasters was estimated at Rp 24.6 trillion (approximately US$1.71 billion). The city of Palu alone accounted for Rp 23.9 trillion (US$1.66 billion) of this total.

Which of the following was NOT reported as a collapsed structure in Palu due to the disaster?

Answer: The Indonesian Presidential Palace

While Antapura Hospital, the Roa-Roa Hotel, and the Mutiara SIS Al-Jufrie Airport Control Tower were reported as collapsed or severely damaged, the Indonesian Presidential Palace was not listed among the structures destroyed by the earthquake and tsunami.

Related Concepts:

  • Which iconic bridge in Palu was destroyed, and what was its significance?: Palu's iconic Kuning Ponulele Bridge, also known as Palu IV Bridge, was destroyed. This bridge held the distinction of being the first arch bridge built in Indonesia.
  • How were religious sites affected by the disaster in Palu?: Many religious sites suffered damage. Of the 24 mosques in Palu, 20 were severely damaged, although the Floating Mosque of Palu survived, albeit partially submerged. The Baiturrahman Mosque was particularly hard-hit, with reports of 300 worshippers killed during evening prayers.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.

What happened to the Donggala Penitentiary following the earthquake?

Answer: Its walls collapsed, and a significant number of inmates escaped.

The Donggala Penitentiary sustained severe damage, with its walls collapsing, leading to the escape of over half of its inmates amidst the ensuing chaos.

Related Concepts:

  • What was the reported impact on the prison system in Donggala?: The Donggala Penitentiary suffered severe damage, with its walls collapsing. In the chaos following the earthquake, over half of its 560 inmates escaped, and a riot broke out as prisoners demanded to see their families.

Disaster Response and Management

The tsunami detectors in Palu functioned correctly and issued timely alarms.

Answer: False

The tsunami detectors in Palu were damaged by the earthquake and failed to transmit signals, meaning official tsunami alarms were not activated, leaving many residents unaware of the impending danger.

Related Concepts:

  • What critical infrastructure failed to function as intended during the tsunami warning?: The tsunami detectors in Palu were damaged by the earthquake and failed to send signals to alert residents. This critical failure meant that official tsunami alarms were not activated, leaving many, including festival attendees on the beach, unaware of the imminent danger.

The Indonesian government decided to bury identified victims in mass graves primarily to save space.

Answer: False

The primary reason cited for the government's decision to bury identified victims in mass graves was to prevent the potential spread of diseases, given the scale of the disaster and the number of deceased.

Related Concepts:

  • What measures were taken by the Indonesian government regarding the deceased due to fears of disease spread?: Fearing the potential spread of diseases, the Indonesian government decided to bury identified victims in mass graves. They prepared at least one large grave site and planned for more as the scale of the tragedy became apparent.

The BMKG faced criticism for lifting the tsunami warning before the waves had struck Palu.

Answer: False

The BMKG faced criticism primarily because they lifted the tsunami warning after the waves had already impacted the coast, leading to confusion about the timing of the warning system's effectiveness.

Related Concepts:

  • Why was the BMKG (Indonesian Agency for Meteorology, Climatology and Geophysics) criticized regarding the tsunami warning?: The BMKG faced criticism on social media because they lifted the tsunami warning after the waves had already struck. This timing led to confusion, with some believing the warning was lifted before the tsunami hit, partly due to time zone differences affecting perceptions of sunset times.

Telecommunication companies like Telkom Indonesia provided free WiFi and communication services in affected areas.

Answer: True

Telecommunication providers, including Telkom Indonesia and Indosat Ooredoo, offered crucial support by providing free WiFi and SMS services to help affected individuals connect with their families and access information.

Related Concepts:

  • How did telecommunication companies contribute to the recovery efforts?: Several telecommunication companies provided crucial support. Telkom Indonesia offered free WiFi and telecommunication services, while Indosat Ooredoo allowed free SMS services in the affected areas to help people connect with loved ones and access information.
  • How did the Indonesian government coordinate the response to the disaster?: President Joko Widodo immediately ordered the Coordinating Minister of Politics, Legal, and Security Affairs to lead relief efforts. He also mobilized the Indonesian National Armed Forces and declared the event a major disaster, while also visiting the affected areas.

The Indonesian government initially denied reports of looting in the disaster areas.

Answer: True

Initially, some government officials and the President refuted claims of widespread looting. However, the situation evolved, and authorities later ordered police action against looters.

Related Concepts:

  • How did the Indonesian government coordinate the response to the disaster?: President Joko Widodo immediately ordered the Coordinating Minister of Politics, Legal, and Security Affairs to lead relief efforts. He also mobilized the Indonesian National Armed Forces and declared the event a major disaster, while also visiting the affected areas.

Aid delivery was smooth due to undamaged infrastructure and sufficient airport capacity.

Answer: False

Aid delivery faced significant challenges due to widespread destruction of roads and the limited capacity of Palu's airport to handle the influx of materials, causing considerable delays.

Related Concepts:

  • What challenges hindered the delivery of international aid to the affected areas?: Aid deliveries were significantly hampered by the extensive destruction of local infrastructure, including roads. Palu's airport also lacked the capacity to handle the large influx of materials, leading to severe delays in distributing essential supplies.

What was the primary reason cited for the Indonesian government's decision to bury identified victims in mass graves?

Answer: To prevent the potential spread of diseases.

The Indonesian government decided to bury identified victims in mass graves primarily as a public health measure to prevent the potential spread of diseases following the disaster.

Related Concepts:

  • What measures were taken by the Indonesian government regarding the deceased due to fears of disease spread?: Fearing the potential spread of diseases, the Indonesian government decided to bury identified victims in mass graves. They prepared at least one large grave site and planned for more as the scale of the tragedy became apparent.

Which statement accurately describes the initial government response to reports of looting?

Answer: Authorities initially refuted claims of widespread looting.

Initially, authorities and the President denied widespread looting. However, the government later directed police to apprehend looters and clarified the situation regarding the taking of essential items.

Related Concepts:

  • What was the government's initial stance on reports of looting, and how did it change?: Initially, authorities and the President refuted claims of widespread looting, with some officials even suggesting that taking essential items was permissible for 'emergency purposes'. However, as the situation became clearer, the government ordered the police to capture looters and later clarified that the government would compensate for essential items taken from stores.

What challenge did international aid delivery face due to Palu's airport?

Answer: The airport lacked the capacity to handle the large influx of materials.

Palu's airport, while operational, lacked the necessary capacity to manage the large volume of international aid materials arriving, significantly hindering the distribution process.

Related Concepts:

  • What challenges hindered the delivery of international aid to the affected areas?: Aid deliveries were significantly hampered by the extensive destruction of local infrastructure, including roads. Palu's airport also lacked the capacity to handle the large influx of materials, leading to severe delays in distributing essential supplies.

What was the initial emergency period declared in Central Sulawesi following the disaster?

Answer: 14 days

An initial emergency period of 14 days was declared in Central Sulawesi following the earthquake and tsunami, commencing on September 28, 2018.

Related Concepts:

  • What was the duration of the initial emergency period declared in Central Sulawesi, and was it extended?: An initial 14-day emergency period was declared in Central Sulawesi starting September 28, 2018. This period was later extended to October 26, 2018, reflecting the ongoing need for disaster management and recovery efforts.
  • How did the Indonesian government coordinate the response to the disaster?: President Joko Widodo immediately ordered the Coordinating Minister of Politics, Legal, and Security Affairs to lead relief efforts. He also mobilized the Indonesian National Armed Forces and declared the event a major disaster, while also visiting the affected areas.

Chronological and Comparative Context

The 2018 Sulawesi earthquake occurred on the anniversary of the 2006 Yogyakarta earthquake.

Answer: False

While both were significant Indonesian earthquakes, the 2018 Sulawesi earthquake did not occur on the anniversary of the 2006 Yogyakarta earthquake. The Sulawesi event occurred on September 28, 2018.

Related Concepts:

  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.

The main Sulawesi earthquake occurred during the morning commute.

Answer: False

The main earthquake struck at 18:02 WITA (6:02 PM local time), which is during the evening rush hour, not the morning commute.

Related Concepts:

  • What was the significance of the mainshock's timing in relation to local events?: The mainshock occurred at 18:02 WITA, during the evening rush hour. Coincidentally, it happened on the 40th anniversary of Palu city, a time when a festival (Palu Nomoni Festival) was being held, attracting many people to the coastal areas.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.

The 2018 Sulawesi earthquake was the deadliest earthquake worldwide in that year.

Answer: True

The 2018 Sulawesi earthquake and tsunami event was indeed the deadliest earthquake worldwide in 2018, surpassing other significant seismic events that year.

Related Concepts:

  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.
  • When and where did the significant earthquake and tsunami event occur in 2018?: In 2018, a shallow, large earthquake struck on September 28th in the neck of the Minahasa Peninsula, Indonesia. The epicenter was located in the mountainous Donggala Regency of Central Sulawesi, impacting the region with both seismic activity and a subsequent tsunami.

The earthquake occurred on the 40th anniversary of Palu city.

Answer: True

The main earthquake struck on September 28, 2018, which coincided with the 40th anniversary of Palu city. A festival was being held at the time, drawing many people to the coastal areas.

Related Concepts:

  • What was the significance of the mainshock's timing in relation to local events?: The mainshock occurred at 18:02 WITA, during the evening rush hour. Coincidentally, it happened on the 40th anniversary of Palu city, a time when a festival (Palu Nomoni Festival) was being held, attracting many people to the coastal areas.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.

The earthquake reached an intensity of MMI X (Extreme) in some parts of Palu City.

Answer: True

The earthquake reached an intensity of MMI X (Extreme) in certain areas of Palu City, indicating severe ground shaking and widespread structural damage.

Related Concepts:

  • What was the highest intensity level recorded for the 2018 Sulawesi earthquake, and where was it felt?: The earthquake reached an intensity of MMI X (Extreme) in some parts of Palu City. In other areas of Palu, intensities ranged from MMI VII to IX, depending on the type and extent of damage to buildings and infrastructure like bridges.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.
  • What was the magnitude of the earthquake that struck near Palu, Indonesia, on September 28, 2018?: The earthquake that struck near Palu, Indonesia, on September 28, 2018, had a magnitude between 7.5 and 7.6 Mw (Moment Magnitude scale).

How did the 2018 Sulawesi earthquake rank in terms of deadliness compared to other global earthquakes in the same year?

Answer: It was the deadliest earthquake worldwide in 2018.

The 2018 Sulawesi earthquake and tsunami event was the deadliest earthquake globally in that year, surpassing other significant seismic events such as the Lombok earthquake.

Related Concepts:

  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.

What significant events were occurring in Palu at the time of the main earthquake?

Answer: The city's 40th anniversary celebration and a festival.

The main earthquake occurred on the 40th anniversary of Palu city, during a time when a festival, the Palu Nomoni Festival, was being held, drawing many people to the coastal areas.

Related Concepts:

  • What was the significance of the mainshock's timing in relation to local events?: The mainshock occurred at 18:02 WITA, during the evening rush hour. Coincidentally, it happened on the 40th anniversary of Palu city, a time when a festival (Palu Nomoni Festival) was being held, attracting many people to the coastal areas.
  • What natural disasters combined to cause the high casualty count in Sulawesi in September 2018?: The combined effects of the magnitude 7.5-7.6 earthquake and the subsequent tsunami led to a high number of fatalities. The tsunami struck Palu, causing widespread destruction as it swept inland.
  • What significant geological phenomenon occurred in Palu and its surrounding areas due to the earthquake?: The earthquake caused major soil liquefaction in and around Palu. This phenomenon, where saturated soil temporarily loses strength and behaves like a liquid, led to widespread subsidence and the submergence of buildings in mudflows.

The earthquake's tremors were felt as far away as which Malaysian city?

Answer: Tawau

The seismic tremors from the 2018 Sulawesi earthquake were felt across a wide area, including as far away as Tawau in Malaysia.

Related Concepts:

  • How widely were the seismic effects of the 2018 Sulawesi earthquake felt?: The earthquake's tremors were felt across a considerable distance. They were perceptible as far away as Samarinda in East Kalimantan, Indonesia, and even in Tawau, Malaysia.

The event was the deadliest earthquake in Indonesia since which previous event?

Answer: The 2006 Yogyakarta earthquake.

The 2018 Sulawesi earthquake and tsunami was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake.

Related Concepts:

  • How did the 2018 Sulawesi earthquake and tsunami compare in deadliness to other events in Indonesia and globally?: The event was the deadliest earthquake to strike Indonesia since the 2006 Yogyakarta earthquake. It also became the deadliest earthquake worldwide in 2018, surpassing the Lombok earthquake that occurred nearly two months earlier.
  • What was the magnitude of the 2018 Sulawesi earthquake, and how far was its epicenter from Palu?: The earthquake had a magnitude ranging from 7.5 to 7.6 Mw. Its epicenter was approximately 70 kilometers (43 miles) away from Palu, the provincial capital of Central Sulawesi.
  • What natural disasters combined to cause the high casualty count in Sulawesi in September 2018?: The combined effects of the magnitude 7.5-7.6 earthquake and the subsequent tsunami led to a high number of fatalities. The tsunami struck Palu, causing widespread destruction as it swept inland.

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