2023 Global Seismic Event Analysis
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Questions and Answers

What type of seismic activity was recorded over the nine-day period?

  • Slow, constant waves (correct)
  • Intermittent bursts
  • Pulsating vibrations
  • Quick, sharp waves

What triggered the initial seismic signals in the Dickson Fjord?

  • A landslide and tsunami (correct)
  • Heavy rainfall
  • An underwater volcano
  • Tectonic plate movement

How much rock and ice was dumped into the fjord as a result of the landslide?

  • 30 million cubic yards
  • 40 million cubic yards
  • 33 million cubic yards (correct)
  • 50 million cubic yards

What height did the tsunami reach after the landslide?

<p>650 feet (C)</p> Signup and view all the answers

What caused the prolonged seismic activity after the tsunami?

<p>Seiche in the fjord (B)</p> Signup and view all the answers

What was the role of the high-resolution sonar survey conducted by the Danish Navy?

<p>To reveal the behavior of the tsunami (B)</p> Signup and view all the answers

Where did the landslide occur in relation to the fjord?

<p>200 km inland (B)</p> Signup and view all the answers

Who led the international team investigating the seismic event?

<p>Dr. Kristian Svennevig (D)</p> Signup and view all the answers

Flashcards

The 9-day seismic signal

The slow, constant wave that was recorded by earthquake sensors for nine days in 2023, unlike typical earthquake readings which are quick and sharp.

Cause of the 9-day seismic signal

The seismic signal that lasted for nine days was caused by a landslide and the resulting tsunami in the Dickson Fjord in East Greenland.

Scale of the East Greenland landslide

The landslide caused about 33 million cubic yards of rock and ice to fall into the Dickson Fjord, triggering a 650-foot-tall tsunami.

Seiche in the Dickson Fjord

The tsunami created a standing wave, known as a seiche, by bouncing back and forth in the confined space of the narrow fjord.

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Standing wave (seiche)

A standing wave, or seiche, is a type of wave where the oscillations are trapped between two boundaries, leading to a stationary appearance.

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Impact of the seiche

The seiche in the Dickson Fjord, caused by the tsunami, was powerful enough to create a seismic signal that shook the entire Earth for nine days.

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Location of the landslide

The landslide that caused the tsunami happened about 200 km inland from the open ocean.

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Scientific methods used to investigate the event

Scientists used high-resolution sonar surveys to analyze the fjord and pinpoint the cause of the 9-day seismic signal.

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Study Notes

Mysterious Global Seismic Event of 2023 Explained

  • A slow, sustained seismic wave, lasting nine days in September 2023, puzzled scientists globally. Unlike typical earthquakes, this event exhibited a continuous, unusual pattern.

Origin of the Seismic Rumble

  • The epicenter of the event was traced to a landslide in Dickson Fjord, East Greenland.
  • A massive landslide on September 16, 2023, involved approximately 33 million cubic yards of rock and ice.
  • The landslide triggered a 650-foot-tall tsunami, exceeding recent historical heights.

The Role of the Fjord in the Event

  • The narrow geometry of the fjord trapped the mega-tsunami wave, creating a standing wave effect (seiche).
  • This standing wave, intensely concentrated in the fjord, reverberated and shook the Earth for nine days.
  • The confined space within the fjord prevented the energy of the wave from dissipating. The event's impact was amplified by the fjord's structure.

Connection to Climate Change

  • The landslide was a consequence of rising temperatures in Greenland, leading to glacier melt at the mountain base.
  • The thinning glacier destabilized the mountainside, causing the collapse.
  • Scientists believe this event may represent the initial global impact of climate-driven processes on the Earth's crust.

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Description

Explore the mysterious global seismic event of September 2023, where a prolonged seismic wave puzzled scientists for nine days. This quiz delves into the origin of the seismic rumble, its connection to a massive landslide in East Greenland, and the role of the fjord's geometry in amplifying the tsunami's effects.

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