Krakatoa

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Krakatoa is located in the Sunda Strait in Indonesia, while Java is an island in Indonesia. The closest point of Java to Krakatoa is approximately 50 kilometers (31 miles).

Krakatoa is located in Indonesia, specifically in the Sunda Strait between the islands of Java and Sumatra. It is approximately 160 kilometers (100 miles) west of Jakarta, the capital city of Indonesia.

Volcanic ash can clog the throat and damage the eyes and lungs. The weight of it can bring town trees and roofs. When mixed with water it can form deadly mudflows called lahars. It shorts out electrical circuits and can clog and damage the engines of cars and planes, potentially causing planes to crash.

Krakatoa is not a mainland volcano; it is actually a volcanic island located in Indonesia. The island is part of the Krakatoa volcanic group and is situated in the Sunda Strait between Java and Sumatra.

The eruption of Krakatoa in 1883 caused widespread destruction, resulting in massive loss of life and property. The exact cost of the damage is difficult to quantify, but it had a significant impact on the region and beyond in terms of economic losses and environmental consequences.

Yes. Activity continued after the 1883 eruption causing a new island, Anak Krakatau, to emerge in 1927 which continues to grow to this day.

An erupting volcano may not always be visible due to factors such as weather conditions like clouds or fog, the time of day (nighttime), or the location of the volcano (hidden by terrain). Additionally, some eruptions may be small or occur underwater, making them harder to detect visually.

The eruption of Mount Krakatoa produced lava flows, pyroclastic flows, ash clouds, and tsunamis. These events led to widespread destruction of the surrounding area and resulted in the deaths of thousands of people.

Generally, yes. When a volcano is dormant the temperatures are generally no different from what you would find on a non-volcanic mountain. One exception would be the occasional hot spring or fumarole venting hot gas.

Mount Krakatoa is located in Indonesia, between the islands of Java and Sumatra. It is part of the Krakatoa volcanic group, which includes several other volcanic cones. The most famous eruption of Krakatoa occurred in 1883, causing massive destruction and tsunamis in the region.

The eruption of Krakatoa in 1883 primarily affected the islands of Java and Sumatra in Indonesia. The volcanic eruption caused widespread devastation and resulted in the deaths of over 36,000 people. Ash from the eruption also spread to countries as far as Australia and the United States.

Krakatoa's magma viscosity was estimated to be relatively low, indicating it was more fluid-like. This low viscosity contributed to the violent explosive eruption in 1883, producing devastating volcanic events such as pyroclastic flows and tsunamis.

The eruption of Krakatoa in 1883 was so explosive due to the accumulation of high-pressure magma beneath the volcano, which eventually led to a catastrophic release of energy. The eruption was triggered by the collapse of the volcano's magma chamber, resulting in a series of powerful explosions that generated massive tsunamis and global climatic effects.

The loudest sound of a volcanic eruption was heard during the 1883 eruption of Krakatoa in Indonesia. The sound was heard over 3,000 miles away and is considered one of the loudest sounds in recorded history.

According to records compiled from different sources there was not a 535 AD eruption of Krakatau, however there was a major eruption around 416 AD that completely destroyed the volcano and created a large undersea caldera. refer to Smithsonian Institute of Global Volcanism for further details

The 1883 eruption of Krakatoa, a volcano in Indonesia, killed tens of thousands of people and blasted ash into the stratosphere. This had the effect of cooling the planet by about 3 degrees in the year following the explosion.

It is difficult to predict with certainty, but Krakatoa volcano is still active and has been known to produce significant eruptions in the past. It is monitored closely by scientists to assess any potential risks to surrounding areas. It is important to stay informed about updates from authorities regarding the volcano's activity.

There is currently no evidence to suggest that Krakatoa is reforming. The volcanic island last erupted in 1883, causing one of the most powerful eruptions in recorded history. While volcanic activity can never be entirely ruled out, there is no indication at present that Krakatoa is undergoing any significant reformation.

The Krakatoa eruption in 1883 affected an area of about 1.6 million square miles, with the volcanic ash spreading across the globe. The explosion was one of the most powerful in recorded history and had devastating impacts on the surrounding regions.

Began May 1883 until 27th. August 1883

The Krakatoa haze refers to the atmospheric effects caused by the eruption of Krakatoa in 1883. The explosion injected large amounts of ash and sulfur dioxide into the atmosphere, leading to colorful sunsets, cooler temperatures, and vivid twilights around the world in the following months.

It took several decades for the people of Krakatoa to fully recover from the devastation caused by the 1883 eruption and tsunami. The eruption resulted in the loss of thousands of lives and widespread destruction of property, leading to long-term economic and social impacts on the local population. The recovery process was slow and challenging, requiring significant rebuilding of infrastructure and communities.

There was no specific warning issued before the Krakatoa eruption in 1883. The event happened suddenly and caught people by surprise, resulting in a devastating disaster.

Both Stromboli and Krakatoa are volcanic islands formed by stratovolcanoes. Stromboli is in the Mediterranean Sea off the coast of southern Italy. It has erupted almost continuously for nearly 2,000 years. Krakatoa is in the Sunda Strait between the islands of Java and Sumatra in Indonesia. The island famously destroyed itself in a massive eruption in 1883. A new island, Anak Krakatau emerged in its place in 1927.