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Showing posts with the label geohazard

Spectacular volcano videos: Identifying eruption processes

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- Dr. Janine Krippner We are fortunate that there is a large availability of volcanic eruption videos online for all of us to enjoy (see below warning), and we can learn a lot from them too. When I am looking at my satellite images of dome collapse block and ash flow and column collapse pyroclastic flow deposits on Shiveluch and Mount St. Helens volcanoes I have videos of these processes running through my mind. This is a short guide to what you are seeing in these incredible videos. WARNING: There are very dangerous and life threatening hazards associated with retrieving this footage, and here at In the Company of Volcanoes we strongly discourage anyone from trying to take your own. It is never, ever worth risking your life. --- This video shows the dome at Unzen volcano undergoing a partial collapse in 1991. This shows how a near-solid body of rock rapidly fragments down to smaller pieces of rock and ash, creating a billowing ash plume rising from the block and ash...

Volcanology Teaching Resources

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- Dr. Janine Krippner I am excited about an upcoming set of Google Hangout sessions with 6th graders talking all about volcanoes, why they erupt, why some erupt more violently than others, what their hazards are, and what we, as volcanologists, are doing to try and help people that live near them. So I sent out a request to the world of Twitter and volcanologists (links to their twitter feeds included, also full of information and resources - many more twitter volcanologists can be found) from around the world got back to me with great ideas and resources, and here they are! This is an open blog, I will add more resources as they come to my attention, so if there is something missing please contact me and I will add it for everyone to enjoy. Volcanologist @kenhrubin has put together a list of Twitter volcanologists, volcano watchers, and volcano-related organizations so you can keep an eye on the latest activity and volcano news. You can watch the list Here . This looks like a...

How fast is volcano-fast?

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- Janine and Alison This morning I (Janine) was researching the May 18, 1980 Mount Saint Helens eruption to begin the next phase of my research. Reading through the descriptions of the start of the eruption - when massive blocks of the volcano slid to the north, I enthusiastically jumped out of my chair surprising my office mates. Marking out 1 meter with my feet I looked up at them and told them "this is one meter, now imagine 50 of these. Now imagine a massive chunk of rock moving 50 of these in one second! 50 m per second! This is nuts!" The joys of sharing an office with an over-enthusiastic volcanologist... 50 m/s is how fast the side of the mountain began to travel down and away from the volcano, taking chunks of rock the size of 30 story buildings northward. As the slide evolved into a debris avalanche, the sediment mass began flowing, the blocks reached speeds of up to 80 m/s [1]. So this got us talking about the insane speeds involved in volc...

In the Company of Volcanoes at AGU

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-Alison and Janine The largest geoscience conference happens every year in San Francisco. The American Geophysical Union (AGU)  meeting draws more than 20,000 participants from around the world every December. We gather to share our new results, catch up with friends and colleagues, and drink beer. Janine and Alison will both be attending this year. Although we have been to conferences in three other countries together, this will be Janine's first AGU and the first conference in the US where we both be in attendance. Both of us have posters to present on our research, and then will spend the rest of the visit stuffing our brains full of new information and names of new colleagues. If you are going to AGU we'd love you to stop by and chat! Janine and Alison in Japan for the IAVCEI conference in 2013. So what sort of topics get covered in a 20,000 person conference? Way more than we could fit in a blog post, but you can get the idea just from our examples....