The video I found is of Mount Tavurvur erupting in 2014. The eruption captured in this video is an explosive one. The lava is not just flowing out, there is some pressure built up which leads to the explosion. The video also captures the sound burst which I thought was very cool.
Mount Tavurvur is an active volcano in Papua New Guinea and is considered to be quite dangerous. It is a cinder cone. I think it is fairly new, but I am unsure and couldn't find the age of it. Cinder cones are built from ejected lava fragments that begin to harden in flight. It is relatively small at a height of 223 meters, with steep sides and a characteristic crater. (Map from http://www.dailymail.co.uk/sciencetech/article-2747577/Holy-smokes-Watch-explosive-moment-volcano-erupts-triggers-SONIC-BOOM-sending-shockwaves-sky.html)
from https://www.washingtonpost.com/news/capital-weather-gang/wp/2014/09/03/ nasa-satellite-captures-incredible-extent-of-tavurvur-volcano-ashfall/
Tavurvur is a sub-vent of the Rabaul caldera and is the most active volcano in that caldera. The caldera Rabaul violently exploded in 1994 and destroyed the island's largest city and since then Mount Tavurvur is showing the most activity in that caldera.This graphic is from NASA and shows the ashfall from the most recent eruption of Tavurvur, pictured to the left. While we don't have anything quite that exciting happening locally, we do have two volcanic tuff cones nearby, the Menan Buttes, pictured below. These were formed about 10,000 years ago when magma ran into an aquifer and the hot magma was explosively fragmented. Overall, volcanos are awesome! No matter if the explosion is effusive or explosive, it is definitely a powerful thing to see, even if it's just through video.
from http://trailrunner.com/event/spitfire-ultra-trail-challenge-at-menan-butte/
From the places we go, to the food we eat, to the cars we drive and the products we use, geology surrounds us. It's easy to forget how much we depend on the geological processes of the Earth. Idaho in particular is a geological hotspot (figuratively speaking). Not too far from Rexburg, we have the Menan Buttes, two of the largest volcanic tuff cones. This an amazing piece of geologic history that we are welcomed to explore and observe exposed igneous rock, such as obsedian. We are also close to Yellowstone, City of Rocks, the Tetons, and many other cool places to explore geology. We are even fairly close to the Rockies where the continental crust can be up to 70 kilometers (45 miles) thick! (Image from hike at Menan Butte) Along with that Rexburg is a large farming community. In order to have a successful crops, farmers have to analyze the soil content, determine what minerals go in their fertilizer. The minerals in the soil will depend on what kind of rock it originat...
"Odd New Theory Explains How Early Earth Got Its Oxygen" Cyanobacteria diagram from https://en.wikipedia.org/wiki/Cyanobacteri a Oxygen production on Earth is theorized to have started about 2.5 billion years ago by oceanic cyanobacteria. These cyanobacteria produced oxygen as a product of photosynthesis. At around 2.3 billion years ago, an environmental change occurred, called the Great Oxygenation Event (GOE). At this point, the oxygen sinks on Earth became saturated, so oxygen produced by these cyanobacteria was free to go into the atmosphere. But what happened during that in between period? There are many theories that explain what happened in that time lag in between the beginning of oxygen production and the GOE. A more recent one is addressed in the news article I found. Convergent Boundary from https://geomaps.wr.usgs.gov/parks/pltec/converge.html According to a news article on Live Science, a new study by Megan Duncan and Rajdeep Dasgupta at Rice...
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