10 of the Most Interesting Volcanoes in the World

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Planet Earth Planet EarthNova Share Program Description Follow a team of volcano sleuths as they embark on a worldwide hunt for an elusive volcanic mega-eruption that plunged medieval Earth into a deep freeze. The mystery begins when archaeologists find a hastily dug mass grave of 4, men, women, and children in London. So what killed off these families? The chronicles of that time describe a run of wild weather that devastated crops and spread famine across Europe. Across the globe, it turned summer into winter. What would happen if another such cataclysm struck again today? Our planet is capable of unleashing extreme chaos. Volcanoes, earthquakes, hurricanes and floods can cause untold devastation.

Hawaii Volcanoes National Park

Blocks are angular fragments that were solid when ejected. Bombs have an aerodynamic shape indicating they were liquid when ejected. Bombs and lapilli that consist mostly of gas bubbles vesicles result in a low density highly vesicular rock fragment called pumice. Rock formed by accumulation and cementation of tephra called a pyroclastic rock or tuff.

Big, bad, Martian volcanoes unveiled Anne M Stark, [email protected], That’s the conclusion of a team of scientists, including Lawrence Livermore National Laboratory cosmochemist Bill Cassata, about the evolution of volcanoes on the red planet, compared to those on Earth.

This is because they have played an important role in how the lush landscape of this region has come into being. Due to the many eruptions over the past millennia, the soil in Costa Rica is rich in many minerals and is very fertile. For example, Volcan Irazu is known for its astonishing green blue lake that sits in one of its craters, while within a crater of the Poas Volcano there is a boiling acid lake.

Volcanic Ranges The volcanoes of Costa Rica can be divided into 3 volcanic range systems. The Talamanca Range has only one volcano, the El Viejo. This is because it was until recently the most active volcano in the country, spewing hot gases and steam on a regular basis. All of this stopped in December The most accessible active volcano in Costa Rica is the Poas Volcano , which sits in the national park of the same name.

This volcano has only one active crater, while the other two are dormant. While the active crater has a boiling acid lake, one of the inactive carters has a lovely icy cold water lake which flows down the side of the volcano to become the Rio Sarapiqui. Regular tours of this volcano can be arranged any time. Kennedy visited Costa Rica. As the soil on this volcano is very fertile, its slopes are lush and green with plenty of forestation and pastureland’s for grazing cattle.

The trails leading up to the summit are also stunning and are home to numerous exotic and beautiful birds like tapirs and tanagers.

Ice cores yield history of volcanic eruptions, climate effects

Blind Leading the Blind: Because radiometric dating utterly refutes their biblical interpretations, young-Earth creationists YECs are desperate to undermine the reliability of these dating methods. As part of their efforts, YECs clearly believe that they can discredit K-Ar dating if they can show that excess argon routinely enters rocks and minerals as they form. That is, they believe that excess argon will cause rocks and minerals that are supposedly less than 10, years old to have ‘deceptively’ old K-Ar dates of millions or billions of years.

In particular, YECs attempt to demonstrate that excess argon is a ‘problem’ for K-Ar dating by locating examples of historically erupted volcanics, which yield K-Ar dates that are hundreds of thousands or millions of years older than their eruption dates. The data were miscopied from Dalrymple

Oct 26,  · Over the past few days, news out of Iceland is that Öræfajökull, one of Iceland’s largest and most powerful volcanoes, is getting volcano is “accumulating magma” and an.

General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled. This then can be used to deduce the sequence of events and processes that took place or the history of that brief period of time as recorded in the rocks or soil.

For example, the presence of recycled bricks at an archaeological site indicates the sequence in which the structures were built. Similarly, in geology, if distinctive granitic pebbles can be found in the sediment beside a similar granitic body, it can be inferred that the granite, after cooling, had been uplifted and eroded and therefore was not injected into the adjacent rock sequence.

Although with clever detective work many complex time sequences or relative ages can be deduced, the ability to show that objects at two separated sites were formed at the same time requires additional information. A coin, vessel, or other common artifact could link two archaeological sites, but the possibility of recycling would have to be considered. It should be emphasized that linking sites together is essential if the nature of an ancient society is to be understood, as the information at a single location may be relatively insignificant by itself.

Similarly, in geologic studies, vast quantities of information from widely spaced outcrops have to be integrated. Some method of correlating rock units must be found. In the ideal case, the geologist will discover a single rock unit with a unique collection of easily observed attributes called a marker horizon that can be found at widely spaced localities. Any feature, including colour variations, textures, fossil content, mineralogy , or any unusual combinations of these can be used.

It is only by correlations that the conditions on different parts of Earth at any particular stage in its history can be deduced. In addition, because sediment deposition is not continuous and much rock material has been removed by erosion , the fossil record from many localities has to be integrated before a complete picture of the evolution of life on Earth can be assembled. Using this established record, geologists have been able to piece together events over the past million years, or about one-eighth of Earth history, during which time useful fossils have been abundant.

With 8 threatening volcanoes, USGS says California deserves close monitoring

It’s also become a fixture of pop culture—so much so that even people who haven’t read it know or think they know the story: An ambitious young scientist named Victor Frankenstein creates a grotesque but vaguely human creature from the spare parts of corpses, but he loses control of his creation, and chaos ensues. It’s a wildly inventive tale, one that flowed from an exceptional young woman’s imagination and, at the same time, reflected the anxieties over new ideas and new scientific knowledge that were about to transform the very fabric of life in the 19th century.

The woman we remember as Mary Shelley was born Mary Wollstonecraft Godwin, the daughter of political philosopher William Godwin and philosopher and feminist Mary Wollstonecraft who tragically died shortly after Mary’s birth. Hers was a hyper-literate household attuned to the latest scientific quests, and her parents Godwin soon remarried hosted many intellectual visitors.

Hawai’i Volcanoes Lodge Company operates Volcano House. and iconic location within Hawai’i Volcanoes National Park on Hawai’i Island. Drawing upon a storied history dating back to , Volcano House is now ready for a new era.

Scope[ edit ] Major volcanoes in Indonesia There is no single standard definition for a volcano. It can be defined from individual vents, volcanic edifices or volcanic fields. Interior of ancient volcanoes may have been eroded, creating a new subsurface magma chamber as a separate volcano. Many contemporary active volcanoes rise as young parasitic cones from flank vents or at a central crater. Some volcanic cones are grouped into one volcano name, for instance, the Tengger caldera complex , although individual vents are named by local people.

The status of a volcano, either active or dormant , cannot be defined precisely. An indication of a volcano is determined by either its historical records, radiocarbon dating , or geothermal activities. Complementary sources for the latest volcanic data are taken from the Volcanological Survey of Indonesia, a governmental institution which is responsible for volcanic activities and geological hazard mitigation in Indonesia, [8] and some academic resources. Sumatra[ edit ] Map showing the location of volcanoes and geological fault lines of Sumatra The geography of Sumatra is dominated by a mountain range called Bukit Barisan lit:

Makushin Volcano description and information

From Krakatau to Bali – Java Indonesia: It made the cover of Science in , but the story behind starts years ago, or on a personal scale, in late The present-day caldera of Santorini with the white Minoan deposit visible as the thick topmost layer in the cliffs. The Minoan pumice layer in the quarry near Fira. When the volcano on Santorini exploded around years ago, the eruption began with a heavy rain of hot pumice falling out from the eruption column that reached about 40 km height.

Planet Surfaces Chapter index in this window — — Chapter index in separate window This material (including images) is copyrighted!.See my copyright notice for fair use practices. Select the photographs to display the original source in another window.

They do it by comparing the ratio of an unstable isotope, carbon , to the normal, stable carbon All living things have about the same level of carbon , but when they die it begins to decay at uniform rate—the half-life is about 5, years, and you can use this knowledge to date objects back about 60, years. However, radiocarbon dating is hardly the only method that creative archaeologists and paleontologists have at their disposal for estimating ages and sorting out the past.

Some are plainly obvious, like the clockwork rings of many old trees. But there are plenty of strange and expected ways to learn about the past form the clues it left behind. Camel on Your Knife It’s wasn’t so long ago that megafauna ruled the American continent. Sloths and wooly mammoths pushed their weight around; horses and camels had their day. But after the end of the last Ice Age those animals disappeared, so when scientists turn up traces of those animals on archaeological remains, those remains go way back.

Killer Volcanoes

Without volcanoes, most of Earth’s water would still be trapped in the crust and mantle. Early volcanic eruptions led to the Earth’s second atmosphere, which led to Earth’s modern atmosphere. Besides water and air, volcanoes are responsible for land, another necessity for many life forms.

A comprehensive investigation of any volcano must also include the careful, systematic mapping of the nature, volume, and distribution of the products of prehistoric eruptions, as well as the determination of their ages by modern isotopic and other dating methods.

Each island is made up of at least one primary volcano, although many islands are composites of more than one. The Big Island, for instance, is constructed of 5 major volcanoes: Mauna Loa is the largest active volcano on Earth. Kilauea is presently one of the most productive volcanoes on Earth in terms of how much lava it erupts each year. The primary volcanoes on each of the islands are known as a shield volcanoes, which are gently sloping mountains produced from a large number of generally very fluid lava flows.

Hawaiian volcanoes primarily erupt a type of rock known as basalt. When molten, basalt produces liquids of relatively high fluidity, compared to volcanoes that erupt more silica rich magma types such as andesite, dacite or rhyolite. The fluidity of molten basalt favors the formation of lava flows, which is why the Hawaiian volcanoes generally have gentle sloping sides.

These other types of volcanoes common outside of Hawaii are typically steeper sided. The Hawaiian volcanoes were produced by the Hawaiian hot spot, which is presently under the Big Island of Hawaii. The image below shows the islands of the Hawaiian chain and the intervening shallows, banks and reefs along a line from southeast to northwest. Note that the islands of Lanai and Kahoolawe are not shown because they would “overlap” with Molokai and Maui, respectively see the map of the Islands on the Hawaiian Volcanoes page In general, when you move along the island chain from southeast Hawaii to northwest, Kure , the volcanoes become older and older.

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[NOVA SpaceNow 2015] Earth’s Volcanoes – NEW Science Documentary Full HD


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