Volcano's Deadly Warning. Volcanoes Online. National Geographic: Eye in the Sky. Volcanoes are awesome manifestations of the fiery power contained deep within the Earth.
These formations are essentially vents on the Earth's surface where molten rock, debris, and gases from the planet's interior are emitted. When thick magma and large amounts of gas build up under the surface, eruptions can be explosive, expelling lava, rocks and ash into the air. Less gas and more viscous magma usually mean a less dramatic eruption, often causing streams of lava to ooze from the vent. The mountain-like mounds that we associate with volcanoes are what remain after the material spewed during eruptions has collected and hardened around the vent. This can happen over a period of weeks or many millions of years. A large eruption can be extremely dangerous for people living near a volcano. Volcanoes tend to exist along the edges between tectonic plates, massive rock slabs that make up Earth's surface. Volcanoes - Introduction.
Volcano Live, John Seach. Volcano Hazards Program. Volcano Field Trip. Terrestrial Volcanoes. Terrestrial Volcanoes By turns hot embers from her entrails fly, And flakes of mountain flame that arch the sky.
-Virgil's Aeneid. SAVAGE EARTH Online. Please note: SAVAGE EARTH ONLINE looks best when viewed using Netscape 3.0 or above, or Internet Explorer 3.0 or above, on Macintosh, Windows 95 or Windows 3.1.
If you have an earlier version, or another browser, all pages may not be presented exactly as designed. To view the animations in SAVAGE EARTH ONLINE, you will need the free Flash plug-in. Premiere: July 19, 1998, at 8 pm (ET) on PBS. (Watch for repeat showings on your local PBS station.) A Study of Plate Tectonics. Mount St Helens. Feature. Mount St. Helens - May 18, 1980. Seismogram from station CPW, 112 km (70 mi) northwest of Mount St.
Helens, May 18, 1980. Mount St. Helens National Volcanic Monument. Fireweed, growing in Mount St.
Helens' devastated area; view from the north. Summer 1984. The Mount St. Helens National Volcanic Monument is within the Gifford Pinchot National Forest and managed by the USDA Forest Service. The Monument was established in 1982 to designate 445 km2 (110,000 acres) around Mount St Helens for research, recreation, and education. Mauna Loa, Decade Volcano. How Volcanoes Work. Global Volcanism Program: Worldwide Ho. Mount Saint Helens. Cascades Volcano Observatory (CVO) Researchers use geophysics to locate aquifers at Mount St.
Helens.July 06, 2016 Every year, Mount St. Helens gets an average of 162 inches of rain and about 40 feet of snow. So where does all the water go? Some of it enters rivers and streams that originate on the volcano and some of it enters the groundwater system. Using a geophysical method called Controlled-Source Audio-Magnetotellurics, researchers located two aquifers at Mount St.
Knowing more about groundwater at Mount St. Read more at Where is the Hot Rock, and Where is the Groundwater—Using CSAMT to Map Beneath and Around Mount St. Recent Mount Hood earthquake swarm typical for this Oregon volcano.May 16, 2016 At Mount Hood, a swarm of small earthquakes was detected May 15-16, 2016. The earthquakes in this swarm are located 2-3 miles south of the summit of Mount Hood at depths of 2-3 miles below sea level. Volcano's Deadly Warning. By Lexi Krock Posted 11.12.02 NOVA What's the difference between lava and magma?
What are volcanic vents, dikes, and fissures? In this anatomy of a volcano, explore the basic geological features of a volcano such as Mt. St. Helens as well as the deadly materials released during volcanic eruptions. To learn more about the various numbered parts of this volcano diagram, read on. There are many different kinds of volcanoes, ranging from the Hawaiian type, which produces gentle, effusive eruptions that tourists can observe from mere steps away, to the andesitic variety, which can produce violent, life-threatening eruptions with little warning. The 3 basic rock types. Ask GeoMan...
What are the 3 basic types of rocks? Just as any person can be put into one of two main categories of human being, all rocks can be put into one of three fundamentally different types of rocks. They are as follows: Igneous Rocks Igneous rocks are crystalline solids which form directly from the cooling of magma. This is an exothermic process (it loses heat) and involves a phase change from the liquid to the solid state. Sedimentary Rocks In most places on the surface, the igneous rocks which make up the majority of the crust are covered by a thin veneer of loose sediment, and the rock which is made as layers of this debris get compacted and cemented together. Clastic: your basic sedimentary rock. Click here for more on sedimentary processes and rocks (RCC). Metamorphic Rocks The metamorphics get their name from "meta" (change) and "morph" (form). Click here to ask GeoMan a question Return to Ask GeoMan's Index of Questions Return to GeoMan's Home Page.