No, and geologically there is no reason to expect one to appear. There is evidence, however, of multiple ash falls from ancient volcanoes preserved in rocks of Cambrian, Ordovician, and Devonian age in outcrops in eastern West Virginia and in the subsurface in the western part of the State, and in a flint clay in the Hernshaw coal bed of Middle Pennsylvanian age (Kanawha Formation) in southern West Virginia.

The turn off to the Mud Volcanoes is 38 km (check on GPS and include GPS map) short of Hingol River and is marked by a small blue sign (about 1 foot wide) saying “Sapt Post”. The color on the sign board will vary, but the road will take you straight to the coast guard camp at Sapt. Turn off the road at this sign towards the sea and follow the tracks. Here, a saying goes, “all tracks lead to Chandra Gupt.

Volcanoes are a natural way that the Earth and other planets have of cooling off. Planets are warm in their mantles. Heat inside planets escapes towards their surfaces. For reasons that are not well understood, heat sometimes melts rocks, which then rise buoyantly toward the planet's surface. When the hot rocks - called magma - and included gases break through the crust, an eruption occurs. The buildup of ash and lava flows around the eruption hole (or vent) makes a volcano.

Volcanoes erupt because of density and pressure. The lower density of the magma relative to the surrounding rocks causes it to rise (like air bubbles in syrup). It will rise to the surface or to a depth that is determined by the density of the magma and the weight of the rocks above it. As the magma rises, bubbles start to form from the gas dissolved in the magma. The gas bubbles exert tremendous pressure.

The absolute number of volcanoes that exists depends on your definition: active only, active, dormant plus extinct volcanoes? And even if we decide on a definition, nobody has really counted all of the volcanoes, especially the tens on thousands on the sea floor. The best guess is 1511 volcanoes have erupted in the last 10,000 years and should be considered active.

High blood sugar levels can develop slowly, gradually climbing a little each month, especially if you are gaining weight. They may also develop quickly by eating a meal or snack high in carbohydrates, not exercising, forgetting your medicine or becoming ill. There are often observable symptoms when blood sugar is too high. Thirst and hunger often increase, you may become sleepy or tired and urinate more frequently. Infections are more common, wounds don't heal and your vision may become blurred.

Alaska contains over 100 volcanoes and volcanic fields which have been active within the last one and a half million years. There are more then 70 potentially active volcanoes in Alaska. In the 1980's one morning of April 1st Sitka, Alaskans woke up to black smoke billowing out of the dormant volcano, Mt. Edgecombe; people were in a panic. The biggest joke had just been played on a whole town.

Call the USGS Cascades Volcano Observatory in Vancouver, Washington, at (360) 696-7693; the URL is http://vulcan.wr.usgs.gov.

Most of the Earth's volcanoes are located around the Pacific Ocean because that is where most of the Earth's subduction zones. A subduction zone is a place where one plate of oceanic lithosphere (= the crust + uppermost mantle) is shoved under another plate. The down going plate eventually starts to melt, and the material rises up to erupt through the overlying plate. If the overlying plate is a continent, you get a chain of volcanoes such as the Andes or Cascades.

Shield volcanoes--the largest of all volcanoes on Earth (not counting flood basalt flows). The Hawaiian volcanoes are the most famous examples. These volcanoes are mostly made up of basalt, a type of lava that is very fluid when erupted. For this reason these volcanoes are not steep (you can't pile up a fluid that easily runs downhill).

Kilauea, Hawaii; Mount St.

There's an old Hawaiian expression for an angry wife which translates something like this: "Pele is pouring lava on Puna again..." Well, Puna does take the brunt of her wrath, but there are other places that could be affected sometime in the future. Here's a lava flow hazard map: http://pubs.usgs.gov/gip/hazards/maps.html

Maui does not have any active volcanoes like the Big Island of Hawaii. Mount Haleakala on Maui is a dormant volcano that has not erupted since the 1790’s.

Yes, the moon has some volcanoes. But as far as I know they are all "dead" volcanoes that have not erupted for millions of years. Most of the craters on the moon are from the surface being hit by asteroids and comets billions of years ago. The moon is a very "quiet" place. There is no air or water to erode the surface, and there are no earthquakes or volcanoes to change the surface. Only the smallest rocks may still hit the surface.

Ans: No, there are different earth processes responsible for volcanoes. Earthquakes may occur in an area before, during, and after a volcanic eruption, but they are the result of the active forces connected with the eruption, and not the cause of volcanic activity.

Cholesterol is a type of fat called a lipid. The body uses it for many things, such as making new cells. Your liver makes the cholesterol that your body needs. You also get cholesterol from the foods you eat. Your body needs some cholesterol. But if you have too much, it starts to build up in your arteries. (Arteries are the blood vessels that carry blood away from the heart.) This is called hardening of the arteries, or atherosclerosis.

The back pad should span the lumbar spine with the back cushion approximately centered on the belt line. Experiment until you find the most comfortable position for you.

Mars shows abundant signs of past volcanic activity spanning a wide range of geologic ages and volcanic rocks cover most of the surface. The most obvious features are the large volcanoes in the Tharsis province, such as Olympus Mons, and the extensive plains formed from volcanic flows. Volcanoes are also important to climate science: in the past they would have injected large quantities of gases into the Martian atmosphere, e.g.