recommendations for mud volcanoes?
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First mould a volcano with plastercine or play dough.\n\nThen fill it with bicarbonate of soda, baking powder or health salt.\n\nGet some vinegar and then mix it with reddish-orangey (Lava colour) ink or food colouring.\n\nThen pour your coloured mixture with the bicarbonate of soda, baking powder or health salt in the volcano.\n\nHey Presto! The bubbles should start to rise. \n\nWhen Bicarbonate of Soda is mixed with an acid liquid (Vinegar)it releases the gas carbon dioxide (CO2): \n\nNaHCO3     +     H+     ----->     Na+     +     H20     +     CO2\n(soda)         (acid)           (sodium)       (water)        (gas)\n\n^ Above is the word equasion. If you are good at science you might be able to understand this.\n\nI hope I helped you.
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http://pubs.usgs.gov/gip/volc/types.html\nThe website above takes you to USGS pub called: \nPrincipal Types of Volcanoes.\n\nIt will help you answer your  question.
125954
I would try out these sites and go from there.  I seemed to be able to find quite a bit of information just searching for "Goleta Beach erosion".  Good luck ad hooray for geology.
602845
Any slope that's safe from avalanche.
709259
http://www.volcanolive.com/volcanocams.html
562648
Try Mira Mesa, or Del Mar
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A volcano is a geological landform usually generated by the eruption through a planet's surface of magma, molten rock welling up from the planet's interior. Other forms of volcano include ice volcanoes (particularly on some moons of Jupiter, Saturn and Neptune) and mud volcanoes. On Earth, volcanoes tend to occur near the boundaries of crustal plates. Important exceptions exist in hotspot volcanoes, which occur at locations far from plate boundaries; hotspot volcanoes are also found elsewhere in the solar system, especially on its rocky planets and moons.\n \nSmoking Bromo and Semeru (background) volcanoes on Java in Indonesia.\n\nMud volcanoes are formations often not associated with known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those of igneous volcanoes, except when a mud volcano is actually a vent of an igneous volcano.\n\nThe name "volcano" is thought to derive from Vulcano, a volcanic island in the Aeolian Islands of Italy whose name in turn originates from Vulcan, the name of a god of fire in Roman mythology. The study of volcanoes is called volcanology (sometimes spelled vulcanology).\nContents [hide]\n1 Volcano classification \n1.1 Erupted material\n1.2 Shape \n1.2.1 Shield volcanoes\n1.2.2 Cinder cones\n1.2.3 Stratovolcanoes\n1.2.4 Supervolcanoes\n1.2.5 Submarine volcanoes\n1.3 Subglacial volcanoes\n1.4 Classifying volcanic activity\n2 Notable volcanoes \n2.1 Volcanoes on Earth\n2.2 Volcanoes elsewhere in the solar system\n3 Volcanology \n3.1 Volcano formation \n3.1.1 Tectonic environments of volcanoes \n3.1.1.1 Constructive plate margins\n3.1.1.2 Destructive plate margins\n3.1.1.3 Hotspots\n4 Predicting volcanic eruptions \n4.1 Seismicity\n4.2 Gas emissions\n4.3 Ground deformation\n4.4 Iceberg tremors\n4.5 Hydrology\n4.6 Remote Sensing \n4.6.1 Local Predictions\n4.6.2 Early Warning for Lahars\n4.7 Predicting future eruptions of Mt. Etna\n4.8 Monitoring of Sakurajima, Japan\n5 Effects of volcanoes\n6 Past beliefs\n7 See also \n7.1 Lists\n7.2 Types\n7.3 Specific locations\n7.4 Volcano-related phenomena\n7.5 General topics\n7.6 People\n8 References\n9 Further reading\n10 External links\n\n[edit]\n\nVolcano classification\n[edit]\n\nErupted material\n\nOne way of classifying volcanoes is by the type of material erupted (ejecta), since this affects the shape of the volcano. If the erupted magma contains a high percentage (>65%) of silica, the lava is called felsic. Felsic lavas tend to be highly viscous (not very fluid) and are erupted as domes or short, stubby flows. Viscous lavas tend to form stratovolcanoes or lava domes. Lassen Peak in California is an example of a volcano formed from felsic lava and is actually a large lava dome. This type of volcano has a tendency to explode when erupting, because the viscous lava traps volatiles (gases), which cannot escape easily. Mount Pelée on the island of Martinique is another example. Pyroclastic flows (ignimbrite) are highly hazardous products of such volcanoes, since they are composed of molten volcanic ash too heavy to go up into the atmosphere, so they hug the volcano's slopes and travel far from their vents during large eruptions. Temperatures as high as 1,200 °C are known to occur in pyroclastic flows, which will incinerate everything flammable in their path and thick layers of hot pyroclastic flow deposits can be laid down, often up to many meters thick. Alaska's Valley of Ten Thousand Smokes, formed by the eruption of Novarupta near Katmai in 1912, is an example of a thick pyroclastic flow or ignimbrite deposit.\n\nIf, on the other hand, the magma contains a relatively low percentage of silica, the lava is called mafic or basaltic and will be fluid as it erupts, capable of flowing for long distances. Mafic refers to the chemical composition of the lava—it contains higher percentages of magnesium (Mg) and iron (Fe), and correspondingly lower percentages of silica. Due to its low viscosity, v
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I like Rincon, Humacao and Caguas, I could give you more info depending on what you are looking for.
465753
http://www.volcano.si.edu/reports/usgs/index.cfm
890167
volcanoes and earthquakes (faults)
1177665
Hmmmmm ..... some volcano probably??   You probably know that - can't think of one that fits.
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Contact Trenggo Minerals out of Malaysia.  If I can decipher your e-mail correctly, you are looking for barite mud, which is used in the drilling for oil and gas. \n\nTrenggo can be reached at: :+609 681 1400 \n\nThe parent website is at: http://www.m3nergy.com
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Try this:\n\nhttp://rubberscape.org/_wsn/page3.html\n\nor even better:\n\nhttp://www.playsafesurfacing.com/Playground_Mulch/playground_mulch.html
205366
try the Idiot's Guide to Geology and Minig...
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Curiously, I could not find a comprehensive listing.  This site might be helpful, however, or at least give you a start.\n\nhttp://dir.yahoo.com/Science/Earth_Sciences/Geology_and_Geophysics/Volcanology/Volcanoes
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try www.wwfstinks.com theres some good stuff on there you might like!
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Morne Diablotins - Dominica\nThe mountain is volcanic, and erupted 30,000-40,000 years ago. There are no known historical eruptions.\n\nKick-'em-Jenny - Grenada\nAn active submarine volcano on the Caribbean sea floor 8 km north of the island of Grenada.  The volcano has erupted on at least twelve occasions since 1939 and 2001 (the last being on December 4, 2001)\n\nLa Grande Soufrière - Guadeloupe\nor simply La Soufrière (French: "sulphur outlet"), is an active stratovolcano located on the French island of Basse-Terre, in Guadeloupe.  Last eruption in 1977\n\nMartinique, Montserrat, Netherlands Antilles, Saint Kitts and Nevis, Saint Lucia, and Saint Vincent and the Grenadines also have some, just follow the link, click on the country name in the right hand box and that will take you to the names of volcanoes in each of those countries (some have links with even more info about the volcano)\n\nhope this helps