How are a sof frink in a magma alike ???
341557
If you meant,  "How are a soft drink and magma  alike?" it goes like this.  In magma there are a lot of compressed gasses of  various  kinds, including carbon dioxide, the compressed gas in soft drinks.  When the magma is very deep in the earth, the gasses are powerfully compressed and the bubbles remain very small. But  as the magma rises to the surface of the earth, the pressure decreases and the  bubbles become larger.  This is something  like popping the top on a can of warm soda after shaking it up real hard.  The soda kind of explodes from the expanding carbon dioxide bubbles getting very large, very fast.  The same  thing happens with the compressed gasses in erupting magma.  They  help cause the magma to explode up into the air.  Other compressed gasses in magma include hydrogen sulfide and sulfer dioxide.
82209
Basically one of three ways. These are extrusion, intrusion, and accretion. \n\nExtrusion is the process of volcanism. Volcanoes erupt molten rock that may have originated as subducted oceanic crust or deeper rock. This magma adds huge volumes of rock to the crust as it erupts and cools into solid rock. \n\nIntrusion is a similar process, but no eruption takes place. Large bodies of molten rock float upward over long time periods through the crust. When these cool and harden they are called plutons or batholiths (depending on size-batholiths are larger). These form large parts of the crust.\n\nAccretion is the other method. In some instances plate tectonics can force oceanic plates up and over continental plates. These often form what are called ophiolites where we can examine oceanic crust on dry land. Large parts of continents or islands are often forced against continental plates. This can force sediments and oceanic crust upward creating what are called 'accretionary terrane'. Much of California is an accretionary terrane, built of islands in a fore arc subduction zone that were forced up against a paleocoastline that once was near the eastern border of present day California. \n\nHere two other explanations similar to my own that illustrate these processes:\nhttp://www.physicalgeography.net/fundamentals/10j.html\nhttp://earth.leeds.ac.uk/assyntgeology/extra_info/ehistory.htm
793858
WATER: water in touch with hot rock (or magma) changes into steam... the kind of eruption is named a phreatomagmatic eruption.\n\nSILICA: at greater percent of silica in magma, stronger eruption the volvano makes....
99133
Well, the way I always did it was to build your model volcano out of usually brown playdoh.  One of the better methods is to take a discarded paper towel cardboard center and glue it to some sort of paper (best more cardboard) then build your volcano around it making sure to keep the hole in th center open.  Pour baking soda into it...take it to school and at the precise moment pour vinegar into the baking soda...I think some people put food coloring into it (bright orange)
210093
Deep within the Earth it is so hot that some rocks slowly melt and become a thick flowing substance called magma. Because it is lighter than the solid rock around it, magma rises and collects in magma chambers. Eventually some of the magma pushes through vents and fissures in the Earth's surface. A volcanic eruption occurs! Magma that has erupted is called lava. \n\nalso\n\nWhen rock inside the Earth becomes hot enough it melts.\nThis molten rock, or magma, is less dense than the surrounding\nsolid rock.  Just as an object that is less dense than\nwater will float on water, the relatively low density of\nthe magma causes it to rise to the surface of the Earth.\n \nIf the magma contains water and dissolved gasses, when\nthe magma reaches the surface the water and dissolved\ngasses will suddenly expand into steam and gas, causing\na violent eruption.  This is like shaking a coke\ncan and then popping the tab.
280076
Difluoro arsenate, AsF2O2-, should have the same general structure as H2AsO4-, with two OH- groups replaced with F-.  This will be closest to tetrahedral, but distorted toward a smaller F-As-F angle because of the resonant double bond with the oxides.
839939
The shape - the sheild shape, gentle slopes, and runny (low viscosity) basalt
205880
igneous... hmm fudge? sedimentary, sugar cookies? metamorphic chocolate chip. neat question but I think candy is more like igneous, fudge more like sedimentary, and metamorhic... crush up several types and rebake them as granite!
523806
viscous felsic or high silica magmas
448232
Depends on the composition of the magma.\n\nMagma high in silica tends to be thick & gas bubbles are trapped. The gas builds up & boom! Explosion.\n\nBasaltic lava tends to be "soupy" so that the gas bubbles escape. No explosions here.\n\n:)
787241
Bowen's reaction series is what you're looking for.\n\nIn a nutshell, the rate of cooling, temperature, and magma composition determine which minerals form and the ultimate rock type.  The links provide more information.
708867
crust - is made of solid\nmantel - something like silly puddy consistency\nouter core - liquid\ninner core - solid
740828
There are two\nINTRUSIVE\nthe magma cooled of slowly, leaving gross crystals (granit)\nEXTRUSIVE\nthe magma cooled off fast, leaving crystal so small you can't see them (basalt)
883204
http://math.arizona.edu/~lega/UG/Colonies/Colonies.htm\n\nhttp://www.magma.ca/~scimat/B_subtil.htm\n\nhttp://www.pnas.org/cgi/content/full/0600829103/DC1
910296
We don't know they are all different for sure, but the statistical likelyhood of any two being the same are very small.\n\nIce crystals form in several ways, and the structure is extremely sensitive to humidity and temperature, which is slightly different in different parts of the cloud. Then snowflakes can hit each other and fragment, or stick together. So, you see, so much happens that it would be rare to see two that look exactly the same.
635078
fluffy? thats a nice term!  \nThey look fluffy becuase they are just water molecules in almost a gas form.  They float around near each other in this form, constantly changing shape.\n\nbut fluffy is good!
1178623
solid's particles are compact, while on liquids they are loose but gas' are the most loose (more distances with each other)