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Editing 40d:Ice
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== Melting outdoor ice == | == Melting outdoor ice == | ||
− | It can be very important to be able to extract water from permanently-frozen ice (for instance on cold northern maps) in order to give water to the wounded. This can be done with [[magma]]. Dig out a tunnel one z-level below the ice sheet and fill it with magma. The ice on the above z-level will melt. You can see this happening here: http://mkv25.net/dfma/movie-153-meltingwateronglacier. Stationary magma below surface water does not | + | It can be very important to be able to extract water from permanently-frozen ice (for instance on cold northern maps) in order to give water to the wounded. This can be done with [[magma]]. Dig out a tunnel one z-level below the ice sheet and fill it with magma. The ice on the above z-level will melt. You can see this happening here: http://mkv25.net/dfma/movie-153-meltingwateronglacier. Stationary magma below surface water does not effect the freezing of the water. However any change in the amount of magma in the tile below the ice will melt the ice (which will soon freeze again), so flowing magma will keep surface water mostly usable in biomes with a cold winter. |
− | If you would like to transport magma to heat a frozen [[brook]] or other such feature that is very far away from the magma pipe, try to use a magma duct that is nearly as wide as the area you intend to fill. Otherwise, magma will tend to evaporate as it disperses from a narrow duct to a wider area. | + | If you would like to transport magma to heat a frozen [[brook]] or other such feature that is very far away from the magma pipe, try to use a magma duct that is nearly as wide as the area you intend to fill. Otherwise, magma will tend to evaporate as it disperses from a narrow duct to a wider area. |
=="Melting" ice without magma == | =="Melting" ice without magma == |