
n.
The lower layer of the earth's outer crust that underlies the sial and is rich in silica, iron, and magnesium.
[SI(LICA) + MA(GNESIUM).]
| Dictionary: si·ma |

[SI(LICA) + MA(GNESIUM).]
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| Chemistry Dictionary: sima |
The rocks that form the earth's oceanic crust and underlie the upper crust. These are basaltic rock types rich in silica (SiO2) and magnesium (Mg), hence the name. The sima is denser and more plastic than the sial that forms the continental crust.
| Geography Dictionary: sima |
The lower part of the continental crust and the oceanic crust, dominated by silica and magnesium.
| Buddhism Dictionary: sīmā |
(Pāli, boundary, limit). The boundary formally drawn around monastic territory.
| Wikipedia: Sima (mead) |
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Sima is a sweet mead, still an essential seasonal, sparkling brew connected with the Finnish Vappu festival. It is usually spiced by adding both the flesh and rind of a lemon. During secondary fermentation raisins are added to control the amount of sugars and to act as an indicator of readiness for consumption — they will swell by absorbing carbon dioxide and rise to the top of the bottle when the drink is ready. Sima is usually accompanied by munkki (a donut), tippaleipä (a special Vappu funnel cake) or rosetti (a rosette).
Ingredients for sima include Lemon, sugar, active dry yeast, and raisins. The concoction of water and the lemon and sugars are mixed, boiled , and cooled to room temperature (25'C or 75'F). The yeast is added and the mixture left to stand overnight. The sima will be ready to drink when the raisins rise to the top of the bottles, about 3-7 days depending on the temperature of the room where they are stored. It is usually served chilled.
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![]() | Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2009. Published by Houghton Mifflin Company. All rights reserved. Read more | |
![]() | Chemistry Dictionary. A Dictionary of Chemistry. Sixth Edition. Copyright © Market House Books Ltd, 2008. All rights reserved. Read more | |
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