What is the origin of coal and where can coal veins be found?

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The term "coal vein" refers to a specific geological formation where coal is found, typically within sedimentary rock layers. Coal veins are formed through the accumulation of organic material, primarily from plant matter, which undergoes transformation over millions of years under heat and pressure. There are two main theories regarding the origin of coal: the allochthonous theory, which suggests coal is formed from materials transported by water, and the autochthonous theory, which posits that coal originates from local vegetation in situ. The latter theory has gained more support among European geologists. The organization and structure of coal have historically been under-researched, leading to ongoing debates about its formation. For detailed information on coal veins, particularly in Pennsylvania, resources are available through state geological databases.
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What is the "Coal Vein"?

I've just heard this term, and am almost completely ignorant as to its meaning. What is the defintion of the "coal vein"? Where is it found?

Any information (or a link) about the "coal vein" is appreciated.
 
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I've heard the term "vein" relating to minerals before. I believe it is due to fissures forming in old hard rock, and mineral rich sedimentation filling the cracks. I have no backing for this, it is just the way I always imagined it.

Njorl
 
Here is a database of Pennsylvania Coal Veins:

http://www.dep.state.pa.us/dms_apps/anthracite3.asp

There also seems to be a town in North Dakota, Burning Coal Vein.

Njorl
 
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Any more information?
 
http://www.geocities.com/aleph135/morwell18.html
For over a century and a half a controversy has raged in regard to that all important mineral, coal. On the one hand it has been maintained that its raw materials are the result of transport by water and that consequently coal is essentially of the nature of an aqueous organic sediment. On the other hand, the opinion has been held that coal is in the main the result of vegetable accumulations similar to those in actual circum-polar peat bogs consisting of the subaerial deposits, representing the successive generations of fallen peat plants. The first view of the origin of coal is usually called the allochthonous or transport theory. The second is known as the autochthonous or in-situ hypothesis. European geologists have in the main in recent years held to the latter view and their American colleagues have for the most part followed them in this opinion. It is important to emphasize however that the earlier and even the current views in regard to the origin of coal are for the most part arrived at in complete ignorance of its organization. Except in very recent years figures revealing the organization of coal are conspicuously absent in geological works, even in those which particularly deal with coal. It is apparently not without significance that the French who above all others gave early attention to the actual organization of coal, are supporters of the transport or aquatic hypothesis of the origin of coal. Although new methods and improved old methods now give us real insight into the organization of coal, there is yet unfortunately in general little observable rational improvement in geological theories regarding the formation of coal deposits.

You can find the location of coal veins here: http://www.dep.state.pa.us/dms_apps/anthracite3.asp?vein=Zero
 
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