Virtual Museum ID: 19-OM11
Coal is a kind of sedimentary rock made almost entirely of carbon, formed as decaying plants are buried and gradually transformed to rock over time. Variable amounts of other elements, hydrogen, oxygen, nitrogen and sulphur, are also present in coal. At first, the decaying organic matter forms peat, then lignite and eventually, after millions of years, coal. If heating and compaction continue, or the coal is subjected to high temperatures and pressures, anthracite will ultimately form. Coal is usually found as long thin beds, called seams, which are either mined underground or in large open pits.
The information listed below relates to the current holding location or collection that the sample is from, and whether the item is viewable at that location or is part of a private collection. Coordinates are given as guides, and we remind you that collecting specimens from these locations is not allowed. Caution is advised visiting such sites and Below BC assumes no responsibility for any injuries or trespassing charges that may occur as a result of the viewer entering these sites.
Original Collection:Oliver & District Heritage Society Museum (OM)
Virtual Museum ID:19-OM11
Date Added to VM:2019-06-06
Primary Mineral Formula:C
Advanced Geological Information
The following section provides geological data relating to the specimen or the site it was collected from, when available. Information has been obtained from various sources including private and government datasets but may not be up to date. Any geological time periods or ages listed often relate to the primary geology of the area, and may not be the actual date of an event such as mineral formation.