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Venezuela  are estimated at 250  billion  barrels, equivalent to the
           total reserves of Saudi Arabia.
                  Most  oil  shales  are  fine-grained  sedimentary  rocks
           containing relatively large amounts of organic matter from which
           significant  amounts  of  shale  oil  and  combustible  gas  can  be
           extracted  by  destructive  distillation.  One  of  the  largest  known
           locations is the oil shale locked in the 40.000 km2 (16000 sq-mile)
           Green River Formation in Colorado, Utah, and Wyoming.
                  Oil shale differs from coal whereby the organic matter in
           shales has a higher atomic Hydrogen to Carbon ratio. Coal also has
           an organic to inorganic matter ratio of more than 4,75 to 5 while as
           oil  shales  have  a  higher  content  of  sedimentary  rock.  Sources
           estimate the world reserves of Oil Shales at more than 2,5 trillion
           barrels.
                  Oil  shales  are  thought  to  form  when  algae  and  sediment
           deposit in lakes, lagoons and swamps where an anaerobic (oxygen
           free) environment prevent the breakdown of organic matter, thus
           allowing it to accumulate in thick layers. That is later covered with
           overlying rock to be baked under high temperature and pressure.
           However  heat  and  pressure  was  lower  than  in  oil  and  gas
           reservoirs.  The  shale  can  be  strip  mined  and  processed  with
           distillation. Extraction with fracturing and heating is still relatively
           unproven.  Companies  are  experimenting  with  direct  electrical
           heating rather than e.g. steam injection. Extraction cost is currently
           around 25-30 USD per barrel [9].

                  Coal, Coal Gasification and Liquefaction
                  Coal is similar in origin to oil shales but typically formed
           from  anaerobic  decay  of  peat  swamps  relatively  free  from
           nonorganic sediment deposits, reformed by heat and pressure. To
           form a 1 meter thick coal layer, as much as 30 meters of peat was
           originally required. Coal can vary from relatively pure carbon to
           carbon soaked with hydrocarbons, sulfur etc.
                  It  has  been  clear  for  decades  that  synthetic  oil  could  be
           created from coal. Coal gasification will transform  coal  into e.g.
           methane. Liquefaction  such as the  Fischer- Tropsch process will




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