Abstract: A method of separating and removing magnesium chloride hexahydrate from deep subterranean salt formations containing magnesium chloride hexahydrate, such as a carnallite bed or a bischofite bed, wherein one or more holes are drilled or provided through an overburden and into the bed. A solvent formed from any one of the lower saturated monohydric aliphatic alcohols having 1 to 4 carbon atoms, such as methanol, is directed downwardly in the hole and into contact with the bed, then upwardly through and out of the cased hole. Magnesium chloride hexahydrate is dissolved selectively by the solvent, but other salts, such as potassium chloride and sodium chloride, remain substantially insoluble in the solvent. The insolubles may be elevated out of the hole simultaneously with the lifting of the solvent-magnesium chloride hexahydrate solution or subsequent to such lifting.

Abstract: Hydraulic mining of tar sands in a formation wherein water is introduced into a plurality of spaced cavities in the bottom of a tar sands formation and above a number of tunnels communicating with respective cavities by openings. In one embodiment of the method, water is sprayed onto exposed tar sands surfaces in the cavity and further creates a moist atmosphere in those regions of the cavity where the water is not directly sprayed on the surfaces. The moist atmosphere can be in the form of suspended water droplets or can be saturated water vapor at a temperature above the ambient temperature of the tar sands or a combination of both. The water on the exposed surfaces penetrates the formation along paths of preferential wetability, causing adjacent portions of the formation to separate and break loose from the formation itself in a direction in which the portions are free to expand.

Abstract: Method for recovering bitumen from oil or tar sand using jets of hot water and/or steam introduced into the sand via raises connected to underlying spaced aprt tunnels. The jets are arcuately moved horizontally in overlapping patterns to slurry the sand. Caverns are formed by caving the tar sand and removal of the slurry into which the over burden is permitted to cave forming there above a surface depression usable as a tailing pond. Cavities are formed by other jets which connect with the priorly formed cavities so there is a continuous backward movement of interconnecting cavities.