This, however, is not sufficient to establish the pyrogenic origin of all crystallized paraffine, as crystals can be obtained from the amorphous residues by distillation at normal or reduced pressure or in a current of steam.  To explain these facts two assumptions are possible.  Either the chemical and physical properties of all or some of the solid constituents are changed by the distillation, and the paraffine is changed from the amorphous into the crystalline variety, or the change produced by the distillation takes place in the medium (i.e., the mother liquid) in which the paraffine exists.  The change effected in ozokerite and in petroleum residues when crystalline paraffine is obtained by distillation is to be regarded as a purification, and can be effected partially by treatment with amyl alcohol.  In the same way, by repeated treatment of petroleum residuum with amyl alcohol, a substance of melting point 59 deg.  C. can be obtained, which cannot be distinguished from ordinary paraffine.

The treatment with amyl alcohol has therefore accomplished the same results as was obtained by distillation, and the action is probably the same, i.e., a partial separation of colloid substance.  These facts point to the conclusion that crystallizable paraffine exists ready formed in both petroleum and in ozokerite, but in both cases other colloidal substances prevent its crystallization.  By distillation, these colloids appear to be destroyed or changed so as to allow the paraffine to crystallize.

It is a generally known fact that liquids always appear among the products of the distillation of paraffine, no matter in what way the distillation be conducted.  This shows that some paraffine is decomposed in the operation.

The name proto-paraffine has been given to ozokerite and to the paraffine of petroleum in contradistinction to pyro-paraffine, the name that has been applied to the paraffine obtained by distillation from any source.

According to Reichenbach, paraffine may crystallize in three forms:  needles, angular grains, and leaflets having the luster of mother-of-pearl.  Hofstadter, in an article on the identity of paraffine from different sources, confirmed this statement, and added further that at first needles, then the angular forms, and then the leaflets are formed.  Fritsche found, by means of the microscope, in the ethereal solution of ozokerite, very fine and thin crystal leaflets concentrically grouped, and in the alcoholic solution fine irregular leaflets.  Zaloziecki has recently developed these microscopic investigations to a much greater extent.  According to this observer, the principal part of paraffine, as seen under the microscope, consists of shining stratified leaflets with a darker edge.  The most characteristic and well developed crystals are formed by dissolving paraffine in a mixture of ethyl and amyl alcohols and chilling.  The crystals are rhombic or hexagonal tablets or leaves, and are quite regularly formed.  They are unequally developed in different varieties of paraffine.  The best developed are those obtained from ceresine.  Their relative size and appearance give an indication as to the purity of the paraffine, and, as they are always present, they are to be counted among the characteristic tests for paraffine.  Reichenbach observed that mere traces of empyreumatic oil prevented their formation.