KNOWLEDGE OF EARTH STRUCTURE 167 



originally of sedimentary origin,) gives rise to "igneous" rocks 

 often not distinguishable from other igneous rocks, when it is 

 ejected through fissures far from its place of origin ; while crys- 

 talline rocks are simply metamorphic if they remain in their 

 original relations to the associated rocks, or nearly so. 



Between these latter igneous rocks and the metamorphic there 

 may be indefinite gradations, as claimed by Hunt. But if our 

 reasonings are right, the great part of igneous rocks can be 

 proved to have had no such supercrust origin. The argument 

 from the presence of moisture or of hydrous minerals in such 

 rocks in favor of their origin from the fusion of sediments has 

 been shown to be invalid. ' ' 



The injected marginal rocks and the post-intrusive 

 metamorphism of most of the New England granites has, 

 however, obscured more or less their real igneous nature 

 so that the gradation from metamorphic sediments 

 through igneous gneisses to granites could be read in 

 either direction. These features misled Dana who 

 accepted the prevailing idea of the general metamorphic 

 origin of granite. Dana makes the following statement 

 (6, 164, 1873) : 



"But Hunt is right in holding that in general granite and 

 syenite (the quartz-bearing syenite) are undoubtedly meta- 

 morphic rocks where not vein-formations, as I know from the 

 study of many examples of them in New England; and the 

 veins are results of infiltration through heated moisture from 

 the rocks adjoining some part of the opened fissures they fill." 



Granite, although regarded at this time as the extreme 

 of the metamorphic series and originating from sedi- 

 ments, was looked upon as typically Archean in age, 

 though in some cases younger. Such a doctrine per- 

 mitted such extreme misinterpretations as that of 

 Clarence King and S. F. Emmons on the nature of the 

 intrusive granite of the Little Cottonwood canyon in the 

 Wahsatch Range. This body cuts across 30,000 feet of 

 Paleozoic rocks and to the careful observer^ as later 

 admitted by Emmons, shows clear evidence of its trans- 

 gressive nature. But at that time it was generally con- 

 sidered that granite mountains were capable of resist- 

 ing the erosion of all geological time. Consequently it 

 did not seem incredible to King and his associates that 

 here a great granite range of Archean origin had stood 



