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Show series than series. Thus, it from the was were do those in the they since the is concluded either that the direction of flow southwest, formerly much or Precambrian, p3.rticularly by source source the tilloid is of the carbonate truly glacial, trans port) Fault. , . by Tertiary some was fresh state the tilloid, then the distance a-ay because (IRrticularly regardless This some possibility t.ha t the .. eroded and faul ted. out was a gives source Va.lley could the Sal t more· a of the distance of by source movement direction oppcs i.t.e to the only area. area. the Hinera.l· Fork, in idea and 1s Valley. the ultima.te source Sheep.rock Range, the islands of the Great a.s. of the lithologies in the tl110id of the Mineral Fork Formation will become known after extensive work with similar Preca.mbrian to the along the. Vasa tch popular tilloids in the Lake, and. in many other nearby conglomerates ws in the present loea. tien of the Salt Lake easily explain Deepcreek Range, Probably, and if glacial transport tends to hard to prove without bedrock data from the Salt lake However, However, if is unknown. • There may be west,' but a destroyed by changes a.ssimila tion fragments fragments ma.y have been preserve clasts in metamorphics area. the immedlate source of the ultimate that the Little Willow extensive and have been more intrusions in the general The Farmington Canyon metamorphic "glacial" forma.tlons lithologies in nearby ' . |
