Pressing flowers between pages…
Research Article| January 31, 1936 Tomichi Dome Flow J. T. STARK; J. T. STARK Search for other works by this author on: GSW Google Scholar C. H. BEHRE, JR. C. H. BEHRE, JR. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1936) 47 (1): 101–110. https://doi.org/10.1130/GSAB-47-101 Article history received: 07 Jun 1935 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation J. T. STARK, C. H. BEHRE; Tomichi Dome Flow. GSA Bulletin 1936;; 47 (1): 101–110. doi: https://doi.org/10.1130/GSAB-47-101 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTION AND ACKNOWLEDGMENTSTomichi Dome is a roughly hemispherical mountain in Gunnison County, southwestern Colorado (Fig. 1), some thirty miles west of the Continental Divide and about 20 miles east of Gunnison. Its crest is in the northeast comer of section 28, T. 49 N., R. 4 E. The new highway from Pitkin to Salida passes through Waunita Hot Springs in section 11, and the dome can best be ascended on foot from the northern side, where the hot springs are located.The dome is mapped on the Hayden atlas1 and on the geological map of Colorado published in 1913, as Carboniferous sediments. More recently, the fact that it consists mainly of igneous rock has been recognized, but geologists appear generally to regard this as intrusive. No detailed map of the area has hitherto been published, however, nor, so far as is known, have any careful petrographic studies of its . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.
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