PLATE 1 of 3

Total Page:16

File Type:pdf, Size:1020Kb

PLATE 1 of 3 110°00' W A' B' 109°00' W Qal Kmu Kmu C' Qal Qap Ks Kf Ks Kc Ks Kc 1100 Kc Kmb Kb Ks Ks Kf Qms Qes Qes 3 Kb Kc Kms Qap Kmu Qes Jctm Xb Xd Xd Xb 39° 00' N Kmu Qam Qes Ks Kmu Qap Qap Kms Qap Kd Xa Jk Jk Qmt Qat Qat Qap Qap Kc Kn Kmb Qms Kc Qap Qap Jsmt Qat Qmt Qmt Qea Qmt Kb Qes Qap Qat Kmu Qam Jk Qam Qap 500 5 Qap Qat Kcm Qes Qat R Qes Kc Qes Qes Qmt Qmt Qmt Kms Qam Kmu T c TRc Qal Kc Qes Kmb Kc Qam Jctm Jw Jk Xb Kmf Qap Qmt Qal Qes Qal Qat Jk Kb 3 Kc 4 Kc Qap Qap Jmb Qat Kmt Kf Kb Qap Kmu Kms Qat Qes Jk Jk Qmt TRc Qat Qap Qap Qmt Qal Kb Kb Qmt Qap Kmu Qal Qat Qat Qes Qes Jw Kmu Qam Qmt Kb Kc Kmu Qap Qap Qes Jes Qal Qea TRc Qmt Jk Qea Qat Kc 5 Kmb Qmt Kms Qam Kms Jw Xa Jw 1200 Kmu Qap Qmt Kms Qat Qes Xg Qam Kmu Qap Qap Qap Qmt Qam Jes Xd Qam Kmu Kmu Qes 600 Qes Kc Qmt Qes Kmu Qap Qap Kms Kmf Jn Qes Qap Qmt Qap Qmt 700 Kms Qat Qat Jctm Jk Qat TRc Xg Jw Qal 700 Qam 8 Qam Qes Jw Qmt Qam Qes Kb Qap Kb Qmt Qmt Qat 5 Qal Jk Xb Qes Qal Kc 600 Qap Qap Qam Qam Jcd Xf TRc Xb Jw Qap 800 Kc Qmt Qap Qal Qal TRc Jk Qal Qap Qap Kms Jes 1300 Jw Qes Qam Kmb Qmt Qat Kmu Qat Jms Xa Qat Kmf Kmu 900 Qap Kb Kmu Kmu Qat Qat Qal Jn Qes Qea Xb Xa Qmt Qap Qam Qap Kmu Kmt Qat Xf Jw Jk Qam Qam Qat Kms Kcm Qes Qal Qmt Jk Qea Kc Kb Qap Qap Qam Qam Qat Qes Jw Xa Qmt Qap Kmu Qam 1500 Jw Qat 1100 Qap Qap Qmt TGE #1 Kc Qmt Kc 1400 Jk Jk Kcm Qal 1000 Qam Qmt Kmu 800 Qal Qal Jw 1600 Xb Kmt Qap Qap Qmt Qap Qam Jk Jw 1300 Qap Qap Kmu Qam Kmf Kd Qes Jk Jw Kmu Kb Kmu Qap Qam Qat Qes Qmt Jmb Qap Kc Qat Xf Qap Qap Qam Qam Qam Qea Qal Xa TRc Kc Kmu 7 Qat Qea Jes Qal Qes TRc Qmt Jk Qes Qap Kmu Qam Qal Kd 1700 Jw Qat Qap Qam Qat Kmu Jcd Qes Qal Qap Qap Kc Kb Kms Kms Kms Qat Qap Jes 500 Qat Jw Jk Qat Qap Kc Qam Qam Qat Jcd Jk Xg Kcm Kb Kmu Kmu Kmu Kmf Kmt Qat Jmb Jk Xb Qap Kmu Qam Qal Qat 1800 Jk 1900 Jw Kmu Kms Kc Kmu Qap Qap TRc Qmt Kms Qap Kmu Qap Kmu 900 Qal Qap Qmt Kmu Qam Qam Kd Jcd Qat Qes Jk TRc Jk Jw Xa Xg Qat Qap Kb Qap Qal Qam Kms Jmb Qat Qal Qes Xa Xg Jw Qap Qam Qal Kms Qes Kmu Qam Qam Qat Qam 700 Jms Qal TRc Kms Qmt Kmu Qam Jk Xa Xb Qea Kmf Qap Qap Kmu Qag Qal Jw Jw Kb 5 Jsmt Jk Xb Xa Qmt Jk Qes Qal Qam Qam Kmf Jk Jk Qmt Qap Kmu Qam Mobil #1-30 Qam Qap Jw Qes Xb Xa Qmt 1400 Jsmt Jmb Kc Kmu Qat Kmu Kmt Jk Qmt Xb Yl Qap Qap Qam Qap Qap Kmu Qam Qat Kmt Qal Qat Jw Jms Kb Kms Qap Kc Qap Qat Kmf Kmt Jctm Qat Qea TRc Xg 2000 TRc Qal Qap Qam Qam Qam Kmf TRc Xb Jsmt Jms Qap Kms 1000 Qal Qat Qam Qat Jsmt Jk Xa Yap Xg Qmt Qst Qap Qap Qap Qat Kmf Jw Qat Qat Qap Kms Kmu Kcm Xa Xa Xb Xa Xg Qap Kms Kmt Qap Jmb Xb Qes Qap Qam Qal Xa Xa Qmt Qal Qap Kmu Qat Qal Qea Kd Xf Jk Kms Qap Qap Qam Kmu Qal Qms Qal Qal Qap Qam Qam TRc TRc Qat Qat Qap Qap Qat Qms Qat Jsmt Jctm Qea Qap Qam Qat Kmu Qat Qat Jmb Jw Xb TRc Kmt Qat Kcm Kd Jmb Kmf Kmu Kmu Qam Kd Qmt Jes Qap 600 Qap Qam Qam Qat Qal Qal Jw Jk Kmf Kmf Kmu Qat Qat Qam Qea Qal Jk Jk Qal Qap Kmu Qap Qal Qat Jmb Jw TRc Qam Qap Qat Qal 1100 Qat Qap Xg Xb Jk Qat Qal Kd Kmt Kmf Qam Kmu Qam Qat Qat Qea Qea 2100 Qal Qap Qat Qaf Qap Qat Kmu Qat Qap Kmf Kmt Jms TRc Xb Jes Kd Qam Kms Kms Qat Qat Qat Qmt Kcm Kmt Qap Qag Qap Qal Qal Jk Qal Kmf Qat Qap Qat Qat Kd Jms Qea Kmt Qam Kmu Jw Xg Qap Qap Qat Qam 1200 Qat Kmu Kms Qal Qap Qal Kmt Jk TRc Xb Qes Kmu Qap Qam Kmu Qaf Qam Qat Kmu Qat Qea Qal Qat Kms Qam Qap Qal Jk Xg Jk Qea Qat Qap Kmf Qam Qam Qal Qat Jsmt Qag TRc Yg Qaf Kmu Kmu Qat Qal Qap Kmt Kd Jctm Jw Qag Qat Kd Qam Qes Qat Kcm Qat Jes Yl Qmt Qes Kms Qal Qea Jw TRc Qmt 1200 Qat Qea Qes Kmt Qap Qal Qea Qat 1300 Qal Qat Qal Qat Kmu Qap Qat Qam Kmf Qat Xg 2200 Kmt Qat Qes Kd Kmu Kmu Kcm Jms Qea Jmb Qat Qal Kmu Kmu Qes Kmf Kms Qat Kcm Kd Xb Qal Qes Qam Kmf Kmu Kd Jcd Yap TRc Qea 1300 Qap Qat Qat Qam Qat Jw Qmt Qaf Qap Kmt 1200 Qal Qea Jms Kcm Qal Qes Qal Qap Jw Yap TRc Qat Qes 700 Qam Qat Kmt Jsmt Kmu Kmu 10 Kms Qat Jmb Kcm Qea Qmt Qat Qat Kmt Kmu Qat Qat 1400 Qat 1300 Jmb Qal Qam Kmu Qat Kd Qea Qea Qea Jw Jk Jw Qea Qea Qam Qat Qat Jcd Jw Kmf Jw Xg 7 Qam Qal Qat Kcm Qal TRc Kcm Qap Kmu Qat Qag Kcm Qat Qat Qam Kmu Qat Qat Qag Jw Qea Yg Kcm Kmu Qap 1500 Qat Kmu Kmu Kmu Jmb Qat Jsmt TRc Qat Kcm Kmt Qap Qea 1300 Qal Qal Jctm Jk Yg Qam Qal Kcm Qal Kmu Kmf Kms Qal Kd Jk 4 4 Kms Kms Kmu Kms Qat Kd Yap Qea Qaf Kms Qap Jw Qmt TRc 1400 Qal Kd Qea Kmu Qat Kms Jms Qms Qea Jmb Qes Kmt Qam Jmb Jes Kmt Qes Qat Kmf Qat Jsmt Jes Jw TRc Qes Jk Qal Qal Kd Kmf Kmu Qat Jctm Qag Jw Kmt Qat Kcm Qap Qal Qam Qap Kd Kd 1600 Jk Jmb Jmb Qea Kmf Kmt Kmu Kms Kmu Qat Qat Qat Qat Kmu Qat Qag Jmb Qal Qaf Qaf 3 Kmu Qat Qal Qms Qea Jms Jctm TRc Jk Kmt Kmf Qam Kcm Kmt Jmb 3 Qat Qea 1400 Qat Kmt Kmf Kmu Kmt Qat Jmb Kcm Qea 2300 Kcm Jmb Qat Qea Qat Kd Qal Qea Jw TRc Qea Qea Qat Kmf Qag Jmb Jms Jmb Qal Qea Kd Kmt Kd Jms Jms Jw Qea Kmt Qat Kmf Kd Qal Jsmt Jes Jk TRc Kcm Qes Kcm Qam Kd Kd Qam Jw Qmt Jms Qat Qat Qal Kmu Kd Kmt Qam Qat Qea Qea Jk Jms Qea Qea Qal Qal Kmu Kmf Qal Qag Qms 1700 Kcm Jmt Kcm Kmt 800 Kmt Kmf Kd Kmu 1400 Kmt Qag Jmb Jes Yg 500 Qal Qms Jn Kmu Qal 6 Kd Qag Qms Jw Kmt Jmb Qal Qea Qea Qea Kmt Qal Jes Jw Jw Qmt Jw Kd Jmt Qap Kcm Kd Kmf Qea Jw TRc Qat Qea Kd Kd 9 Kmf Qea Kmf Jmb 1800 Jk Qag Qam Kmf Kd Kd Qag Qal TRc Pc TRc Qea Js Kcm Kmu Kmf Qea Kmt Kmf Qat Kd Jcd Qes Jk Jk Kmt Kmu Kmf Kmt Kd Qmt Qmt Qal Qea Qes 1500 Qea Kd Qag Qea Qes Pc Jk Qat Jct Jms Qal Kmu 12 Qea Kd Qea Kmf Kmt Kd Jsmt Jn Jk Jmb Qst Jese Qal Qes Kd 7 Qea Kd Qat Kd Qmt Jw Jw Kcm Kmf Qea Kcm Qat Jmb TRc Qea Jmb Kmt Kd 4 Qes Jw Jmb Qam Kmf Qea Qea Qea Qea Jk TRc Qes Qat Qea Qes Kd 4 6 Jk TRc Yq Jmb Qag Qst Jmb Jmb Kcm Kcm Jmb Jk 2400 Qag Qes Kmf Kd Kmu Qea Kd Qes Kd Jk Qmt Jmb Kd Jcd Jmb Kd 1500 Kmt Jms Qes Jcd Jw Qea Qst Qes Kcm Kmu Qea Kcm Qes Qea 6 Kd Kmt Qal Qat Jms Kmt Jmb Kmt Kd Jmb Jk 900 Qea Qal Kd Jmb Qal Qat Qms Jk Jk Qal Qst Qes Qam Kdcm Qag Jmb 700 Jmb Jk Yg TRc Qal Qes Kmt Jmb Qal Qea Jmb Qea Kd Kcm TRc Jk Jmb Kcm Jese Jct Qes Qat Kmt Qea Jw Qmt Jn Kcm Qea Jw Jms Qag Qea Qea Kmf Kd Kcm Jes Jn Jk Qmt Jw Qal Jmt Jee Kdcm Kd Qal Qea Qes Jmb Qmt Jmb Qes Qes Qag Kmu 1500 Kd Kd Qea Jmb Qea Jw Jmb Kcm Js 1600 Jmb Jms Jes Jms Kd Qea Kd 6 Kcm Qms Qat Qes Jmt Qat Kd Kd 6 Qea Kd Kd Qal Jmt Qea Qea Qam Jn Qea Jms Qal Jms Qal Jctm Jctm 1600 Qea Kd Kd Qes Jes Qmt 600 Qal Qes IP Qat Qat Kd Jmb TRc Yg Jmt Kcm Jese Qes Kmf Kcm Jsmt Qal Qal Qes Ybg Jmt Qag Jese Qes Jmb Jmb Kmt Qea 5 Qea Jmb Jcd Js Jmt 1700 Qes Qea Qal Kmt Jsmt Jms Qea Jmb Qea Qea Qea Qea Jw Qat Qes Qes Qes Qat Kcm Jmb Qea Jk Jmb 1000 1600 Jsmt Qat Qat Qea Jes Kcm Qes Kmt Kd 1800 Qes Kcm Qea Qea Jmb 800 Jw Jk Ybg Jese Kmu Kmf Qes Kdcm Jmb Kcm Qea Jctm Qes Qes Kd Jmb Ybg Jct Js Jmt Kmf Jsmt Qea Qes Qea Kd Qea Jk Qaf Yg Qal Kcm Qes Qea Kmt Kcm Jn Jw Jms Qes Jee Qam Jctm Jctm Qal Qea Qes Qat Qms Jw Qea Jk Qat Qal Kmt Qal 13 Qag Qea Qea Jsmt Jw Jk Qes Qes Jmb Qat Qag Jes Qea Jms Qms Jctm Jk Qea Qea Jese Jmt Qam Jsmt Jsmt Qes Qea Qes Qes Jw Qat Jmb Qea Kmu IP Jcd Jmb Jmb Jms Jmb Qat Qea Jw Jw Jmt Qes Kd Qag Qea Jms Qal Qes Qea Qea Qes Qmt Qal Jms Qes Kcm Jk Kd Jmb Qea Qes Jctm Qal Qea Qat Kd Qes Jw Qes Qes Jmb Kcm Kmt Jmb Kcm Qat Qag Qag Qea Qes Kd Jcd Jmt Qes Qes Jms Jctm Qal Jsmt Qea Qea Jctm Jsmt Qes 5 Jmb Qea Jw Qea Qat IP Pure #1 Jmb Qea Jw Jk Qes Kcm Jmb Qea Jmb Jes Jctm 900 Qat TRc Jms Jct Jmt Qag Kd Qag Jsmt Jsmt Jms Qes Qat Jw Yg Jms 1100 Qam Qes Jw Jes Jsmt Kcm Jmb Qea Qea Jmb Qes Qal Qmt Pc Qmt Qes Kmt Kmf Kmu IP Qes Jes Kd Qea Qms Js Qal Kcm Continental Qes Qaf Qat Jms Qes Qea Kmu Qea Jctm Jms Jms Jsmt Qms Qes Qes Qat Jct Kd Qea Qms Qea Jms Kd Qes Qea Jw Qal Qes Jmt Qes Qes Kcm 4 Qat Jmb IP Jcd Qes Qea Qes Qes Qea Qat Jw Qmt Qmt Jctm Qes Jn TRc 30 Jctm TRc 800 Qea Jctm Kcm Qms Qea Pc Pc Kmu Qam Qea Jsmt Qms Qes Jsmt Jctm Qes Qea Kcm 4 Qes Qat Jmt Jmb 6 Qag Jmb Jmb Qes Qat Qat Jms Jmt Kmu Qes Jsmt Jes Qes Qat Jmb Jsmt TRc Qmt Jk Qea Qal Jsmt IP Qea Qea Qes Qat Qal Jcd 8 Qmt TRc Pc 1900 700 Qal Jms Kmf Kcm Jcd Qes Jk Kmu Qal Kcm 6 Qag Jmb IP 900 Jms Qea Jes Qms Jms Jn TRc Ybg 7 Kmu 7 Qea Jk Jn Jcd Jms Jsmt Jes Qes Jes Qms Jmb Jk 4 Jk Jct Js Jmt Qea Qea Qam Kmu Jms Jsmt Qes Qes Qes Qat Jct TRc Qes Jms Jcd Qal Pc Kmf Jctm Jctm Qes Qes Qes Qat Jmb Jes Jw Pc Pc Kcm Qes Jsmt Jcd 1000 Jms Qal Qms Jw D' Qat Js Kmf Jsmt Jsmt Jsmt Jms Jcd Qat Jmb TRc Jct Qes Jmb Jctm Jsmt IP Qea Jcd Jsmt Jctm Qes Qat Jcd Qat Qal Qat Jes Qea Kmt Jw 1000 Qes Qea Qes Qat Jct Qes Kcm Qes Jctm Qes Qms Jmb Qmt Jcd Kmu Qam Jmb Kd Jcd Qea Jw Qst Jee Jmb Kcm Jmb Jmb Jms Jctm Qes Qal Qal Qat Qes Jee Qea Qag Jes Jsmt 8 Qmt Jmb Qam Jee Texaco Smoot #2 Kcm Qam Qag Qea Jes 1100 Qea Qes Jsmt Qes Qes Qat Jsmt Jsmt Jcd Ject Jee Jw Qea Qal Qal Kmf 1200 Qes Qes Qes 4 Qal Kcm Kcm 8 Jee Jmb Qes Jsmt Jcd Jctm Jes Qes Jcd Qes Jctm Jmb Jsmt 1500 Jw Qmt Jes Jee Jes Kcm Kmf Jn Jcd Jn Jes Jcd 2000 Jms Jms Kd 1700 Qmt Qes Qat Qes 1800 Jmb 1600 Qea Jcu Jmb Jk Qes 1300 Qes Jes Qes Qat Jes Jn Jcec Js Jes Texaco #1 McKinnon Qes Qes Jn Qat Jcd Kd Jk Jw Jsmt Jmb Jee Jct Jctm Qes Qms Qat Jee Qes Qea Jmb Jsmt Jes Jcd Qes Qes Jcd 1100 5 Jcd Jk Qal Jct Jee Qea Jms Qes Jes Qat Jmb Qat Jctm Qea Qea Qes Shell 1-21 Jmb Jms Qea 1900 Jsmt Qes Jmb Jctm Qes Qes Qes Qal Jw Qea Jms Qes 1200 Qam Qal Qes Jcd Jn Jes Qmt Ject Jee Qag Qes 6 Jsmt Jn Qmt Jcd Qag Qed Jsc Qes Jn Qms Qat Qes Jes Jcd Jn Jw Qat Qat Qal Jsc Kmu Kmu Jctm Qes Qea Qes Jn Qea Jsmt Qea Qes Jk Qal Jms Kcm 5 Jn Jn Qmt Qal Qal Qag Jsmt Qal Jcd Jw Qea 1200 Jn 800 Jee Qea Jmb Qea Qea Jctm Jn Qmt Jcd Qes 7 Qmt Jes Qes Jms Jmb Jctm Jes Jn Qes Jms Qes Jee Qat Qes Kcm Kmf Jk Qes Jn Qes Qes Kcm Qea Jsmt Jctm Qes TRc Pc Qms Jmb Kmt Kcm Jctm Jsmt Qal Qat Jctm Jcd Qes Jk Qat Jsmt 7 Jsmt Qes Jms Jctm Jsmt Qes Qes Qat Jctm Jms Jn Jw Qmt Jes Jes Jsc Qes Qam Jmb Qea Jk Jms Qes Jee Jsmt Kmu Qag Jw IP Jsmt Qes Jcd Jmb Jcd Qea Qes Kcm Jes Qes Qmt Qes
Recommended publications
  • Ron Blakey, Publications (Does Not Include Abstracts)
    Ron Blakey, Publications (does not include abstracts) The publications listed below were mainly produced during my tenure as a member of the Geology Department at Northern Arizona University. Those after 2009 represent ongoing research as Professor Emeritus. (PDF) – A PDF is available for this paper. Send me an email and I'll attach to return email Blakey, R.C., 1973, Stratigraphy and origin of the Moenkopi Formation of southeastern Utah: Mountain Geologist, vol. 10, no. 1, p. 1 17. Blakey, R.C., 1974, Stratigraphic and depositional analysis of the Moenkopi Formation, Southeastern Utah: Utah Geological Survey Bulletin 104, 81 p. Blakey, R.C., 1977, Petroliferous lithosomes in the Moenkopi Formation, Southern Utah: Utah Geology, vol. 4, no. 2, p. 67 84. Blakey, R.C., 1979, Oil impregnated carbonate rocks of the Timpoweap Member Moenkopi Formation, Hurricane Cliffs area, Utah and Arizona: Utah Geology, vol. 6, no. 1, p. 45 54. Blakey, R.C., 1979, Stratigraphy of the Supai Group (Pennsylvanian Permian), Mogollon Rim, Arizona: in Carboniferous Stratigraphy of the Grand Canyon Country, northern Arizona and southern Nevada, Field Trip No. 13, Ninth International Congress of Carboniferous Stratigraphy and Geology, p. 89 109. Blakey, R.C., 1979, Lower Permian stratigraphy of the southern Colorado Plateau: in Four Corners Geological Society, Guidebook to the Permian of the Colorado Plateau, p. 115 129. (PDF) Blakey, R.C., 1980, Pennsylvanian and Early Permian paleogeography, southern Colorado Plateau and vicinity: in Paleozoic Paleogeography of west central United States, Rocky Mountain Section, Society of Economic Paleontologists and Mineralogists, p. 239 258. Blakey, R.C., Peterson, F., Caputo, M.V., Geesaman, R., and Voorhees, B., 1983, Paleogeography of Middle Jurassic continental, shoreline, and shallow marine sedimentation, southern Utah: Mesozoic PaleogeogÂraphy of west central United States, Rocky Mountain Section of Society of Economic Paleontologists and Mineralogists (Symposium), p.
    [Show full text]
  • Geology and Stratigraphy Column
    Capitol Reef National Park National Park Service U.S. Department of the Interior Geology “Geology knows no such word as forever.” —Wallace Stegner Capitol Reef National Park’s geologic story reveals a nearly complete set of Mesozoic-era sedimentary layers. For 200 million years, rock layers formed at or near sea level. About 75-35 million years ago tectonic forces uplifted them, forming the Waterpocket Fold. Forces of erosion have been sculpting this spectacular landscape ever since. Deposition If you could travel in time and visit Capitol Visiting Capitol Reef 180 million years ago, Reef 245 million years ago, you would not when the Navajo Sandstone was deposited, recognize the landscape. Imagine a coastal you would have been surrounded by a giant park, with beaches and tidal flats; the water sand sea, the largest in Earth’s history. In this moves in and out gently, shaping ripple marks hot, dry climate, wind blew over sand dunes, in the wet sand. This is the environment creating large, sweeping crossbeds now in which the sediments of the Moenkopi preserved in the sandstone of Capitol Dome Formation were deposited. and Fern’s Nipple. Now jump ahead 20 million years, to 225 All the sedimentary rock layers were laid million years ago. The tidal flats are gone and down at or near sea level. Younger layers were the climate supports a tropical jungle, filled deposited on top of older layers. The Moenkopi with swamps, primitive trees, and giant ferns. is the oldest layer visible from the visitor center, The water is stagnant and a humid breeze with the younger Chinle Formation above it.
    [Show full text]
  • Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In
    Appendix 2 Radioisotopic ages used in GTS2020 M.D. SCHMITZ 1285 1286 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Quaternary À not compiled Neogene À not compiled Pliocene Miocene Paleogene Oligocene Chattian Pg36 biotite-rich layer; PAC- Pieve d’Accinelli section, 43 35040.41vN, Scaglia Cinerea Fm, 42.3 m above base of 26.57 0.02 0.04 206Pb/238U B2 northeastern Apennines, Italy 12 29034.16vE section Rupelian Pg35 Pg20 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 145.8 m above base 31.41 0.03 0.04 206Pb/238U 145.8, equivalent to GSSP), northeastern Apennines, Italy 12 28003.83vE of section MCA/84-3 Pg34 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 142.8 m above base 31.72 0.02 0.04 206Pb/238U 142.8 GSSP), northeastern Apennines, Italy 12 28003.83vE of section Eocene Priabonian Pg33 Pg19 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 14.7 m above base of 34.50 0.04 0.05 206Pb/238U 14.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-14.7 Italy Pg32 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.9 m above base of 34.68 0.04 0.06 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E section Italy Pg31 Pg18 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.7 m above base of 34.72 0.02 0.04 206Pb/238U
    [Show full text]
  • Lexique Stratigraphique Canadien - Volume V-B - Region Des Appalaches, Des Basses-Terres Du Saint-Laurent Et Des Iles De La Madeleine Lexique Stratigraphique
    DV 91-23 LEXIQUE STRATIGRAPHIQUE CANADIEN - VOLUME V-B - REGION DES APPALACHES, DES BASSES-TERRES DU SAINT-LAURENT ET DES ILES DE LA MADELEINE LEXIQUE STRATIGRAPHIQUE CANADIEN Volume Fa Région des Appalaches, des Basses-Terres du Saint-Laurent et des îles de la Madeleine par Yvon Globensky et collaborateurs 1993 Québec ©© LEXIQUE STRATIGRAPHIQUE CANADIEN Volume r-8 Région des Appalaches, des Basses-Terres du Saint-Laurent et des Îles de la Madeleine par Yvon Globensky et collaborateurs DV 91-23 1993 Quebec ®® DIRECTION GÉNÉRALE DE L'EXPLORATION GÉOLOGIQUE ET MINÉRALE Sous-ministre adjoint: R.Y. Lamarche DIRECTION DE LA RECHERCHE GÉOLOGIQUE Directeur: A. Simard, par intérim SERVICE GÉOLOGIQUE DE QUÉBEC Chef: J.-M. Charbonneau Manuscrit soumis le: 30-01-91 Accepté pour publication le: 14-06-91 Lecteur critique J. Béland Édition Géomines / F. Dompierre Préparé par la Division de l'édition (Service de la géoinformation, DGEGM) Couvert 1: 1) Paucicrura rogata et Platystrophia amoena. Membre de Rosemont. Au SW de Saint-Jean-sur-Richelieu. Photo: tirée de Globensky, 1981b, page 39 2) Formation de Solomon's Corner. Saint-Armand-Station. Photo: tirée de Globensky, 1981b, page 126 3) Faciès de Terrebonne, formation de Tétreauville. Rivière L'Assomption. Photo: Y. Globensky 4) Formation de Covey Hill. Coupe à l'extrémité NW du lac Gulf, à l'ouest de Covey Hill. Photo: tirée de Globensky, 1986, page 9 Couvert 4: 1) Formation d'Indian Point. Péninsule de Forillon. Photo: D. Brisebois 2) Coupe type de la Formation de Wallace Creek. Étang Streit, près de Philipsburg. Photo: tirée de Globensky, 1981b, page 101 3) Euomphalopsis sp.
    [Show full text]
  • Mesozoic Stratigraphy at Durango, Colorado
    160 New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin, 2005, p. 160-169. LUCAS AND HECKERT MESOZOIC STRATIGRAPHY AT DURANGO, COLORADO SPENCER G. LUCAS AND ANDREW B. HECKERT New Mexico Museum of Natural History and Science, 1801 Mountain Rd. NW, Albuquerque, NM 87104 ABSTRACT.—A nearly 3-km-thick section of Mesozoic sedimentary rocks is exposed at Durango, Colorado. This section con- sists of Upper Triassic, Middle-Upper Jurassic and Cretaceous strata that well record the geological history of southwestern Colorado during much of the Mesozoic. At Durango, Upper Triassic strata of the Chinle Group are ~ 300 m of red beds deposited in mostly fluvial paleoenvironments. Overlying Middle-Upper Jurassic strata of the San Rafael Group are ~ 300 m thick and consist of eolian sandstone, salina limestone and siltstone/sandstone deposited on an arid coastal plain. The Upper Jurassic Morrison Formation is ~ 187 m thick and consists of sandstone and mudstone deposited in fluvial environments. The only Lower Cretaceous strata at Durango are fluvial sandstone and conglomerate of the Burro Canyon Formation. Most of the overlying Upper Cretaceous section (Dakota, Mancos, Mesaverde, Lewis, Fruitland and Kirtland units) represents deposition in and along the western margin of the Western Interior seaway during Cenomanian-Campanian time. Volcaniclastic strata of the overlying McDermott Formation are the youngest Mesozoic strata at Durango. INTRODUCTION Durango, Colorado, sits in the Animas River Valley on the northern flank of the San Juan Basin and in the southern foothills of the San Juan and La Plata Mountains. Beginning at the northern end of the city, and extending to the southern end of town (from north of Animas City Mountain to just south of Smelter Moun- tain), the Animas River cuts in an essentially downdip direction through a homoclinal Mesozoic section of sedimentary rocks about 3 km thick (Figs.
    [Show full text]
  • Climbs and Expeditions, 1988
    Climbs and Expeditions, 1988 The Editorial Board expresses its deep gratitude to the many people who have done so much to make this section possible. We cannot list them all here, but we should like to give particular thanks to the following: Kamal K. Guha, Harish Kapadia, Soli S. Mehta, H.C. Sarin, P.C. Katoch, Zafarullah Siddiqui, Josef Nyka, Tsunemichi Ikeda, Trevor Braham, Renato More, Mirella Tenderini. Cesar Morales Arnao, Vojslav Arko, Franci Savenc, Paul Nunn, Do@ Rotovnik, Jose Manuel Anglada, Jordi Pons, Josep Paytubi, Elmar Landes, Robert Renzler, Sadao Tambe, Annie Bertholet, Fridebert Widder, Silvia Metzeltin Buscaini. Luciano Ghigo, Zhou Zheng. Ying Dao Shui, Karchung Wangchuk, Lloyd Freese, Tom Elliot, Robert Seibert, and Colin Monteath. METERS TO FEET Unfortunately the American public seems still to be resisting the change from feet to meters. To assist readers from the more enlightened countries, where meters are universally used, we give the following conversion chart: meters feet meters feet meters feet meters feet 3300 10,827 4700 15,420 6100 20,013 7500 24,607 3400 11,155 4800 15,748 6200 20,342 7600 24,935 3500 11,483 4900 16,076 6300 20,670 7700 25,263 3600 11,811 5000 16,404 6400 20,998 7800 25,591 3700 12,139 5100 16,733 6500 21,326 7900 25,919 3800 12,467 5200 17.061 6600 21,654 8000 26,247 3900 12,795 5300 7,389 6700 21,982 8100 26,575 4000 13,124 5400 17,717 6800 22,3 10 8200 26,903 4100 13,452 5500 8,045 6900 22,638 8300 27,231 4200 13,780 5600 8,373 7000 22,966 8400 27,560 4300 14,108 5700 8,701 7100 23,294 8500 27,888 4400 14,436 5800 19,029 7200 23,622 8600 28,216 4500 14,764 5900 9,357 7300 23,951 8700 28,544 4600 15,092 6000 19,685 7400 24,279 8800 28,872 NOTE: All dates in this section refer to 1988 unless otherwise stated.
    [Show full text]
  • Redbeds of the Upper Entrada Sandstone, Central Utah
    Brigham Young University BYU ScholarsArchive All Theses and Dissertations 2016-12-01 Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Geology Commons BYU ScholarsArchive Citation Valenza, Jeffery Michael, "Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments" (2016). All Theses and Dissertations. 6112. https://scholarsarchive.byu.edu/etd/6112 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in All Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Thomas H. Morris, Chair Jani Radebaugh Sam Hudson Scott M. Ritter Department of Geological Sciences Brigham Young University Copyright © 2016 Jeffery Michael Valenza All Rights Reserved ABSTRACT Redbeds of the Upper Entrada Sandstone, Central Utah: Facies Analysis and Regional Implications of Interfingered Sabkha and Fluvial Terminal Splay Sediments Jeffery Michael Valenza Department of Geological Sciences, BYU Master of Science First distinguished from other sedimentary successions in 1928, the Entrada Sandstone has been the subject of numerous studies.
    [Show full text]
  • Oil and Gas Plays Ute Moutnain Ute Reservation, Colorado and New Mexico
    Ute Mountain Ute Indian Reservation Cortez R18W Karle Key Xu R17W T General Setting Mine Xu Xcu 36 Can y on N Xcu McElmo WIND RIVER 32 INDIAN MABEL The Ute Mountain Ute Reservation is located in the northwest RESERVATION MOUNTAIN FT HALL IND RES Little Moude Mine Xcu T N ern portion of New Mexico and the southwestern corner of Colorado UTE PEAK 35 N R16W (Fig. UM-1). The reservation consists of 553,008 acres in Montezu BLACK 666 T W Y O M I N G MOUNTAIN 35 R20W SLEEPING UTE MOUNTAIN N ma and La Plata Counties, Colorado, and San Juan County, New R19W Coche T Mexico. All of these lands belong to the tribe but are held in trust by NORTHWESTERN 34 SHOSHONI HERMANO the U.S. Government. Individually owned lands, or allotments, are IND RES Desert Canyon PEAK N MESA VERDE R14W NATIONAL GREAT SALT LAKE W Marble SENTINEL located at Allen Canyon and White Mesa, San Juan County, Utah, Wash Towaoc PARK PEAK T and cover 8,499 acres. Tribal lands held in trust within this area cov Towaoc River M E S A 33 1/2 N er 3,597 acres. An additional forty acres are defined as U.S. Govern THE MOUND R15W SKULL VALLEY ment lands in San Juan County, Utah, and are utilized for school pur TEXAS PACIFIC 6-INCH OIL PIPELINE IND RES UNITAH AND OURAY INDIAN RESERVATION Navajo poses. W Ramona GOSHUTE 789 The Allen Canyon allotments are located twelve miles west of IND RES T UTAH 33 Blanding, Utah, and adjacent to the Manti-La Sal National Forest.
    [Show full text]
  • Late Cretaceous Stratigraphy of Black Mesa, Navajo and Hopi Indian Reservations, Arizona H
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/9 Late Cretaceous stratigraphy of Black Mesa, Navajo and Hopi Indian Reservations, Arizona H. G. Page and C. A. Repenning, 1958, pp. 115-122 in: Black Mesa Basin (Northeastern Arizona), Anderson, R. Y.; Harshbarger, J. W.; [eds.], New Mexico Geological Society 9th Annual Fall Field Conference Guidebook, 205 p. This is one of many related papers that were included in the 1958 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • Lithology and Subdivisions of the Jurassic Stump Formation in Southeastern Idaho and Adjoining Areas
    Lithology and Subdivisions of the, . „ - nj,Jurassic ~ - -' - - - - Stump- - - - JL": •-Formation - - - - - in Southeastern Idaho and dning iGEOLOGlCAL SURVEY PROFESSIONAL PAPER 1035-C Lithology and Subdivisions of the Jurassic Stump Formation in Southeastern Idaho and Adjoining Areas By GEORGE N. PIPIRINGOS and RALPH W. IMLAY UNCONFORMITIES, CORRELATION, AND NOMENCLATURE OF SOME TRIASSIC AND JURASSIC ROCKS, WESTERN INTERIOR UNITED STATES GEOLOGICAL SURVEY PROFESSIONAL PAPER 1035-C Marked rapid lateral changes in lithology, fossil content, and thickness of the Stump Formation are due principally to erosion associated with the Cretaceous (K) and Jurassic (]-4) unconformities UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Pipiringos, George Nicholas, 1918- Lithology and subdivisions of the Jurassic stump formation in southeastern Idaho and adjoining areas. (Unconformities, correlation, and nomenclature of some Triassic and Jurassic rocks, western interior United States) (Geological Survey Professional Paper 1035-C) Bibliography: p. 25 1. Geology, Stratigraphic Jurassic. 2. Geology Idaho. 3. Geology The West. 4. Petrology Idaho. 5. Petrology-The West. I. Imlay, Ralph Willard, 1908-joint author. II. Title. HI. Series. IV. Series: United States Geological Survey Professional Paper 1035-C. QE681.P49 551.7'6 78-1687 For sale by the Superintendent of Documents, U.S. Government
    [Show full text]
  • Geology of the Northern Portion of the Fish Lake Plateau, Utah
    GEOLOGY OF THE NORTHERN PORTION OF THE FISH LAKE PLATEAU, UTAH DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State - University By DONALD PAUL MCGOOKEY, B.S., M.A* The Ohio State University 1958 Approved by Edmund M." Spieker Adviser Department of Geology CONTENTS Page INTRODUCTION. ................................ 1 Locations and accessibility ........ 2 Physical features ......... _ ................... 5 Previous w o r k ......... 10 Field work and the geologic map ........ 12 Acknowledgements.................... 13 STRATIGRAPHY........................................ 15 General features................................ 15 Jurassic system......................... 16 Arapien shale .............................. 16 Twist Gulch formation...................... 13 Morrison (?) formation...................... 19 Cretaceous system .............................. 20 General character and distribution.......... 20 Indianola group ............................ 21 Mancos shale. ................... 24 Star Point sandstone................ 25 Blackhawk formation ........................ 26 Definition, lithology, and extent .... 26 Stratigraphic relations . ............ 23 Age . .............................. 23 Price River formation...................... 31 Definition, lithology, and extent .... 31 Stratigraphic relations ................ 34 A g e .................................... 37 Cretaceous and Tertiary systems . ............ 37 North Horn formation. ..........
    [Show full text]
  • Italic Page Numbers Indicate Major References]
    Index [Italic page numbers indicate major references] Abbott Formation, 411 379 Bear River Formation, 163 Abo Formation, 281, 282, 286, 302 seismicity, 22 Bear Springs Formation, 315 Absaroka Mountains, 111 Appalachian Orogen, 5, 9, 13, 28 Bearpaw cyclothem, 80 Absaroka sequence, 37, 44, 50, 186, Appalachian Plateau, 9, 427 Bearpaw Mountains, 111 191,233,251, 275, 377, 378, Appalachian Province, 28 Beartooth Mountains, 201, 203 383, 409 Appalachian Ridge, 427 Beartooth shelf, 92, 94 Absaroka thrust fault, 158, 159 Appalachian Shelf, 32 Beartooth uplift, 92, 110, 114 Acadian orogen, 403, 452 Appalachian Trough, 460 Beaver Creek thrust fault, 157 Adaville Formation, 164 Appalachian Valley, 427 Beaver Island, 366 Adirondack Mountains, 6, 433 Araby Formation, 435 Beaverhead Group, 101, 104 Admire Group, 325 Arapahoe Formation, 189 Bedford Shale, 376 Agate Creek fault, 123, 182 Arapien Shale, 71, 73, 74 Beekmantown Group, 440, 445 Alabama, 36, 427,471 Arbuckle anticline, 327, 329, 331 Belden Shale, 57, 123, 127 Alacran Mountain Formation, 283 Arbuckle Group, 186, 269 Bell Canyon Formation, 287 Alamosa Formation, 169, 170 Arbuckle Mountains, 309, 310, 312, Bell Creek oil field, Montana, 81 Alaska Bench Limestone, 93 328 Bell Ranch Formation, 72, 73 Alberta shelf, 92, 94 Arbuckle Uplift, 11, 37, 318, 324 Bell Shale, 375 Albion-Scioio oil field, Michigan, Archean rocks, 5, 49, 225 Belle Fourche River, 207 373 Archeolithoporella, 283 Belt Island complex, 97, 98 Albuquerque Basin, 111, 165, 167, Ardmore Basin, 11, 37, 307, 308, Belt Supergroup, 28, 53 168, 169 309, 317, 318, 326, 347 Bend Arch, 262, 275, 277, 290, 346, Algonquin Arch, 361 Arikaree Formation, 165, 190 347 Alibates Bed, 326 Arizona, 19, 43, 44, S3, 67.
    [Show full text]