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Classic Geologic Outcrops: Preservation and Future Accessibility

Marjorie A. Chan, Dept. of Geology & Geophysics, University of Utah, Salt Lake City, Utah 84112, USA, marjorie.chan@utah.edu;
Diane L. Kamola, Dept. of Geology, University of Kansas, Lawrence, Kansas 66045, USA, kamola@ku.edu

INTRODUCTION                                  GEOCONSERVATION, ETHICAL                                Blackhawk Formation (Fig. 2). The scar-
                                              ISSUES, AND CHALLENGES                                  ring is permanent, despite later efforts to
  Geologists are privileged to work in                                                                fill the drill holes.
some of the most remarkable, beautiful,         Geoconservation focuses on recognizing
and remote areas on the Earth. As profes-     and preserving unique sites and landscapes                Sadly, these are not isolated incidents.
sionals, we must care for important outcrops  that have important scientific value and add            Great outcrops deserve respect. We must
so they can continue to enlighten and edu-    to our quality of life. Some efforts have               protect Earth’s library of information; a
cate earth scientists well into the future.   resulted in global designations for UNESCO              photo is never the same as seeing a geologic
Rock archives of valuable information,        Geoparks and World Heritage sites (e.g.,                feature in outcrop. While modest and dis-
and access to these outcrops, can be          O’Halloran et al., 1994; Burek and Prosser,             creet sampling of some outcrops is critical
destroyed by a few thoughtless actions.       2008). The U.S. National Park Service pro-              to advancing our science, there is no legiti-
Accessible, exemplary geologic sites are      tects many beloved landscapes, but other                mate reason to deface a classic outcrop.
visited by numerous individuals and field-    public-owned lands with remote sites are
trip groups each year. The consequences       difficult to manage with limited resources.               Numerous classic outcrops on private
of unauthorized access, and the impact of     Vandalism of outcrops on public land has                land have been accessed by geology groups
rock hammers, painted section numbers,        occurred on classic sites, such as the expo-            for decades, and are important for teaching
drill plug holes, and other evidence of       sure of the Moab fault in Bartlett Wash                 basic concepts and skills to the geologic
increasing visits to these classic sites has  near Moab, Utah, USA (B. Trudgill, 2017,                community (Mogk, 2004). A prime exam-
serious consequences. In order to protect     pers. comm.). In this instance, people with-            ple is the Cretaceous of the northern Book
continued access for students and research-   out required permits from the U.S. Bureau               Cliffs, near Helper, Utah, USA. Numerous
ers, we, as a geologic community, must act    of Land Management (BLM) cut a chunk                    field trips routinely stop at Gentile Wash
responsibly by getting proper permits where   of rock with deformation bands from a                   (Fig. 3) to observe classic fluvial-dominated
required, conserving and protecting clas-     pristine outcrop exposure adjacent to the               delta front and shelf turbidites in the Panther
sic localities, and respecting land-use       fault, leaving a gaping hole (Fig. 1).                  Tongue (Newman and Chan, 1991; Van
rules. In the following, we discuss a few                                                             Wagoner et al., 1990; Olariu et al., 2010),
examples of the preservation and acces-         At another highly visited locality                    or to see classic wave-dominated para­
sibility of classic outcrops we have studied  (Tuscher Canyon) in the Book Cliffs,                    sequences of the Blackhawk Formation
for years, recognizing that similar issues    numerous drill holes were cut into world-               (Van Wagoner et al., 1990; Kamola and
are prevalent globally.                       class exposures of hummocky cross-                      Van Wagoner, 1995). The number of
                                              stratified sandstone of the Cretaceous                  groups at times makes it seem like you

SW NE

   Je Kcm                                                                                             Figure 1. A well-visited exposure
                                                                                                      of a splay off the Moab fault near
                                                                                                      Moab, Utah, USA. (A) The eolian
                                                                                                      Jurassic Slickrock Member of the
                                                                                                      Entrada Sandstone (Je) is juxta-
                                                                                                      posed against the Cretaceous
                                                                                                      Cedar Mountain Formation (Kcm).
                                                                                                      Credit: M. Chan. (B) A ~ 60 cm chunk
                                                                                                      of slickrock sandstone was cut
                                                                                                      and removed in 2011 without
                                                                                                      proper permission and BLM per-
                                                                                                      mits. Credit: B. Trudgill.

A  Footwall                                   Hanging wall B

     GSA Today, v. 27, doi: 10.1130/GSATG343GW.1. Copyright 2017, The Geological Society of America.

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