Page 5 - i1052-5173-30-6
P. 5

N N N
               E E E


                                                               accretion
                                                     paleo ow
                                                     paleo ow  accretion                                        channel-belt deposit
                                     2
                                     2 mm
                   channel-belt base                                       oodplain mudstone      channel-belt base
         Figure 1. Geologic interpretations (line drawing on 2D field photograph), a common conventional method to highlight stratigraphic architecture and distri-
         bution of related units. Mudstones are gray to light brown; sandstones are light gray to white. This process is often performed on photos or a photomosaic
         acquired in the field.




             ALBERTA


                                                                  Figure 2. Traditional geologic map used to share field measurements,
              Dinosaur                                            observations, and interpretations in 2D plan-view. This geologic map
             Provincial                                           was constructed from the integration of traditional fieldwork methods
                                                                  (measured sections as well as paleoflow and bedding measurements)
                  Park                                            with digital outcrop model mapping to characterize heterolithic chan-
         111.59º W                                                nel-belt deposits exposed at Dinosaur Provincial Park, southeastern
                                                  meander-belt edge
                                                                  Alberta, Canada. Field-based Facies Associations (FA)1—sandy point
          50.82º N                                                bar; FA2—heterolithic point bar; FA3—Counter-point bar; FA4—aban-
                                                                  doned channel; FA5—mudstone. Bedding surfaces, noted in Figure 1
              Extent of                                 Fig. 1    (red), were digitally mapped on the 3D model and yield a more refined
              3D model                                            and detailed interpretation of accretion surface orientation and strati-
                                                                  graphic architecture. These methods are being widely applied, yet the
              Measured                                            results are difficult to disseminate and share in 3D.
              section
              Strike/Dip
              of bedding                                   N
              Interpreted                           200 m
              scroll pattern

                         FA1  FA2 FA3 FA4   FA5


         specialized software, or transfer and storage   bottlenecks remain, with a lack of accessible   issues relative to underlying base layers
         of large files. This prompts an increased   visualization software and the need to trans-  (Tavani et al., 2014).
         ability to share data sets, interpretations, and   fer large files.      Web-based dissemination may be one of
         results with a wider community, expanding   Though separate 3D viewers are available   the most promising and practical means for
         opportunities for scientific communication   to supplement proprietary software (e.g.,   rapidly streaming 3D digital data sets with-
         and open science education.         Trimble RealWorks, FugroViewer), they typ-  out transferring raw data (Turner, 2006; von
                                             ically require local storage of large files,   Reumont et al., 2013). Advances of applica-
         RELATED WORK                        learning curves, and have associated licens-  tion programming interfaces (APIs), such as
          Visualization of digital 3D models has   ing restrictions. Alternative applications,   WebGL, allow modern Internet browsers to
         been practical for more than two decades;   such as digital globes (e.g., Google Earth) are   access the local GPU to improve rendering of
         however, early geoscience applications were   a popular method for disseminating spatial   2D and 3D graphics, without the need for
         typically restricted to dedicated geovisual-  and non-spatial data in an interactive, semi-  plug-ins or extensions (Boutsi et al., 2019).
         ization labs and required specialized soft-  immersive environment, with intuitive con-  Though not guaranteed, WebGL enables
         ware (e.g., Thurmond et al., 2006; Jones et   trols (Goodchild et al., 2012). Digital globes   GPU functionality on various operating sys-
         al., 2009; Bilke et al., 2014). Today, visual-  have been used to create “virtual field trips”   tems and devices (Schuetz, 2016). Several
         ization of large 3D data sets is no longer lim-  (McCaffrey  et  al.,  2010;  Simpson  and  De   proprietary web viewers, such as Sketchfab
         ited to sophisticated labs, but rather an aver-  Paor, 2010; De Paor and Whitmeyer, 2011)   (https://www.sketchfab.com), use WebGL
         age  computer  can  render  3D  models  ef-   and present 3D data sets (Blenkinsop, 2012;   for sharing 3D models. Proprietary web-
         ficiently, due in large part to inexpensive   De Paor, 2016). Although digital globes pro-  based viewers have recently been used by
         hardware, such as dedicated graphics pro-  vide tremendous benefits, displaying DOMs   geologic databases (e.g., Safari Database,
         cessing units  (GPUs).  Despite  the  capa-   within digital globes requires a significant   https://www.safaridb.com: Howell et al.,
         bilities  of  modern  computing  hardware,   reduction of detail and results in overlay   2014; eRock: Cawood et al., 2019).
                                                                                        www.geosociety.org/gsatoday  5
   1   2   3   4   5   6   7   8   9   10