4 Technology-Driven Active Learning in the Geosciences
Sunday, 14 March 2021
8:00 AM - 12:00 PM
Talcott
USE OF DRONE TECHNOLOGY AND 3D VISUALIZATION SOFTWARE FOR VIRTUAL FIELD TRIP CREATION: PEBBLE BLUFF OUTCROP IN THE NEWARK BASIN, NEW JERSEY
Paper number: 4-5
Program: Theme Sessions
Time: 9:05 AM – 9:25 AM
Authors
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Lauren Neitzke AdamoRutgers University Geology Museum Office of STEM Education, New Brunswick, NJ
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Kenneth MillerRutgers University610 Taylor Road, Earth & Planetary Sci, Piscataway, NJ
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Christian RowanRutgers University, Piscataway, NJ
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James V. BrowningRutgers University, Piscataway, NJ
Abstract
The Pebble Bluff section exposes the Upper Triassic (ca. 215 Ma) Perkasie Member of the Passaic Formation that consists of predominant matrix supported and subordinate grain-supported conglomerates interbedded with sandstones, representing debris flows and wash out deposits on an alluvial fan formed by the border faults (Olsen and Kent 1992). The upper 15 m of the section contains two 7.5 m thick cycles punctuated by cross-bedded sandstone and shales, indicating a lacustrine shoreline and deep lake deposits controlled by short ~20 kyr precessional cycle (Van Houten 1969, Olsen et al. 1996). This cyclicity can clearly be seen in the outcrop and tied to existing cores and outcrops away from the border fault in lacustrine strata. The outcrop’s cyclicity and diverse lithology make the site well suited for exploring sedimentological and stratigraphic concepts.
The learning objectives are for students to 1) identify different lithologies and sedimentary features; 2) recognize stratigraphic patterns in the outcrop that relate to cyclicity, and 3) relate cyclicity to climate change. SfM was used to make 3D models of the outcrop, hand samples, and corresponding sedimentary drill cores from the site. 360 videos and photographs were used to show finer-scale sedimentary details and structures. Although this collection of resources cannot replace the field, it allows students to make similar measurements and observations as they would when walking alongside an actual outcrop.
Geological Society of America Abstracts with Programs. Vol. 53, No. 1
doi: 10.1130/abs/2021NE-361732
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