Abstract

Aerial drone photography of an active pit within a sand and gravel quarry in DeSoto County, Mississippi, was conducted to better understand the Upland Complex, which is a high-level Pliocene terrace of the Mississippi River. The Upland Complex is of great interest economically, as it is the primary source of sand and gravel for Memphis, Tennessee and the surrounding region. The pit dimensions were approximately 820 ft (250 m) by 655 ft (200 m) and 79-ft (24 m) deep upon completion of the mining. Eight 3-D models of the pit were made at different times to illustrate the mining progression. Oblique and horizontal stereo aerial photography of the highwalls was conducted to produce 3-D models and high-resolution photomosaics of the highwalls for geologic mapping and interpretation. The mapped highwall geology included Pliocene Mississippi River bars consisting of sand, sand and gravel, and gravel ranging in thickness from 2 ft (0.6 m) to 32.8 ft (10 m), with variable cross-bed dip directions suggesting a meandering river environment of deposition. Pleistocene loess overlies the Pliocene sediment. The highwalls also revealed northerly-striking late Pliocene or Pleistocene tectonic folding, faulting, and probable earthquake liquefaction in northwestern Mississippi, where no Pliocene or Quaternary tectonic deformation had previously been reported. This study demonstrated Drone aerial photography as a quick, low cost, and safe means to study poorly accessible open-pit mining and to help understand the geology of the lower Mississippi River Valley.

Highlights

  • The central United States is host to one of the largest drainage basins in the world, the MississippiRiver

  • This study focused on a sand and gravel quarry in DeSoto County, Mississippi

  • We do not present the mapping history of the pit but focus on the highwall geology revealed in the drone photography

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Summary

Introduction

The Mississippi River has depths of up to 100 ft (30.5 m) and is 2350 miles (3,781 km) long. The river, has a long and complex history [1,2,3], with some profound changes occurring during the Pliocene and Pleistocene [4,5,6,7,8,9]. Geologists have mapped the UC and use this information to better understand the Pliocene Mississippi River [7,8,9]. Sand and gravel companies are interested in understanding the distribution and thickness of this deposit because it is the major commercial source of sand and gravel along the lower Mississippi River [11]

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