Geologic maps and cross sections showing configurations of bedrock surfaces, Broken Bow 1 degree by 2 degrees Quadrangle, east-central Nebraska

10.3133/i2725 ◽  
2000 ◽  
Geosphere ◽  
2020 ◽  
Vol 16 (6) ◽  
pp. 1495-1507
Author(s):  
Richard W. Allmendinger

Abstract GMDE is a program, available on the desktop for Apple Macintosh, Microsoft Windows, and Linux platforms and in a mobile version for iOS, that enables geologists to extract quantitative structural information from geologic maps and satellite images. The program facilitates the digitizing of strikes and dips or calculating them from three-point problems, calculation of stratigraphic map thickness, determination of piercing points on faults, and the construction of down-plunge projections and vertical cross sections with projected apparent dips, contacts, and cylindrical folds. The program also enables the automatic plotting of planar contacts across topography based on orientation calculated from three clicked points, which can be carried out in the field for immediate hypothesis testing. Error propagation is built into many of the calculations. Maps and satellite images require no projection or datum information, just four points with known latitude and longitude information. Alternatively, the user can enter the map or image in MBTiles format. Users can easily extract X-Y-Z data for any clicked or calculated point or polygon, enabling them to make their own calculations.


Author(s):  
Robert C. Speed ◽  
Hai Cheng

ABSTRACT This chapter presents geological documentation of Quaternary (and perhaps older) event histories of southeastern Barbados. The Barbados Limestone is herein formally defined. A time-stratigraphic division of the Barbados Limestone in southeastern Barbados and the properties of the stratigraphic units are presented. A major finding of this study is that the marine terraces originated wholly by marine erosion, not by reef construction, and evolved in stages over a long duration. The hydrology and thickness data of the Barbados Limestone are discussed, and hypotheses on causes of thickness variations are given. The study domain is divided into seven areas that contain a continuous flight of nine marine terraces preserved in various partial sequences. Discussions of these key seven areas in southeastern Barbados are supported by geologic maps at large scale and cross sections. Sections with VE > 1 display limestone stratigraphy and facies over relatively large lengths. Sections with VE = 1 show true structural configurations over short lengths. Detailed observations and radioisotopic dating of the limestone units permit differentiation and correlation among them.


2021 ◽  
Author(s):  
N.R. Blackford ◽  
et al.

<div>Figure 7. Compilation of cross sections across east-central Nevada and western Utah (1:200,000 scale) with deformed cross sections in the top row (A) and restored cross sections in the bottom row (B). Translucent areas represent eroded rock above the modern surface (deformed cross sections) and above the Paleogene unconformity (restored cross sections).<br></div><div><br></div><div><br></div><div><br></div><div><br></div>


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