SOUTH Judith River Eagle Warm Mowry Shak Kooter Thermope Jurassic Ellis Seyenite Porphry Metamorphic Rocks Gravity-Slide Faults Bearpaw Shale 3 Mississippian Mission Canyph Devonian Jefferson Limestone an Platheadbandstor Bakken/3 Forks Shale NORTH Ordovician Bighorn Dolomite Little Rocky Mountains No Scale - Drawing is approximate length of Reservation Hogeland Basin Creating a cross-section requires some subjective decisions on your part, but it needs to be geologically reasonable. For example, the thickness and dip of a planar layer should remain relatively constant unless the map data requires otherwise. Planar layers should also be laterally continuous unless there is evidence otherwise. Similarly, keep the structure as simple as you can. Steps to producing a cross section: I. Choose the location and direction of the profile on the geological map (usually a straight line) II. Draw or plot the topography of the profile on the cross-section III. Add the geological features from the map onto the topography, e.g. contacts and faults IV. V. For planar layers and surfaces, use the approximate dip to start projecting these features into depth Fill in the rest of the cross-section as necessary and the different units Elevation A 86 Mt Tomah Richmond Mona Vale Distance

Fundamentals of Geotechnical Engineering (MindTap Course List)

5th Edition

ISBN:9781305635180

Author:Braja M. Das, Nagaratnam Sivakugan

Publisher:Braja M. Das, Nagaratnam Sivakugan

Chapter3: Weight-volume Relationships And Plasticity

Section: Chapter Questions

Problem 3.14P

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Please don't explain it. But draw it out for me kindly. And appreciate your time!. All the info is in the images. Thanks!.

Transcribed Image Text:SOUTH Judith River Eagle Warm Mowry Shak Kooter Thermope Jurassic Ellis Seyenite Porphry Metamorphic Rocks Gravity-Slide Faults Bearpaw Shale 3 Mississippian Mission Canyph Devonian Jefferson Limestone an Platheadbandstor Bakken/3 Forks Shale NORTH Ordovician Bighorn Dolomite Little Rocky Mountains No Scale - Drawing is approximate length of Reservation Hogeland Basin Creating a cross-section requires some subjective decisions on your part, but it needs to be geologically reasonable. For example, the thickness and dip of a planar layer should remain relatively constant unless the map data requires otherwise. Planar layers should also be laterally continuous unless there is evidence otherwise. Similarly, keep the structure as simple as you can. Steps to producing a cross section: I. Choose the location and direction of the profile on the geological map (usually a straight line) II. Draw or plot the topography of the profile on the cross-section III. Add the geological features from the map onto the topography, e.g. contacts and faults IV. V. For planar layers and surfaces, use the approximate dip to start projecting these features into depth Fill in the rest of the cross-section as necessary and the different units