The hardness of a mineral on the Mohs scale. Introduction: Mohs Scale is used to determine the numerical value of hardness of any mineral. The Mohs scale consists of 10 minerals arranged in order from softest to hardest.

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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…

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Chapter 1, Problem 9LR

Summary Introduction

The hardness of a mineral on the Mohs scale.

Introduction:

Mohs Scale is used to determine the numerical value of hardness of any mineral. The Mohs scale consists of 10 minerals arranged in order from softest to hardest.

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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…

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