There is a method to distinguish granite (G) or basaltic (B) rocks in the soil, the method consists of examining a portion of the soil by means of the infrared spectrum that the rocks reflect on the soil surface. Let R1, R2 and R3 be intensity levels at different wavelengths of the infrared spectrum. Generally for granite the intensities are presented in the order R1 < R2 < R3, while for basalt they are presented in the order R3 < R1 < R2. When measurements are made remotely (aerially), different orders of the Ris can be presented, whether they are basalt or granite rocks. Several measurements on a region whose soil composition is known have yielded the following information.
There is a method to distinguish granite (G) or basaltic (B) rocks in the soil, the method consists of examining a portion of the soil by means of the infrared spectrum that the rocks reflect on the soil surface. Let R1, R2 and R3 be intensity levels at different wavelengths of the infrared spectrum. Generally for granite the intensities are presented in the order R1 < R2 < R3, while for basalt they are presented in the order R3 < R1 < R2. When measurements are made remotely (aerially), different orders of the Ris can be presented, whether they are basalt or granite rocks. Several measurements on a region whose soil composition is known have yielded the following information.
A First Course in Probability (10th Edition)
10th Edition
ISBN:9780134753119
Author:Sheldon Ross
Publisher:Sheldon Ross
Chapter1: Combinatorial Analysis
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The event G denotes that the rock is Granite and the event B denotes that the rock is Basaltic. It is given that
Also, there are three order of intensities given. The likelihood probabilities are:
Order | Granite | Basalt |
R1<R2<R3 | 0.6 | 0.1 |
R1<R3<R2 | 0.25 | 0.2 |
R3<R1<R2 | 0.15 | 0.7 |
In this table, the probabilities of the three order of intensities given that the rock was G or B are shown.
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