The Strength of the Earths Crust
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Ii -3. 56 -1. 42 -0-55 O. 121 +m f O -5-09 2. 2O O. 4O -0. 03 0. 003 Fv 1 I -m r -17. 78 -7. 12 -2. 48 0. 61 o. Ii . 0. 015 +HI / 14. 22 -4. 08 O. 4O +0. 15- +0. 05 +0. 007 The data in this table are represented by the curves of Fig. 7. It shows that for this arrangement of masses the influence on the surface falls off rapidly at a horizontal distance between 0. 25 and 0. 75, which are also the vertical depths to I and III. When the masses are of opposite sign the anomaly passes through zero at... a horizontal distance of about 0. 6, and the deflection force for opposite sign decreases to half the value of the sum at about o. 75. The ratio between the effects of like and unlike masses becomes more marked the greater the distance of the point, although the actual magnitudes of the forces decrease.
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232 JOSEPH BARRELL Now assume the unit masses at I and III to be parts of masses of like density extending to the left of o to a distance N. Consider the aggregate effect upon a given point, as that at 0.
What to read after The Strength of the Earths Crust?
You can find similar books in the "Read Also" column, or choose other free books by Joseph Farrell to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Ii -3. 56 -1. 42 -0-55 O. 121 +m f O -5-09 2. 2O O. 4O -0. 03 0. 003 Fv 1 I -m r -17. 78 -7. 12 -2. 48 0. 61 o. Ii . 0. 015 +HI / 14. 22 -4. 08 O. 4O +0. 15- +0. 05 +0. 007 The data in this table are represented by the curves of Fig. 7. It shows that for this arrangement of masses the influence on the surface falls off rapidly at a horizontal distance between 0. 25 and 0. 75, which are also the vertical depths to I and III. When the masses are of opposite sign the anomaly passes through zero at... a horizontal distance of about 0. 6, and the deflection force for opposite sign decreases to half the value of the sum at about o. 75. The ratio between the effects of like and unlike masses becomes more marked the greater the distance of the point, although the actual magnitudes of the forces decrease.
.
232 JOSEPH BARRELL Now assume the unit masses at I and III to be parts of masses of like density extending to the left of o to a distance N. Consider the aggregate effect upon a given point, as that at 0.
What to read after The Strength of the Earths Crust?
You can find similar books in the "Read Also" column, or choose other free books by Joseph Farrell to read onlineMoreLess
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