Development of the Profile of Equilibrium of Subaqueous Shore Terrace
Development of the Profile of Equilibrium of Subaqueous Shore Terrace
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It is understood in all cases that the surface effect will lag a little behind the cause below, and therefore appear a little to shoreward.
PROFILES RESULTING FROM FORCES DISCUSSED ABOVE.
In the actual operation of the forces discussed above, the resulting action on a sloping bottom may be outward at all places, or inward at all places, or outward over one part and inward over another. Forces in either direction may be gradu- ually augmented or diminished. The different forces are capable of di...fferent combinations. Each set of conditions will lead to certain features of profile, if there be no change of condition, a permanent profile of equilibrium may be reached. The con« stant supply of load constitutes an ever shifting condition. Equilibrium as commonly realized depends on the uniformity of this supply.
Factors in profile -making. — The agencies which shape the marginal bottom may be treated in three groups, ( i ) oscil- latory wave action and undertow, carrying material from shore ; (2) on-shore currents and translatory wave action, carrying the material toward the shore ; (3) currents alongshore.
What to read after Development of the Profile of Equilibrium of Subaqueous Shore Terrace?
You can find similar books in the "Read Also" column, or choose other free books by N M Nevin Melancthon 1865 1945 Fenneman to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
It is understood in all cases that the surface effect will lag a little behind the cause below, and therefore appear a little to shoreward.
PROFILES RESULTING FROM FORCES DISCUSSED ABOVE.
In the actual operation of the forces discussed above, the resulting action on a sloping bottom may be outward at all places, or inward at all places, or outward over one part and inward over another. Forces in either direction may be gradu- ually augmented or diminished. The different forces are capable of di...fferent combinations. Each set of conditions will lead to certain features of profile, if there be no change of condition, a permanent profile of equilibrium may be reached. The con« stant supply of load constitutes an ever shifting condition. Equilibrium as commonly realized depends on the uniformity of this supply.
Factors in profile -making. — The agencies which shape the marginal bottom may be treated in three groups, ( i ) oscil- latory wave action and undertow, carrying material from shore ; (2) on-shore currents and translatory wave action, carrying the material toward the shore ; (3) currents alongshore.
What to read after Development of the Profile of Equilibrium of Subaqueous Shore Terrace?
You can find similar books in the "Read Also" column, or choose other free books by N M Nevin Melancthon 1865 1945 Fenneman to read onlineMoreLess
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