Definition of Coseismals

1. coseismal [n] - See also: coseismal

Lexicographical Neighbors of Coseismals

cosecants
cosech
cosechs
cosecs
cosed
cosediment
cosedimented
cosedimenting
cosediments
cosegregate
cosegregated
cosegregates
cosegregating
cosegregation
coseismal
coseismals (current term)
coseismic
coseismics
coself
cosenage
cosenages
cosentient
coses
coset
cosets
cosey
coseys
cosh
cosh pocket
coshed

Literary usage of Coseismals

Below you will find example usage of this term as found in modern and/or classical literature:

1. Earthquakes in the Light of the New Seismology by Clarence Edward Dutton (1904)
"... Area—coseismals—General Notion of an Earthquake Vibration—The Spherical Shell—A Case of Radiant Energy—General Statement of the Cause of an Earthquake, ..."

2. The Hereford Earthquake of December 17, 1896 by Charles Davison (1899)
"The average distance between the second and third coseismals for these directions is ... The mean surface-velocity between the first two coseismals is, ..."

3. ... The Hereford Earthquake of December 17, 1896: Considered in Relation to by Edward Greenly (1899)
"The average distance between the second and third coseismals for these directions is 35J ... The mean surface-velocity between the first two coseismals is, ..."

4. Report of the Annual Meeting (1895)
"18, in which coseismals have been drawn, on the assumption that the velocity has increased proportionately with the depth. In this case the earthquake rays ..."

5. A Study of Recent Earthquakes by Charles Davison (1905)
"Now, the average distance between the two inner coseismals is 32! miles, between the two outer ones (so far as drawn) 35^ miles, and between the first and ..."

6. A Study of Recent Earthquakes by Charles Davison (1905)
"Now, the average distance between the two inner coseismals is 32^ miles, between the two outer ones (so far as drawn) 35^ miles, and between the first and ..."

7. Seismology by John Milne (1908)
"32, in which coseismals have been drawn on the assumption that FIG. 32. the velocity has increased proportionately with tho depth. ..."

8. College Physiography by Ralph Stockman Tarr, Lawrence Martin (1914)
"A series of lines connecting places at which the shaking appears at the same time are called coseismals, and lines passing through places of equal intensity ..."

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