Individual Event Report
| Event #627 - Summary, and parameter estimates with source IDs |
| It seems that this location is likely to be in error. Milne cites the ISS as the source for this earthquake but says: "There are no reports to indicate that the tremor was felt, although the epicentre fell in a populated area." |
| TIME |
LOCATION |
MAGNITUDE |
MAX. INTENSITY |
FELT AREA |
| YR |
MO |
DAY |
HR |
MIN |
AM/PM |
Time
Type |
LAT(N) |
LON(W) |
DEP
(km) |
MAG |
Mag
Type |
Felt
Plc. |
Felt
St. |
Inten-
sity |
Int.
Type |
Felt
Area |
Felt
Area
Int. |
Felt
Area
Units |
| 1926 |
9 |
17 |
|
|
|
|
49.00 |
124.00 |
|
5.50 |
IML |
|
|
|
|
|
|
|
| MILNE - 1496 |
MILNE - 1496 |
- |
WWC - 1882 |
- |
- |
Underlying Source Material
| Source ID |
Publication |
Pub Date |
Pub Details |
| 1496 |
Milne, W.G., 1956, Seismic Activity in Canada, west of the 113th meridian 1841-1951: Canada Dominion Obs. Pub., V. 18, No. 7, pp. 119-146 |
1957 |
|
| Transcription: 1926 SEPTEMBER 17. phi = 49.0 degrees N; lambda = 124 degrees W. ISS. There are no reports to indicate that the tremor was felt, although the epicentre fell in a populated area. |
| |
| Source ID |
Publication |
Pub Date |
Pub Details |
| 1882 |
Woodward Clyde Consultants, unpublished |
1981 |
Woodward-Clyde Consultants (1981), Historical Catalog (1841-1980) for the Pacific Northwest Region, unpublished catalog prepared for the Washington Public Power Supply System. Copy provided to UW in 1993. |
| Transcription: 192609172214400 50000-123000 550ML CA 01 |
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