Earthquake Details
| Magnitude |
8.1 |
| Date-Time |
Saturday, January 13, 2007 at 04:23:20 (UTC)
= Coordinated Universal Time
Saturday, January 13, 2007 at 2:23:20 PM
= local time at epicenter |
| Location |
46.272°N, 154.455°E |
| Depth |
10 km (6.2 miles) |
| Region |
EAST OF THE KURIL ISLANDS |
| Distances |
510 km (315 miles) SSW of Severo-Kuril'sk, Kuril Islands, Russia
530 km (330 miles) ENE of Kuril'sk, Kuril Islands
1710 km (1060 miles) NE of TOKYO, Japan
7275 km (4520 miles) NE of MOSCOW, Russia
|
| Location Uncertainty |
horizontal +/- 4.7 km (2.9 miles); depth fixed by location program |
| Source |
USGS NEIC (WDCS-D) |
The following is a release by the United States Geological Survey, National Earthquake Information Center: A major earthquake occurred about 525 km (325 miles) ENE of Kuril'sk, Kuril Islands or about 1710 km (1060 miles) NE of TOKYO, Japan at 10:23 PM MDT, Jan 12, 2007 (Jan 13 at 2:23 PM local time in Russia).
The magnitude and location may be revised when additional data and further analysis results are available. Earthquakes of this type sometimes cause tsunamis, however the USGS has no information that an actual tsunami has been generated. For information about tsunamis, contact the NOAA Tsunami Warning Centers at http://tsunami.gov.
Tectonic Summary
The Kuril Islands earthquake of January 13, 2007, occurred as normal-faulting in the Pacific plate near the boundary between the Pacific plate and the Okhotsk plate. In the region of the earthquake's epicenter, the Pacific plate moves northwest with respect to the Okhotsk plate with a velocity of about 90 mm/year. The Pacific plate subducts beneath the Okhotsk plate at the Kuril Trench and becomes progressively deeper to the northwest, remaining seismically active to a depth of 680 km. The January 13 earthquake occurred approximately 95 km ESE of an M8.3 earthquake that occurred on November 15, 2006. The November 15 earthquake is the largest earthquake to have occurred in the central Kuril Islands since the early 20th century. A central Kuril Islands earthquake in 1915 is estimated to have had a magnitude of about 8. The central Kuril Islands commonly experiences one or more shocks of magnitude 6 or greater in a decade. To the southwest, the southern Kuril Islands chain experienced a magnitude 8.5 earthquake in 1963. To the northeast, a magnitude 9 earthquake occurred offshore of Kamchatka in 1952.
Tsunami Information

Tsunami travel time map (click to enlarge)
Tide gauge |
Peak amplitude (above sea level in cm) |
Observed Initial Arrival time (UTC) |
Computed Initial Arrival time (UTC) |
Initial motion |
Sample Interval (min) |
|
|
|
|
|
|
Adak, Alaska |
5 |
0738 |
0735 |
fall |
1 |
| Dutch Harbor, Alaska |
6 |
0846 |
0844 |
|
1 |
Shemya, Alaska |
32 |
0642 |
0636 |
fall |
.25 |
Sitka, Alaska |
8 |
|
1049 |
|
1 |
Yakutat, Alaska |
5 |
|
1049 |
|
1 |
Pago Pago, Amer. Samoa |
11 |
|
1337 |
|
6 |
Arena Cove, California |
25 |
1250 |
1250 |
fall |
1 |
Crescent City, California |
23 |
|
1247 |
|
1 |
Point Reyes, California |
12 |
|
1303 |
|
1 |
Port San Luis, California |
11 |
1331 |
1322 |
fall |
1 |
San Francisco, California |
5 |
|
1333 |
|
1 |
Santa Barbara, California |
10 |
|
1438 |
|
1 |
Antofagasta, Chile |
10 |
|
0028 1/14 |
|
2 |
Iquique, Chile |
9 |
0048 1/14 |
0007 1/14 |
fall |
2 |
Talcahuano, Chile |
8 |
|
0141 1/14 |
|
2 |
Rarotonga, Cook Is |
8 |
|
1507 |
|
6 |
Hilo, Hawaii |
11 |
|
1112 |
|
1 |
Honolulu, Hawaii |
6 |
|
1047 |
|
1 |
Kahului Maui, Hawaii |
17 |
1108 |
1104 |
rise |
1 |
Nawiliwili Kauai, Hawaii |
10 |
1020 |
1032 |
fall |
1 |
Hanasaki, Japan |
13 |
0536 |
0541 |
fall |
1 |
Ofunato, Japan |
22 |
|
0613 |
|
1 |
Kwajalein, Marshall Is. |
11 |
|
0947 |
|
1 |
Midway Island |
19 |
0820 |
0821 |
rise |
1 |
Charleston, Oregon |
9 |
|
1242 |
|
1 |
Callao-La Punta, Peru |
14 |
|
2306 |
|
2 |
Wake Island |
8 |
0817 |
0813 |
rise |
1 |
DISCUSSION
The Kuril Islands earthquake of 15 November 2006, occurred as thrust-faulting on the boundary between the Pacific plate and the Okhotsk plate. The M8.1 earthquake on 13 January 2006 occurred as normal-faulting approximately 95 km ESE of the November earthquake within the outer-rise portion of the Pacific plate. In the region of these earthquake epicenters, the Pacific plate moves northwest with respect to the Okhotsk plate with a velocity of about 90 mm/year. The Pacific plate subducts beneath the Okhotsk plate at the Kuril-Kamchatka Trench and becomes progressively deeper to the northwest, remaining seismically active to a depth of about 680 km. The 15 November earthquake is the largest earthquake to have occurred in the central Kuril Islands since the early 20th century. A central Kuril Islands earthquake in 1915 is estimated to have had a magnitude of about 8. The central Kuril Islands commonly experiences one or more shocks of magnitude 6 or greater in a decade. To the southwest, the southern Kuril Islands chain experienced a magnitude 8.5 earthquake in 1963. To the northeast, a magnitude 9 earthquake occurred offshore of Kamchatka in 1952.
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