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The section runs north-south from Victoria on Vancouver Island to southern Washington state. Scientists call it a transient slip zone because the fault between two plates slips gradually every 14 months or so. This gradual slip takes place over a two-week period and triggers tremors that are so small people don’t notice them.
In this study the slowly slipping section of the fault beneath Washington state was found to be 27 to 42 kilometres deep instead of 25 to 35. Using sound from compressed air sources in the ocean and small nearby earthquakes, Calvert and his colleagues determined how long it took seismic waves to propagate through the Earth. This told them there is a lot of sedimentary rock in the fault beneath Washington state.
So we have a 3.7 quake (moderate size) right where the subduction zone is and at that depth, it's a bit more concerning. Add to it the micro quakes occuring nearby at a more shallow depth, may (and I stress may) indicate the stress and dynamics going on bellow. I am NOT a geologist. I am just an avid quake watcher. I have watched my area for nearly 15 years now so I know what is unusual. ....
MAP 3.7 2011/07/24 12:19:28 47.708 -123.178 42.3 20 km ( 12 mi) WNW of Brinnon, WA
Experts say a future megathrust earthquake, measuring 9.0 on the Richter scale, will occur somewhere off the coasts of B.C., Washington state and California. That is where the Juan de Fuca and North America plates are locked and are known to slip every 500 to 600 years. The last such earthquake was in 1700.
MAP 1.0 2011/08/05 18:48:49 38.823 -122.799 3.3 3 km ( 2 mi) NNE of The Geysers, CA
MAP 2.6 2011/08/05 17:59:02 42.616 -122.398 16.5 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 2.4 2011/08/05 17:34:37 42.629 -122.389 2.0 18 km ( 11 mi) ENE of Butte Falls, OR
MAP 2.0 2011/08/05 16:22:52 39.672 -121.893 5.0 9 km ( 6 mi) WNW of Durham, CA
MAP 4.5 2011/08/05 15:10:07 44.144 -128.762 37.2 368 km (229 mi) WNW of Bandon, OR
MAP 1.2 2011/08/05 13:16:06 38.810 -122.811 0.0 1 km ( 1 mi) NNW of The Geysers, CA
MAP 1.5 2011/08/05 12:15:19 38.819 -122.795 3.5 3 km ( 2 mi) NNE of The Geysers, CA
MAP 1.2 2011/08/05 11:27:28 38.800 -122.818 3.2 1 km ( 1 mi) W of The Geysers, CA
MAP 1.4 2011/08/05 10:29:07 38.835 -122.788 2.5 4 km ( 3 mi) NNE of The Geysers, CA
MAP 1.3 2011/08/05 09:36:03 38.800 -122.817 3.3 1 km ( 1 mi) WNW of The Geysers, CA
MAP 1.2 2011/08/05 09:31:43 38.799 -122.816 3.4 1 km ( 0 mi) W of The Geysers, CA
MAP 2.7 2011/08/05 08:56:17 38.800 -122.814 3.1 1 km ( 0 mi) WNW of The Geysers, CA
MAP 2.0 2011/08/05 05:49:47 38.825 -122.799 3.3 3 km ( 2 mi) NNE of The Geysers, CA
MAP 1.7 2011/08/05 05:00:11 38.813 -122.793 3.6 2 km ( 1 mi) NE of The Geysers, CA
MAP 1.9 2011/08/05 04:35:38 42.613 -122.393 14.1 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 1.9 2011/08/05 01:45:48 38.814 -122.835 3.4 3 km ( 2 mi) NW of The Geysers, CA
MAP 3.6 2011/08/05 01:18:42 40.387 -125.037 8.8 64 km ( 40 mi) W of Petrolia, CA
MAP 2.1 2011/08/04 20:01:13 45.063 -122.629 18.3 4 km ( 2 mi) NE of Scotts Mills, OR
MAP 1.7 2011/08/04 18:56:50 46.202 -123.136 10.5 12 km ( 7 mi) WNW of West Longview, WA
MAP 1.5 2011/08/04 18:53:23 38.802 -122.776 4.2 3 km ( 2 mi) E of The Geysers, CA
MAP 2.5 2011/08/04 18:38:20 42.618 -122.405 13.1 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 2.6 2011/08/05 17:59:02 42.616 -122.398 16.5 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 2.4 2011/08/05 17:34:37 42.629 -122.389 2.0 18 km ( 11 mi) ENE of Butte Falls, OR
MAP 4.5 2011/08/05 15:10:07 44.144 -128.762 37.2 368 km (229 mi) WNW of Bandon, OR
MAP 1.9 2011/08/05 04:35:38 42.613 -122.393 14.1 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 1.3 2011/08/05 02:00:31 47.590 -122.490 60.0 6 km ( 4 mi) NE of Manchester, WA
MAP 2.1 2011/08/04 20:01:13 45.063 -122.629 18.3 4 km ( 2 mi) NE of Scotts Mills, OR
MAP 1.7 2011/08/04 18:56:50 46.202 -123.136 10.5 12 km ( 7 mi) WNW of West Longview, WA
MAP 2.5 2011/08/04 18:38:20 42.618 -122.405 13.1 16 km ( 10 mi) ENE of Butte Falls, OR
MAP 2.2 2011/08/04 17:22:31 42.624 -122.396 3.4 17 km ( 10 mi) ENE of Butte Falls, OR
MAP 1.7 2011/08/04 09:15:18 42.640 -122.396 4.3 18 km ( 11 mi) NE of Butte Falls, OR
MAP 1.6 2011/08/04 03:20:20 45.035 -122.578 17.3 7 km ( 4 mi) E of Scotts Mills, OR
MAP 2.2 2011/08/03 23:15:48 45.047 -122.585 20.3 7 km ( 4 mi) E of Scotts Mills, OR
MAP 1.1 2011/08/03 18:29:56 44.508 -123.285 18.2 7 km ( 4 mi) S of Corvallis, OR
MAP 1.6 2011/08/03 16:52:22 44.089 -122.600 11.0 24 km ( 15 mi) NE of Lowell, OR
MAP 1.7 2011/08/03 10:10:19 47.703 -122.082 7.9 4 km ( 2 mi) NW of Union Hill-Novelty Hill, WA
MAP 1.3 2011/08/03 09:34:28 48.584 -121.335 12.3 9 km ( 6 mi) NE of Marblemount, WA
MAP 1.3 2011/08/03 09:01:32 48.397 -124.631 33.2 4 km ( 2 mi) NNW of Neah Bay, WA
MAP 2.1 2011/08/03 08:14:49 45.267 -122.963 12.9 4 km ( 2 mi) ESE of Dundee, OR
MAP 1.2 2011/08/03 03:28:40 47.584 -121.672 12.6 13 km ( 8 mi) NNE of Tanner, WA
Recent Earthquakes near Crater Lake
08/04/26 06:01:35 42.90N 122.16W 18.5 2.0 CC
08/07/23 22:51:09 42.61N 122.40W 14.1 1.9 CC
08/07/23 22:54:12 42.61N 122.40W 13.4 1.9 CC
08/07/23 23:19:26 42.59N 122.40W 4.3 1.6 BD
08/07/24 01:36:54 42.61N 122.41W 18.7 1.6 CC
08/09/03 04:32:08 42.55N 122.44W 8.5 1.2 AC
10/09/30 05:05:02 42.63N 122.40W 11.1 1.6 BC
10/09/30 05:11:12 42.61N 122.40W 12.0 1.6 CC
11/08/04 09:15:18 42.64N 122.39W 4.4 1.7 CD
11/08/04 17:22:31 42.62N 122.39W 3.5 2.2 CC
11/08/04 18:38:20 42.62N 122.40W 4.0 2.5 BC
11/08/05 04:35:38 42.61N 122.39W 14.1 1.9 BC
11/08/05 17:34:37 42.62N 122.38W 2.0 2.4 CC
11/08/05 17:59:02 42.61N 122.39W 16.5 2.6 CC
11/08/05 20:04:13 42.62N 122.40W 10.8 2.3 BC
11/08/05 23:39:57 42.62N 122.40W 14.0 2.5 BC
11/08/05 23:41:34 42.60N 122.40W 13.8 2.0 CC
11/08/05 23:59:50 42.59N 122.42W 17.5 1.7 BC
11/08/06 00:05:20 42.61N 122.40W 8.9 2.8 CC
11/08/06 00:44:01 42.62N 122.40W 15.1 2.3 CC
A well-known crater lake, which bears the same name as the geological feature, is Crater Lake in Oregon, USA. It is located in the caldera of Mount Mazama, hence the name "Crater Lake" is something of a misnomer. It is the deepest lake in the United States with a depth of 594 m (1,949 ft). Crater Lake is fed solely by falling rain and snow, with no inflow or outflow at the surface, and hence is one of the clearest lakes in the world.[1]
Mount Mazama and Crater Lake caldera lie at the intersection of the Cascade chain of volcanoes with the Klamath graben, a north-northwest trending basin bounded by faults whose displacement is mainly vertical. At this latitude, the western margin of the Basin and Range province, characterized by north-south to northwest-southeast trending faults, impinges upon the Cascades. Focusing of volcanism at Crater Lake and the development of the shallow magma chamber which fed the climactic eruption are linked to this regional tectonic situation.
North and south of Crater Lake are many shield volcanoes of modest size and many more cinder cones with associated lava flow fields. Both represent short-lived activity at isolated vents. These monogenetic volcanoes are manifestations of regional volcanism throughout the Oregon Cascades.
Remarks: Largest known eruption from Cascade Range volcano. Catastrophic, caldera-forming eruption 7,000 years ago; post-caldera lava and domes 2 ... From a probable altitude of roughly 12,000 feet, the top of former Mount Mazama was lost to eruption and collapse that left the present huge crater and the deepest lake (1,932 feet) in North America. Explosive eruptions built Wizard Island and two other cones (submerged) on present crater floor 3.
NEWPORT, OR (KPTV) - Oregon State University scientists say they've discovered an eruption of an undersea volcano about 250 miles off the Oregon Coast.
The April 6 eruption produced a lava flow at least 1.2 miles wide, scientists say, and there were hundreds of tiny earthquakes during the eruption.
The volcano, named Axial Seamount, last erupted in 1998, and the team of OSU scientists forecasted it would erupt again before 2014. Oregon State scientists say this marks the first-ever successful forecast of an undersea volcano.
The new eruption was discovered July 28 when scientists used a robot to find a new lava flow on the seafloor that was not present a year ago. Because only a handful of the earthquakes were detected from land, scientists did not initially believe there was an eruption.
"The acid test in science - whether or not you understand a process in nature - is to try to predict what will happen based on your observations," he says.
Newberry volcano is a broad shield volcano located in central Oregon. It has been built by thousands of eruptions, beginning about 600,000 years ago. At least 25 vents on the flanks and summit have been active during several eruptive episodes of the past 10,000 years. The most recent eruption 1,300 years ago produced the Big Obsidian Flow. Thus, the volcano's long history and recent activity indicate that Newberry will erupt in the future.
Crater Lake was formed after the collapse of an ancient volcano, posthumously named Mount Mazama. This volcano violently erupted approximately 7700 years ago. That eruption was 42 times as powerful as the 1980 eruption of Mount St. Helens. The basin or caldera was formed after the top 5000 feet of the volcano collapsed. Subsequent lava flows sealed the bottom, allowing the caldera to fill with approximately 4.6 trillion gallons of water from rainfall and snow melt, to create the seventh deepest lake in the world at 1,932 feet. -- Excerpt from: U.S. National Park Service Website: Crater Lake National Park, 1999
Long Valley Caldera is located 20 km south of Mono Lake along the east side of the Sierra Nevada in east-central California. This area of eastern California has produced numerous volcanic eruptions over the last 3 million years including the massive, caldera-forming eruption 760,000 years ago. The most recent eruptions occurred just 500 to 600 years ago from vents along the Mono Crater-Inyo crater volcanic chain, which extends south from Mono Lake into the western part of Long Valley caldera
Recent Earthquakes near Crater Lake
08/04/26 06:01:35 42.90N 122.16W 18.5 2.0 CC
08/07/23 22:51:09 42.61N 122.40W 14.1 1.9 CC
08/07/23 22:54:12 42.61N 122.40W 13.4 1.9 CC
08/07/23 23:19:26 42.59N 122.40W 4.3 1.6 BD
08/07/24 01:36:54 42.61N 122.41W 18.7 1.6 CC
08/09/03 04:32:08 42.55N 122.44W 8.5 1.2 AC
10/09/30 05:05:02 42.63N 122.40W 11.1 1.6 BC
10/09/30 05:11:12 42.61N 122.40W 12.0 1.6 CC
11/08/04 09:15:18 42.64N 122.39W 4.4 1.7 CD
11/08/04 17:22:31 42.62N 122.39W 3.5 2.2 CC
11/08/04 18:38:20 42.62N 122.40W 4.0 2.5 BC
11/08/05 04:35:38 42.61N 122.39W 14.1 1.9 BC
11/08/05 17:34:37 42.62N 122.38W 2.0 2.4 CC
11/08/05 17:59:02 42.61N 122.39W 16.5 2.6 CC
11/08/05 20:04:13 42.62N 122.40W 10.8 2.3 BC
11/08/05 23:39:57 42.62N 122.40W 14.0 2.5 BC
11/08/05 23:41:34 42.60N 122.40W 13.8 2.0 CC
11/08/05 23:59:50 42.59N 122.42W 17.5 1.7 BC
11/08/06 00:05:20 42.61N 122.40W 8.9 2.8 CC
11/08/06 00:44:01 42.62N 122.40W 15.1 2.3 CC
Magnitude
3.0
Date-Time
Sunday, August 28, 2011 at 03:03:22 UTC
Saturday, August 27, 2011 at 08:03:22 PM at epicenter
Location
36.602°N, 121.203°W
Depth
5.6 km (3.5 miles)
Region
CENTRAL CALIFORNIA
Distances
9 km (6 miles) NW (326°) from Pinnacles, CA
22 km (14 miles) NNE (31°) from Soledad, CA
23 km (14 miles) SSE (153°) from Tres Pinos, CA
32 km (20 miles) SSE (147°) from Hollister, CA
102 km (64 miles) SE (143°) from San Jose City Hall, CA
Location Uncertainty
horizontal +/- 0.1 km (0.1 miles); depth +/- 0.5 km (0.3 miles)
Parameters
Nph= 70, Dmin=7 km, Rmss=0.08 sec, Gp= 32°,
M-type=duration magnitude (Md), Version=1
Source
California Integrated Seismic Net:
USGSCaltechCGSUCBUCSDUNR
Event ID
nc71628800
A cluster of mild earthquakes rumbled early on Saturday near Pinnacles National Monument, site of an ancient volcano in central California, and were widely felt in and around the Monterrey Bay area.
This earthquake occurred on the San Andreas fault, which ruptured from near Parkfield (in the Cholame Valley) almost to Wrightwood (a distance of about 300 kilometers); horizontal displacement of as much as 9 meters was observed on the Carrizo Plain. It caused one fatality. A comparison of this shock to the San Francisco earthquake, which occurred on the San Andreas fault on April 18, 1906, shows that the fault break in 1906 was longer but that the maximum and average displacements in 1857 were larger.
Instances of seiching, fissuring, sandblows and hydrologic changes were reported from Sacramento to the Colorado River delta. Ground fissures were observed in the beds of the Los Angeles, Santa Ana, and Santa Clara Rivers and at Santa Barbara. Sandblows occurred at Santa Barbara and in the flood plain of the Santa Clara River. One report describes sunken trees, possibly associated with liquefaction, in the area between Stockton and Sacramento.