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MamaJ
reply to post by ericblair4891
Dang! How often does that area have quakes? Lawd... I am off to search for more answers. Thanks for the link.
Is it just me or does anyone notice fracking quakes come in at depths of 5? Its me isnt it? loledit on 16-12-2013 by MamaJ because: (no reason given)
MamaJ
reply to post by radpetey
Thank you for that. Yeah not many and the depth is minimal as well. HMMMM?
Fracking quake perhaps? Hopefully nothing bigger comes our way. Im in TN so anything much bigger could possibly be felt here.
On April 24, 1867, the 1867 Manhattan earthquake struck Riley County, Kansas. Measuring 5.1 on the Richter scale, the earthquake's epicenter was by the town of Manhattan, to this day, the strongest earthquake to originate in the state.
The earthquake had an intensity of VII on the Mercalli intensity scale, and was felt over an area of roughly 193,051 square miles (500,000 km2). It caused largely minor damage, reports of which were confined to Kansas, Iowa, and Missouri, according to the United States Geological Survey.
Manhattan is near the Nemaha Ridge, a long structure that is bounded by several faults. The nearby Humboldt Fault Zone in particular poses a threat to the city; though Kansas is not known for earthquake activity, an earthquake could occur at any time.
en.wikipedia.org...
Despite the fact that Kansas is not seismically active, a strong earthquake could pose significant threats to the state. If an earthquake were to occur, it would likely be along the Nemaha Ridge, which is still active.[8] The Humboldt Fault Zone, a fault just off the Ridge, lies just 12 miles (19 km) eastward of the Tuttle Creek Reservoir near Manhattan. If an earthquake were to occur here, it would likely destroy the dam, releasing 300,000 feet (91,440 m) of water per second and flooding the nearby area, also threatening roughly 13,000 people and 5,900 homes. A moderate earthquake "between 5.7 to 6.6 would cause sand underneath the dam to liquefy into quicksand, causing the dam to spread out and the top to drop up to three feet."[2] A large earthquake would spawn gaps, forcing water to leak and eventually cause the dam to collapse. Any earthquake that could pose a threat occurs on a cycle of roughly 1,800 years, according to the United States Army Corps of Engineers, who studied the area first in 1980.[2]
To counter this threat, the group has galvanized an effort to strengthen the dam. Replacing the sand, which could shift during an earthquake, with more than 350 walls, the group has equipped the dam with sensors. Alarms are connected to these sensors, which would alert nearby citizens to the earthquake.[2]
Public ID 2013p944608
Universal Time December 16 2013 at 12:07:26
NZ Daylight Time Tuesday, December 17 2013 at 1:07:26 am
Latitude, Longitude -46.28, 166.04
Intensity ? severe
Focal Depth 25 km
Magnitude 6.2 ML
Location offshore 125 km west of Tuatapere (Puysegur Bank)
www.geonet.org.nz...
M4.2 - 18km WNW of Caldwell, Kansas
2013-12-16 15:09:53 UTC
Event Time
2013-12-16 15:09:53 UTC
2013-12-16 09:09:53 UTC-06:00 at epicenter
2013-12-16 09:09:53 UTC-06:00 system time
Location
37.124°N 97.781°W depth=5.0km (3.1mi)
Nearby Cities
18km (11mi) WNW of Caldwell, Kansas
61km (38mi) SW of Haysville, Kansas
65km (40mi) SW of Derby, Kansas
66km (41mi) W of Arkansas City, Kansas
185km (115mi) N of Oklahoma City, Oklahoma
BO XIAN
reply to post by muzzy
THX THX.
And if one doesn't buy into the subduction theory . . . what is the explanation?
NZ sure has . . . interesting . . . geology.
LOL.
I assume you keep your seat belt buckled!
If its not subduction then there is a big crack between the plates at a 45 degree angle going down from west to east.