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Carroll Township and the Earthquake Swarm
Jeri L. Jones, Jones Geological Services
Dr. Charles K. Scharnberger, Professor Emeritus, Millersville University
The title sounds like a fairy tale and to some residents of Carroll
Township, they wished it was. Beginning on Friday, October 3rd and still
continuing at the writing of this articlein mid December, the area has
been “rocked” or “boomed” by numerous tremors. Over 150 tremors have
been felt or heard by area residents. Of the large number of tremors, 18
of these events were recorded by seismic stations at Millersville
University, Frankliln and Marshall College, Soldier’s Delight State
Park, and several other seismograph stations in the region. Several
dates on which recordable tremors were noted were Sunday, October 5th,
Sunday; October 19th; Monday, October 20th; Thursday, October 23rd;
Sunday, October 26th and Thursday, November 6th. The largest of these
tremors had a magnitude of 2.1 on October 19th. The same day also
included 11 other tremors recorded at the above stations.
Much information from area residents was reported to these
investigators. From the township website and television channel,
personal and telephone interviews and constant record keeping of
residents, we have been able to construct intensity maps for the October
5th and October 19th events as well as a listing of all of the tremors
felt. The quadrant between Mandy Lane, Old York Road, Warrington Road
and Stoney Run Road has the highest intensity for these tremors. Along
with the booms and rumbles, during the 2.1 tremor of October 19th, items
fell off of shelves, the feeling that the house floor rose up two feet
and a old window pane cracking were among the responses from residents.
On Friday, October 24th, personnel from Lamont-Doherty Earth Observatory
of Columbia University installed four portable seismographs in the
Dillsburg area. These portable units will record all of the tremors,
many of which are not strong enough to be recorded at the permanent
stations. From data retrieved from these stations, the epicenters and
depths of these tremors can be precisely located. This information is
not expected back to us until late December.
A community meeting was held on October 28th at the township building.
During the meeting, the local geology was explained, history of
earthquakes in the eastern United States and a lengthy question and
answer period eased the minds of some of the area residents. Based on
the history of earthquakes in the eastern section of the United States,
there is a low probability that a severe earthquake will occur in the
Dillsburg area.
What makes this swarm of shallow earthquakes interesting to investigate?
1). The number of tremors felt over the last ten weeks
2). The regular “boom” that accompanies many of these tremors
3). A sulfur smell associated with the larger tremors and sometimes
within the groundwater
These issues are being investigated by us. We hope to schedule another
informational meeting early in 2009 at a meeting place to be announced.
There will be information also placed on the Carroll Township website
and here at this website.
For additional information, check out these websites:
Millersville University Seismic Station:
www.millersville,edu/esci/geology/seismograph.php
Lamott-Doherty Earth Observatory –
www.ldeo.columbia.edu/LCSN
National Earthquake Information Center –
http:earthquake.usgs.gov/regional/neic/
Free downloadable Earthquake Hazards in Pennsylvania booklet
www.dcnr.state.pa.us/topogeo/education/ed.aspx
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To view a larger map, click on the map image. |
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Intensity map of the October 5, 2008 2.0
earthquake. Zone III is the epicenter area |

Intensity map of the October 19, 2008 2.1
earthquake - Zone IV in in the epicenter area and was a more widely
felt event than the October 5th tremor |
Open the PowerPoint to view
what days have had seismic activity.
May take longer to load on dial-up. (file size: 3.5M)
Measurable Earthquakes from the Lamott-Doherty
Cooperative Seismographic Network from the Dillsburg
Pennsylvania area (PDF Available)
| Date |
Local Time |
Magnitude |
| October 5, 2008 |
6:36 |
2.0 |
| |
|
|
| October 19, 2008 |
4:21 |
1.9 |
| October 19, 2008 |
4:22 |
2.1 |
| October 19, 2008 |
4:26 |
1.2 |
| October 19, 2008 |
4:58 |
1.8 |
| October 19, 2008 |
5:06 |
1.0 |
| October 19, 2008 |
5:08 |
0.8 |
| October 19, 2008 |
5:08 |
1.0 |
| October 19, 2008 |
5:17 |
1.7 |
| October 19, 2008 |
5:45 |
1.5 |
| October 19, 2008 |
5:49 |
1.5 |
| October 19, 2008 |
5:50 |
1.6 |
| |
|
|
| October 20, 2008 |
10:16 |
1.5 |
| October 20, 2008 |
20:08 |
1.2 |
| October 20, 2008 |
20:14 |
1.1 |
| |
|
|
| October 23, 2008 |
11:55 |
1.2 |
| |
|
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| November 6, 2008 |
23:07 |
1.4 |
| |
|
|
| December 31, 2008 |
00:34 |
2.1 |
| |
|
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| April 22, 2009 |
9:21 |
1.1 |
| April 23, 2009 |
6:26 |
2.4 |
| April 24, 2009 |
1:36 |
2.9 |
| April 30, 2009 |
18:36 |
2.0 |
| |
|
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| May 11, 2009 |
1:18 |
1.3 |
| May 11, 2009 |
1:34 |
1.2 |
| |
|
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| October 25, 2009 |
7:16 |
2.6 |
| October 25, 2009 |
7:18 |
1.8 |
| October 25, 2009 |
7:21 |
2.8 |
| June 3, 1020 ** |
8:25 |
2.9 |
The report on the portable seismographs from Columbia University -
Lamont-Doherty Earth Observatory has been published into an
open-file report by the Pennsylvania Geologic Survey.
Click here to read report which includes epicenter, foci and
some thinking on what are causing the tremors.
** 2.9 magnitude earthquake rattles region on
June 3, 2010
At 8:25 a.m. local time, a 2.9 magnitude earthquake rattled a large
region in York, Adams, Cumberland and Dauphin counties,
Pennsylvania. Reports came in from Derry Township and Highspire,
Dauphin County, the Capital building in Harrisburg, Boiling Springs
area, Dover, Mechanicsburg and York Springs. As explained in the
Lamont-Doherty Observatory report on the other Dillsburg tremors,
the closest seismograph to the Dillsburg area are the seismographs
at the Pennsylvania Geologic Survey in Middletown and Millersville
University. No portable stations are deployed in the Dillsburg
region at this time. The further a station is from the epicenter,
the more inaccuracy you get on locating the origin of the tremor. A
calculation of ±5 km accuracy was derived from the previous
Dillsburg tremors.
After several days of interviews, an epicenter of just south and
west of Mt. Pleasant, Monaghan Township was established. Some folks
living in this area reported the tremor as “thought a Mack truck was
coming through the wall and my floor felt like it lifted up a foot.”
This epicenter is about 4 miles northeast of the epicenter area of
the many other Dillsburg tremors.
As mentioned above, the magnitude of this tremor was established as
a 2.9. Initial reports listed the event as a 3.1, but was
down-graded by the Lamont-Doherty seismologists to a 2.9. Based on
the regional extent of this tremor compared to another 2.9 tremor in
the Dillsburg area, the June 3rd tremor had a much larger reach out
into the community. Both Dr. Charles Scharnberger of Millersville
University and myself like the 3.1 magnitude better.
Below is an isoseismal map for the June 3rd event. The small circle
in the middle represents the epicenter with a Modified Mercalli 4
ranking.

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