enola swarm area - faulkner county, arkansas event in the enola swarm area. another notable seismic...

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GH-EQ-ENOLA-002 E E E E E E E E E E E E E E E E E E E E E E E E Æ þ 64 Æ · 36 " ) McGintytown " ) Centerville " ) Barney " ) Naylor " ) Hamlet Faulkner County 2001 (M 4.4) 1982 (M 4.0) 1982 (M 4.5) 1982 (M 4.1) Holland Vilonia Enola Mount Vernon Æ · 36 Æ · 107 Æ · 225 Æ · 310 Æ · 287 Æ · 319 Æ · 107 Æ þ 64 1 0 1 2 3 4 5 0.5 Miles 1 0 1 2 3 4 5 0.5 Kilometers Arkansas Missouri Illinois Kentucky Tennessee NMSZ The area covered by this map is shaded in blue and is located in Faulkner County, Arkansas. Faulkner County and is included within the New Madrid seismic zone (NMSZ) catastrophic planning area (shaded in pink) as designated by the Arkansas Department of Emergency Management (ADEM). The New Madrid seismic zone is shaded in purple. ( N Revised: 08 December 2008 This map represents a sampling of seismic events recorded near the town of Enola in central Arkansas. This seismically active area is known as the “Enola swarm area.” The first seismic event recorded here was a 1.2 magnitude earthquake that occurred on January 12, 1982. Over 40,000 seismic events have occurred in the Enola swarm area since 1982, making it possibly the largest seismic swarm ever recorded in the central United States (Chiu et al., 1984). Most of the seismic events are microquakes, but numerous felt events have been experienced. During the first year of seismic activity, at least 93 earthquakes were felt in the Enola swarm area by at least one person. A 4.5 magnitude earthquake was recorded on January 21, 1982, making it the largest seismic event in the Enola swarm area. Another notable seismic event was the 4.4 magnitude earthquake recorded on May 4, 2001. This event was followed by aftershocks greater than magnitude 2.0. The most recent seismic event was a 2.8 magnitude earthquake recorded on October 17, 2006. Earthquakes associated with the Enola swarm have caused no structural damage, although there have been reports of broken china near epicentral areas. Research indicates that earthquakes occurring in the Enola swarm area are not associated with the New Madrid seismic zone of northeast Arkansas (McFarland, 2001). About the Map Enola Swarm Area - Faulkner County, Arkansas By Scott M. Ausbrooks and Erica Doerr Digital Compilation by Jerry W. Clark Arkansas Geological Survey, State Geologist, Bekki White 2007 Symbols US Highways State Highways Incorporated Areas Æ · 225 ¡ ¢ 62 Although this map was compiled from digital data that was successfully processed on a computer system using ESRI ArcGIS 9.x software at the Arkansas Geological Survey (AGS), no warranty, expressed or implied, is made by the AGS regarding the unity of the data on any other system, nor shall the act of distribution constitute any such warranty. The AGS does not guarantee this map or digital data to be free of errors or liability for interpretations from this map or digital data, or decisions based thereof. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the Arkansas Geological Survey. The 5M DEM base used in the making of this map was acquired at the Spatial Analysis Laboratory, University of Arkansas, Monticello and some of the other Feature Class Data was acquired at the GeoStor online. Disclaimer References Chiu, J, Johnson, A.C., Metzeger, A.G., Haar, L. and Fletcher, J., 1984, Analysis of analog and digital records of the 1982 Arkansas earthquake swarm: Bull. Seismological Society of America, 74: 1721-1742. Johnston, A., et al, 1982, The Central Arkansas earthquake swarm: Tennessee Earthquake Information Center (TEIC) Special Report # 8, parts 1, 2. McFarland, J. D., 2001, Faulkner County earthquakes: Arkansas Geological Commission, Open-File Report. We extend our appreciation to John David McFarland III for compiling the original earthquake database used to make this map and for sharing his knowledge of Arkansas Seismicity. We also thank Buddy Schweig, USGS and Center for Earthquake Research and Information (CERI) at the University of Memphis and Russell Wheeler for their advice regarding the earthquake database. Acknowledgments E Earthquake Magnitudes 0.0 - 1.9 2.0 - 2.9 3.0 - 3.9 4.0 - 4.9

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GH-EQ-ENOLA-002

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Æþ64

Æ·36

")McGintytown

")Centerville

") Barney

")

Naylor

")Hamlet

Faulkner County

2001 (M 4.4)

1982 (M 4.0)

1982 (M 4.5)

1982 (M 4.1)

Holland

Vilonia

Enola

MountVernon

Æ·36

Æ·107

Æ·225

Æ·310

Æ·287

Æ·319

Æ·107

Æþ64

1 0 1 2 3 4 50.5Miles

1 0 1 2 3 4 50.5Kilometers

ArkansasMissouri

Illinois

Kentucky

Tennessee

NMSZ

The area covered by this map is shaded in blue and is located in Faulkner County, Arkansas. Faulkner County and isincluded within the New Madrid seismic zone (NMSZ) catastrophic planning area (shaded in pink) as designated by the Arkansas Department of Emergency Management (ADEM). The New Madrid seismic zone is shaded in purple.

(N

Revised: 08 December 2008

This map represents a sampling of seismic events recorded near the town of Enola in central Arkansas. This seismically active area is known as the “Enola swarm area.” The first seismic event recorded here was a 1.2 magnitude earthquake that occurred on January 12, 1982. Over 40,000 seismic events have occurred in the Enola swarm area since 1982, making it possibly the largest seismic swarm ever recorded in the central United States (Chiu et al., 1984). Most of the seismic events are microquakes, but numerous felt events have been experienced. During the first year of seismic activity, at least 93 earthquakes were felt in the Enola swarm area by at least one person. A 4.5 magnitude earthquake was recorded on January 21, 1982, making it the largest seismic event in the Enola swarm area. Another notable seismic event was the 4.4 magnitude earthquake recorded on May 4, 2001. This event was followed by aftershocks greater than magnitude 2.0. The most recent seismic event was a 2.8 magnitude earthquake recorded on October 17, 2006. Earthquakes associated with the Enola swarm have caused no structural damage, although there have been reports of broken china near epicentral areas. Research indicates that earthquakes occurring in the Enola swarm area are not associated with the New Madrid seismic zone of northeast Arkansas (McFarland, 2001).

About the Map

E n o l a S w a r m A r e a - F a u l k n e r C o u n t y , A r k a n s a sB y S c o t t M . A u s b r o o k s a n d E r i c a D o e r rD i g i t a l C o m p i l a t i o n b y J e r r y W . C l a r k

A r k a n s a s G e o l o g i c a l S u r v e y , S t a t e G e o l o g i s t , B e k k i W h i t e2 0 0 7

Symbols

US Highways

State Highways

Incorporated Areas

Æ·225

¡¢62

Although this map was compiled from digital data that was successfully processed on a computer system using ESRI ArcGIS 9.x software at the Arkansas Geological Survey (AGS), no warranty, expressed or implied, is made by the AGS regarding the unity of the data on any other system, nor shall the act of distribution constitute any such warranty. The AGS does not guarantee this map or digital data to be free of errors or liability for interpretations from this map or digital data, or decisions based thereof. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the Arkansas Geological Survey. The 5M DEM base used in the making of this map was acquired at the Spatial Analysis Laboratory, University of Arkansas, Monticello and some of the other Feature Class Data was acquired at the GeoStor online.

Disclaimer

References Chiu, J, Johnson, A.C., Metzeger, A.G., Haar, L. and Fletcher, J., 1984, Analysis of analog and digital records of the 1982 Arkansas earthquake swarm: Bull. Seismological Society of America, 74: 1721-1742. Johnston, A., et al, 1982, The Central Arkansas earthquake swarm: Tennessee Earthquake Information Center (TEIC) Special Report # 8, parts 1, 2. McFarland, J. D., 2001, Faulkner County earthquakes: Arkansas Geological Commission, Open-File Report.

We extend our appreciation to John David McFarland III for compiling the original earthquake database used to make this map and for sharing his knowledge of Arkansas Seismicity. We also thank Buddy Schweig, USGS and Center for Earthquake Research and Information (CERI) at the University of Memphis and Russell Wheeler for their advice regarding the earthquake database.

Acknowledgments

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Earthquake Magnitudes0.0 - 1.9

2.0 - 2.9

3.0 - 3.9

4.0 - 4.9