Was a sizeable earthquake that rocked Knoxville, Tennessee, on March 28, 1913—just when the massive floodwaters were receding from Ohio and Indiana—somehow related to or even triggered by the Great Easter Flood?
BOOM!
At the loud
shock of what sounds like the building’s boiler exploding, reporters at The Journal and Tribune in Knoxville,
Tennessee, rush to the windows. On the sidewalks below, people are pouring out
of office buildings, factories, and stores into the streets.
Front page story of the Knoxville Journal and Tribune for Saturday, March 29, 1913, about the earthquake shaking the city the afternoon before. |
Simultaneously,
every phone in the newspaper offices starts ringing, anxious residents
demanding answers to the same questions the reporters themselves are wondering:
“Was that an explosion?” “The marble courthouse shook like a leaf for half a
minute!” “It woke me from sound sleep!” “Pictures fell from the walls, the
clocks stopped, and the brick chimney of my neighbor’s house fell into my yard!”
“Did a meteor hit us?” “The asphalt paving in the street literally cracked!” “The
earth literally jumped! It made me feel queasy, physically ill.”
…BOOM!
A second
loud shock with a whip-like motion of the earth, maybe three minutes after the
first one around 4:55 PM Friday, March 28, 1913, set off a fire alarm near the
Southern Railway depot. Dinging fire trucks race through the streets to the
scene, fearing a locomotive had exploded… but there is no fire. Phone calls to
the newspaper offices become even more frantic, reporting wild rumors: the
Knoxville Banking & Trust Co. building collapsing, an oil truck exploding,
gunpowder at the Hand Powder Co. igniting, or a magazine at zinc mines at
Mascot blowing up—all of which the reporters verify to be false.
“Get close to the walls!” shouts a man at the weekly planning meeting of the directors of the National Conservation Exposition. “The building is falling in. Maybe the walls will hold.” In instants, the dozen men are hugging walls as the building sways.
That warning may have been shouted by geology professor C. H. Gordon of the University of Tennessee, who is attending the meeting, and who instantly knows exactly what was happening: an earthquake. Indeed, the fact that objects in the room were being thrown up and down instead of side to side suggests to Gordon that Knoxville itself was right over the center of the earthquake.
That earthquake
realization dawns also on the reporters, after they start receiving calls from
towns miles outside of Knoxville—Newport, Sevierville, Morristown, Maryville,
Jellico. Clearly, this phenomenon was so widespread it could be no mere
explosion: it had to be an earthquake—indeed, the most severe the city had
experienced since the Big One of 1865.
At "ground zero" Dayton, Ohio, of the 1913 flood, homes were inundated up to their eaves. Credit: Dayton Metro Library |
But
Knoxville residents are jumpy. As one reporter at The Journal-and Tribune rather breathlessly observed in a long
article on March 30, “There have been so many appalling floods and disasters of
late that they have preyed upon the minds of people, and the disposition of the
public just at this time is very excitable, everybody’s nerves at high tension,
and most anybody is prepared to believe that almost anything bad may happen.”
Map in Bulletin Z documented flood down the Mississippi River. |
In
fact, on Friday, March 28, just as the earthquake struck Knoxville, the
massive, multistate Great Easter Flood precipitated by unprecedented rains
beginning Sunday, March 23, was still well in progress—although the floodwaters
were just receding from the streets of “ground zero” Dayton, Ohio, where entire
houses had been inundated to their eaves (see “Like a War Zone”). The flood crest cascading down the Ohio River had not yet reached Paducah,
Kentucky.
The public nervousness
was not helped when an aftershock struck Knoxville less than three weeks later,
on April 17 (at which time the devastating floodwaters had poured out of the
Ohio River and the flood crest was bursting levees halfway down the Mississippi River.
Mid-continent active seismic zone
Earthquakes
in Knoxville, Tennessee??
Yes,
indeedy. In fact, just this year (July 2014) the U.S. Geological Survey
released new maps
upgrading the seismic risk of living in eastern Tennessee.
How
extensive was the March 28, 1913 earthquake and the April 17 aftershock?
Fortunately for researchers today, University of Tennessee geologist Gordon immediately began scouring
Knoxville and the surrounding areas, surveying damage and interviewing
residents. His field work and map, published in the December 1913 Bulletin of the Seismological Society of
America, revealed that the quakes had been felt over a 7,000-square-mile
area.
Cover of July 2014 USGS report. I added an arrow pointing to Knoxville in a seismic zone. |
How strong
was the March 28, 1913 earthquake?
In 1913, the
familiar Richter scale that measured the magnitude of earthquakes—that is, the
amount of energy the earthquake released—had not yet been invented (it was
introduced by Caltech seismologist Charles Richter in 1935. And FYI: since the
late twentieth century, the Richter scale has now been supplanted by the
moment magnitude scale, because the monumental Chilean earthquake of 1960 and
the Alaska earthquake of 1964 revealed the inadequacy of the Richter scale in
measuring truly powerful earthquakes.) So in 1913, the scale then in use was
the Mercalli scale, adopted in 1902.
This scale comparing the Modified Mercalli Scale with the Richter scale is on the website of the Missouri Department of Natural Resources. |
The Mercalli
scale measures the local intensity of
an earthquake by the shaking of the earth’s surface, as indicated by damage
observed: chimneys falling, pavement ruptured, people running outdoors. Based
on the Mercalli scale, the USGS rates the intensity of the March 28, 1913
Knoxville earthquake as VII on the Mercalli scale, although perhaps the cracked pavement
might indicate it was higher—up to a IX—in some locations.
But the Mercalli scale is not an absolute measure of the power of the earthquake itself, as the Richter and moment magnitude scales are: after all, the intensity of local shaking falls off with distance from the epicenter, and the damage observed to manmade structures depends on the soundness or flimsiness of their construction as well as on local geology. And if the quake’s epicenter is deeply buried, a stronger quake might produce less shaking at the surface than a shallower quake of lesser magnitude.
But the Mercalli scale is not an absolute measure of the power of the earthquake itself, as the Richter and moment magnitude scales are: after all, the intensity of local shaking falls off with distance from the epicenter, and the damage observed to manmade structures depends on the soundness or flimsiness of their construction as well as on local geology. And if the quake’s epicenter is deeply buried, a stronger quake might produce less shaking at the surface than a shallower quake of lesser magnitude.
Thus, although
there are scales that make rough comparisons of the Mercalli scale and the
Richter scale (see the green rulers above),
there actually is no one-to-one conversion between the scales because they
measure entirely different things (surface shaking versus total energy released).
Indeed, the Mercalli scale can be useful even today for categorizing damage to manmade
structures.
All
disclaimers notwithstanding, the USGS puts the strongest earthquake in Tennessee—the
big one of 1865—at a magnitude of 5.00. It also rates the 1865 quake’s Mercalli intensity as VII—yes, the same as the rating given for Knoxville in 1913. So by Midwest standards, it was an unusual
and significant earthquake that would have inspired apprehension and
respect even in California.
Could the Easter flood have triggered
the earthquake?
To borrow
the title of the 1950s TV game show, the $64,000 question is: Could the Knoxville earthquake of March 28, 1913 (if
not the aftershock of April 17) have been triggered by the massive multistate
Great Easter 1913 flooding of that entire week?
C.H. Gordon's map of the areas of shaking of the March 28, 1913 earthquake and its April 17 aftershock, published in the December 1913 issue of the Bulletin of the Seismological Society of America. |
A flood
trigger an earthquake?? Remember, this was no ordinary flood, as this entire
research blog has been documenting for nearly two years. The geological stresses
and strains of a sudden megatonnage of turbulent water over multiple states first
deluging then receding had to be monumental for the underlying rocks. Knoxville
lies in an active seismic zone. And the sheer timing gives pause: to paraphrase
Rick’s famous line in Casablanca, of all the earthquakes in all the regions in all the world, this one had
to occur in the Midwest as the Noachian waters were shifting…
For decades,
geologists have documented that earthquakes have been triggered in active
seismic zones when the reservoirs behind new dams have been filled for the
first time (see “Selected references” below). That possibility concerns
engineers, who want to ensure their dams are designed to withstand any likely
earthquake.
Natural floods
have also been implicated in the triggering of other California earthquakes. And in 2011, geophysicists at two Florida universities presented a research
paper before the American Geophysical Union called “Disaster triggers disaster”
that showed strong statistical
correlation between unusually heavy, wet tropical cyclones and subsequent
earthquakes.
I’m not a
geologist or geophysicist—my background is in physics and astrophysics, with a
good smattering of engineering, planetary sciences, meteorology, and history of
science—nor am I familiar with the geologies of Ohio, Indiana, Kentucky, or
Tennessee. So this post ends with the same open question with which it begins: Was a sizeable earthquake that rocked Knoxville,
Tennessee, on March 28, 1913—just when the massive floodwaters were receding
from Ohio and Indiana—somehow related to or even triggered by the Great Easter
Flood?.
I would very
much welcome hearing from geologists and geophysicists, including exploring the
possibility of collaborating on a potential research article (my historical
data and your geophysical expertise). Please contact me at t.e.bell@ieee.org.
Next month:Advertising Disaster
Selected references
Selected references
Bulletin Z. The Floods of 1913 in the Rivers of the Ohio
and Lower Mississippi Valleys. U.S. Department of Agriculture. Weather
Bureau. Washington, Government Printing Office, 1913. Principal author was
Alfred J. Henry, but additional reports were contributed by five other authors.
Gordon, C.
H., “Earthquakes in East Tennessee,” Bulletin
of the Seismological Society of America 3: 191-194, December 1913.A
longer version of the same article under the same title was published in The Resources of Tennessee (the journal
of the State Geological Survey) 4(1): 15–23, January 1914.
“How was the Richter scale for measuring earthquakes developed?” Scientific American. The USGS provides a somewhat technical description of the Richter scale and the moment magnitude scale. Actually, if you really want to dive deep into the weeds, there are half a dozen scales for measuring aspects of earthquakes, as described on this page of an education module developed by the Southern California Earthquake Data Center.
“How was the Richter scale for measuring earthquakes developed?” Scientific American. The USGS provides a somewhat technical description of the Richter scale and the moment magnitude scale. Actually, if you really want to dive deep into the weeds, there are half a dozen scales for measuring aspects of earthquakes, as described on this page of an education module developed by the Southern California Earthquake Data Center.
For more about the statistical evidence that extremely heavy, wet tropical cyclone seasons have triggered large earthquakes, see this press release from the University of Miami describing the work of Shimon Wdowinski.
Bell, Trudy E., The Great Dayton Flood of 1913, Arcadia Publishing, 2008. Picture book of nearly 200 images of the flood in Dayton, rescue efforts, recovery, and the construction of the Miami Conservancy District dry dams for flood control, including several pictures of Cox. (Author’s shameless marketing plug: Copies are available directly from me for the cover price of $21.99 plus $4.00 shipping, complete with inscription of your choice; for details, e-mail me), or order from the publisher.