1755 Cape Ann earthquake
|Date||November 18, 1755|
|Areas affected||British America, Province of Massachusetts Bay|
|Max. intensity||VIII - Destructive|
The Cape Ann Earthquake took place off the coast of the British Province of Massachusetts Bay (present-day Massachusetts) on November 18, 1755. At between 6.0 and 6.3 on the Richter scale, it remains the largest earthquake in the history of Massachusetts. No one was killed but it damaged hundreds of buildings in Boston and was felt as far north as Nova Scotia and as far south as South Carolina. Sailors on a ship more than 200 miles (320 km) offshore felt the quake, and mistook it at first for their ship running aground. Many residents of Boston and the surrounding areas attributed the quake to God, and it occasioned a brief increase in religious fervor in the city. Modern studies estimate that if a similar quake shook Boston today, it would result in as much as $5 billion in damage and hundreds of deaths.
The earthquake took place on November 18, 1755, at approximately 4:30 AM. Its epicenter is believed to have been offshore, approximately 24 miles (39 km) east of Cape Ann. The quake was felt as far north as Halifax, Nova Scotia, south to the Chesapeake Bay and South Carolina, and from Lake George and Lake Champlain in the northwest to a ship 200 miles (320 km) off the east coast. Sailors on the ship reported that the quake was so strong, they had feared that they had run aground. The region experienced several aftershocks, the first of which was a little more than an hour after the quake. Most of these aftershocks could not be felt in Boston, affecting only the cape cod northeastern coast of the colony.
Modern research has estimated that the quake was between 6.0 and 6.3 on the Richter scale, and the United States Geological Survey lists it as the largest earthquake in the history of Massachusetts. Scientists are unclear on the causes of this and other quakes in the northeastern United States. There are a number of old faults in the region, but none of them are known to still be active. It is possible that the Cape Ann earthquake may have been remotely triggered by a larger earthquake in Lisbon, Portugal a few weeks prior, although there is not enough evidence to prove that they are linked.
Boston and Cape Ann were the most heavily damaged. In Boston, damage was concentrated in areas of infill near the harbor; infill is less sturdy in earthquakes than solid land. From 1,300 to 1,600 chimneys in the city were damaged in some way, the gable ends of some houses collapsed, and a number of roofs were damaged by falling chimneys. Stone chimneys and buildings were damaged in Falmouth (present-day Portland, Maine), Springfield, Massachusetts, and New Haven, Connecticut as well. Some church steeples in Boston were damaged, ending up tilted from vertical. Stone fencing in rural areas was damaged. Observers also reported that several springs dried up, new ones were created, and cracks appeared in the ground near Scituate, Lancaster, and Pembroke. In this last town, observers noted water and fine sand coming from the crack. Non-structural damage was minor; residents reported damage to china and glassware, and a distiller lost some of his product after a cistern was damaged. The Cape Ann earthquake may also have created the first recorded tsunami in U.S. history. Observers in the Leeward Islands nearly 1,000 miles (1,600 km) south of Cape Ann, reported a receding of water followed by a large wave that lifted several boats ashore and left fish floundering on the beach.
Many Massachusetts residents of the time perceived the quake as punishment from God for immoral behavior. In the days after the earthquake, special prayer services were held and civic authorities declared fast days. A number of sermons and other writings were published as a consequence, including Jeremiah Newland's Verses Occasioned by the Earthquakes in the Month of November, 1755 and Thomas Prince's Earthquakes the Works of God and Tokens of his Just Displeasure. Not all explanations of the event were theological; John Winthrop, a Harvard professor, proposed an alternate explanation having to do with heat and chemical vapors inside the surface of the earth.
Since the 1755 earthquake, Boston and its surrounding towns have become a major metropolitan area. Much new construction has been built on infill, especially in the Back Bay area, which may be prone to greater shaking and to compaction of the sand and gravel used as fill. Many older buildings in the Boston area are built from stone and brick, and are likely to collapse completely during a major earthquake. Given this, modern observers have expressed concern about the effects of another quake in such a major city. A 1990 study by the Massachusetts Emergency Management Agency estimated potential financial losses at between $4 billion and $5 billion, and potential loss of life in the hundreds. As a consequence, the state has updated building codes and zoning laws to require that new construction and additions in vulnerable areas be built to resist earthquakes.
Opposition to the Seabrook Station Nuclear Power Plant, about 15 miles off Cape Ann on the New Hampshire shoreline, highlighted the earthquake risk of the area. The plant was built regardless.
- Ebel, J.E. (2006). "The Cape Ann, Massachusetts earthquake of 1755: a 250th anniversary perspective". Seismological Research Letters 77 (1): 74–86. doi:10.1785/gssrl.77.1.74. Retrieved 2009-10-17.
- Ballard C. Campbell, ed. American Disasters: 201 Calamities That Shook the Nation (2008) pp 28-30
- Newman, William A. and Holton, Wilfred E. (2006). Boston's Back Bay: the story of America's greatest nineteenth-century landfill project. University Press of New England. pp. 177–180. ISBN 1-55553-651-4.
- "Cape Ann, Massachusetts". Historical Earthquakes. United States Geological Survey. Retrieved 2009-10-17.
- Ebel, John. E. "The Cape Ann Earthquake of November 1755". The Massachusetts Historical Society. Retrieved 2009-10-17.
- Hough, Susan Elizabeth; Bilham, Roger G. (2006). After the Earth quakes: elastic rebound on an urban planet. Oxford University Press US. pp. 23–24. ISBN 0-19-517913-7.
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