

Part of Rachel Clark Design's Friday Filter Challenge.
Technorati tags: Rachel+Clark+Designs Friday+Filter+Challenge Halloween diffuse+glow Wordless+Wednesday
_/\_/\_
_/\_/\_
Earlier this month, a quake measuring 1.8 on the Richter scale rattled homes in Amesbury and Merrimac. Officials said that the quake was a late aftershock of an earthquake from 1727 in Newburyport.Can aftershocks linger for 280 years? I went to the United States Geological Survey site to learn more. First, about the Newburyport earthquake:
At Newbury, many stone walls and chimney bricks were shaken down, and almost all tops of chimneys were knocked off. Considerable changes occurred in the flow of water in springs and, in some springs, changes occurred in the character of the water. "Some firm land became quagmire, and marshes were dried up." The rise and fall of the ground made it difficult to walk, and houses shook and rocked as if they would fall apart. Sand blows were reported near Spring Island. Felt from the Kennebec River in Maine to the Delaware River on the New York-Pennsylvania border and from ships at sea to the "extreme western settlements." Aftershocks occurred in the area for several months. The strongest aftershock (MM intensity V) occurred in the Newbury area on Dec. 28, 1727, and Jan. 4 and Feb. 10, 1728 (local dates).Second, the definition of aftershock:
"Foreshock" and "aftershock" are relative terms. Foreshocks are earthquakes which precede larger earthquakes in the same location. Aftershocks are smaller earthquakes which occur in the same general area during the days to years following a larger event or "mainshock", defined as within 1-2 fault lengths away and during the period of time before the background seismicity level has resumed. As a general rule, aftershocks represent minor readjustments along the portion of a fault that slipped at the time of the main shock. The frequency of these aftershocks decreases with time. Historically, deep earthquakes (>30km) are much less likely to be followed by aftershocks than shallow earthquakes. (Univ. of Washington)So yes, it is possible, I suppose, for the 1.8 quake earlier this month to be an aftershock from 1727. I don't know if it is, though. I could not find any other source to confirm it.
One of the most gothic elements associated with Bristol is the belief that a murdered boy and his sidekick, a demonic hound, hold an eternal vigil in the lightless bowels of the mine shaft. They are preternaturally compelled to forever guard against would-be treasure hunters. Franklin S. Harvey wrote, "As these patient toilers hewed their way through the ledge and drew nearer to the object of their search, they could hear the boy sign and groan . . ."
_/\_/\_