Both faults are along plate boundaries that move in similar ways and have ruptured in enormously destructive earthquakes in the past.
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Some rocks will burn, and others will melt, depending on how they were formed and what minerals they contain.
Understanding why some faults creep rather than sticking and causing massive earthquakes is important for gauging the future risk of both earthquakes and tsunamis.
Fill your Feeders: The Christmas Bird Count will take place on Saturday, Dec. 27, in the Bridgton/Sweden circle. Mary Jewett serves as the com…
Winter is in the air, and ice is starting to form on some of the smaller lakes and ponds in the region. Lakes Environmental Association collec…
CL w16 UMaine Extension offers workshop to help farmers get more from soil health practices
The United States Geological Survey reported that an earthquake struck off the coast of Maine on Monday morning, and it was felt as far away a…
