When Geological Processes Collide– Exploring the Link Between Earthquakes and Glaciers

What happens when glaciers melt? Scientists have discussed numerous effects of deglaciation including sea level rise and loss of habitats but recently, geologists have been thinking about how glaciers interact with the crust of the earth. Researchers from the University of Alaska, Fairbanks found a link between melting glaciers and earthquakes in Southeast Alaska which adds new understanding about the indirect effects of climate change and the role of humans in natural disasters.

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Listen for a Change: Bioacoustics in Restored Habitat Combats the Bird Decline

Excerpt: A recent study has revealed that 3 billion birds have disappeared since 1970 in North America. Restoring habitat can help reverse this loss, and technology in listening for birds can be a vital tool to see if this approach to restoring bird habitat is working.

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Alaskan Megathrust Earthquakes: Sedimentary records provide new data and a look 2000 years into the past

In 1964, a historically unprecedented magnitude 9.2 earthquake struck the Aleutian Islands of Alaska. The earthquake prompted scientists to figure out that the Aleutians lie along a unique form of fault, now known as a “megathrust” fault. During a megathrust earthquake, large swaths of land suddenly rise or sink, depending on their location relative to the fault rupture. Over long periods of time, as tectonic plates slide under one another, compression causes the top plate to buckle and rise up along the coast. When enough energy is accumulated, a slip eventually occurs. In places that were being uplifted, the land suddenly falls a few meters as the strain is released, otherwise known as an earthquake. It has been thought that areas of uplift and subsidence remain constant, always rising or falling in exactly the same place with every earthquake. However, a recent study suggests that these areas are not constant, further complicating our understanding of how “megathrust” earthquakes occur.

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