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SWAP Meeting with 2014 Brown Award Recipients

The UK Appalachian Center is hosting a SWAP (Sharing Work on Appalachia in Progress) Meeting from 12 p.m. to 1:30 p.m. on Thursday, February 19, 2015.  Two of five 2014 Brown Award recipients, Lindsay Shade and Kathryn Engle will be presenting on their research.  Each presenter has research interests in Appalachia and are graduate students at the University of Kentucky.

Date:
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Location:
UK Appalachian Center

Lexington Old-Time Music Gathering

Please, join in the fun at the Lexington Old-Time Music Gathering in Lexington, KY!  This event spans February 12, 2015 through February 15, 2015 and has something for everyone.  This is an opportunity for community engagement, learning about traditional mountain music, and hearing artists perform.  During the Saturday, 2/14/15 event, there will be fun for all ages at the Appalachian Youth Day portion of the event from 12 p.m. to 5 p.m.  Admission for the Youth Day is free, and there will be workshops, open mic, jam sessions, singing, and dances!  (Please note that a parent must accompany children at all times.)  Please, see the Lexington Old-Time Music Gathering website for detailed information, including a full schedule of performers and events: http://lexoldtime.com/.

Date:
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Location:
Various including ArtsPlace, 161 North Mill Street, Lexington, KY, Al's Bar, Willy's Locally Known, and Windy Corner Market

WUKY's "UK Perspectives" Talks about UK in Appalachia

WUKY's "UK Perspectives" focuses on the people and programs of the University of Kentucky and is hosted by WUKY General Manager Tom Godell.  This week News Director Alan Lytle guest hosts and visits with UK President Eli Capilouto about the new "Rooted in our Communities" Appalachian initiative recently launched by the university. 

This podcast provided courtesy of 91.3 WUKY.

THE CYCLE OF EROSION

 

Out on the trails of Shaker Village at Pleasant Hill, Kentucky, this morning, I got to thinking about William Morris Davis’ “cycle of erosion” conceptual model (also called the geographical or geomorphological cycle). The drive-by, oversimplified version is that landscape evolution starts with uplift of a more-or-less planar, low relief surface. Weathering and erosion goes to work, and results in an initial stage of increasing relief as streams carve valleys, and slope processes operate on the slopes thereby created. Eventually, however, as the streams begin to approach base level, a new stage of decreasing relief begins as hilltops and drainage divides are lowered and valleys infilled. This continues until the entire landscape is about as close to baselevel as the geophysics of mass transport will allow, creating a low-relief, almost-planar surface called a peneplain. At some point a new episode of uplift occurs and the cycle begins anew.

I was thinking of this because many landscapes in the world, like the one I was viewing this morning, do give the impression of a dissected plateau or a low-relief surface into which denudational processes have cut.

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