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The scaling analysis and numerical calculations indicates that welded tuff at elevations of 850~1100 m can be generated by a single tuff emplacement that decomposed into the upper and lower colonnades.
This finding indicates that the group of columnar joints of colonnades from 850 to 1100 masl in Mt. Mudeung may result from cooling of a single tuff emplacement, divided into upper and lower colonnades corresponding to the Seoseok-dae/Ipseok-dae and Gwangseok-dae colonnades, respectively.
Although the scaling analysis described above implies that welded tuff in the intermediate region of Mt. Mudeung were formed during a single tuff emplacement, it does not answer whether the growth rate of the columnar joints and the face width satisfy reasonable Peclet numbers ranging from 0.1 to 0.5 (Goehring et al., 2009).
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The ratio of the vertical extent of the upper colonnades to that of the lower colonnades (6:4) is consistent with their differences in extent (150 to 100 m), which indicates that the two colonnades resulted from a single thick tuff emplacement (thickness: ~250 m).
The single interbed of welded tuff represents a pyroclastic, ash-flow deposit (ignimbrite) produced by a nearby explosive eruption.
The upper part of the tuff is rooted by a single species of lycopsid (the third flora) again initiating peat accumulation.
To date, the origin of the Campi Flegrei caldera is still under debate and may be related to (1) a single caldera collapse associated with the Neapolitan Yellow Tuff (NYT) eruption, (2) two subsequent caldera collapses associated with the NYT and the preceding Campanian Ignimbrite (CI) eruptions forming a nested-caldera complex, or (3) not related to a caldera collapse after all.
Few geochemical variations of the Mudeungsan Tuff indicate that tuff originated from a single magma chamber.
Quantitative chronological ages have not been reported except for a single K/Ar age (48.1 ± 1.7 Ma) of the Mudeungsan Tuff located at the summit area of Mt. Mudeung (Ahn, 2010).
Nas first worked with Mr. Marley when he contributed a searing verse to "Road to Zion," a brooding single from Mr. Marley's Grammy-winning 2005 album "Welcome to Jamrock" (Tuff Gong/Universal).
The primary parameters of bilinear and nonlinear bond-slip laws were determined from experimental results of single shear bond tests that the authors conducted on masonry blocks of yellow tuff bonded with FRP carbon and glass fabrics.
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