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KSU Agricultural Experiment Station at Hays, Kansas. Bull sculpture is one of many around town by local sculptor Pete Felten who runs the Stone Gallery (www.gigapan.org/viewGigapan.php?id=2251). Taken while I was waiting for my pizza to be made.
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Pillars of Smoky Hill Chalk in the Castle Rock Badlands, south of Quinter, Kansas. I shot this one to capture the contrast in cloud types on either side of the central pillar. I'd appreciate it if a meteorologist could properly identify the cloud types in snapshots or comments.
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- 1969
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180-plus degree panorama at the corner of Park Street and South Campus Drive on the campus of Fort Hays State University. Sheridan Hall is the main administration building at FHSU. Sheridan used to be the main gymnasium on campus and now houses the Beach Schmidt auditorium. Jellison Bridge (www.gigapan.org/vi...
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Union Pacific railroad bridge over Big Creek on the west side of Hays, Kansas. In April 2006 I got a chance to catch Union Pacific steam locomotive No. 844 coming off this bridge (ron.outcrop.org/blog/?p=49
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The Stone Gallery (www.haysusa.com/html/the_arts.html#Picture518
) is the studio of local sculptor Pete Felten, located in downtown Hays, Kansas. A number of sculptures are visible in the yard along with plenty of cats. Subtle vignetting due to insufficient overlap in the original photoset.-
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Another angle on the new Alumni/Foundation Center at FHSU. Same stitching issues as www.gigapan.org/viewGigapan.php?id=2246
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There's a subtle vignetting because I didn't use enough overlap between the images - other stitching irregularities probably for the same reason.
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- 2017
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Erosional remnant of the Smoky Hill Chalk at the Castle Rock Badlands, south of Quinter, Kansas.
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Cretaceous Niobrara Formation, Fort Hays member overlying Cretaceous Carlile Shale, Codell Sandstone member. Some nice fossil details can be seen in the large blocks of Fort Hays chalk on the left. Shot in the last few minutes before sunset. The Moon is just visible at the top of the image - it was rapidly rising ou...
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Tertiary Ogallala Formation conglomerates form a resistant cap that holds up the soft, thin bedded Cretaceous Niobrara Formation, Smoky Hill member chalk deposits below.
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