| dc.creator |
Niebergall, Ernst |
|
| dc.date |
2008-04-28T19:01:42Z |
|
| dc.date |
2008-04-28T19:01:42Z |
|
| dc.date |
1909-1919 |
|
| dc.date |
2008-04-28T19:01:42Z |
|
| dc.date.accessioned |
2013-10-16T04:29:30Z |
|
| dc.date.available |
2013-10-16T04:29:30Z |
|
| dc.date.issued |
2013-10-16 |
|
| dc.identifier |
348.20.u158 |
|
| dc.identifier |
20 |
|
| dc.identifier |
http://hdl.handle.net/2374.OX/2018 |
|
| dc.identifier.uri |
http://koha.mediu.edu.my:8181/xmlui/handle/2374 |
|
| dc.description |
Tufa rock is a porous rock formed when water with a heavy lime content evaporates. Abundant limestone deposits, lots of underground rivers, sink holes - like the Blue Hole - and marshes around Castalia made a fertile ground for the growth of tufa rock. Evaporating water left mineral deposits that encrusted twigs, small pebbles, etc. and grew into unique rock formations. |
|
| dc.format |
5" x 7" |
|
| dc.language |
eng |
|
| dc.publisher |
Rutherford B. Hayes Presidential Center |
|
| dc.relation |
Charles E. Frohman Collection |
|
| dc.rights |
Rutherford B. Hayes Presidential Center |
|
| dc.rights |
http://www.rbhayes.org/hayes/photographs/display.asp?id=497&subj=photographs |
|
| dc.subject |
Erie County (Ohio) |
|
| dc.subject |
Castalia (Ohio) |
|
| dc.subject |
Cold Creek (Ohio) |
|
| dc.subject |
Rivers - Ohio - Erie County |
|
| dc.subject |
Springs - Ohio - Erie County |
|
| dc.title |
Tufa Rock |
|
| dc.type |
Photographic print; black and white |
|
| dc.coverage |
Erie County (Ohio) |
|
| dc.coverage |
Castalia (Ohio) |
|
| dc.coverage |
1901-1919 |
|