Le antiche lucerne sepolcrali figurate, raccolte dalle cave sotterrance e grotte di Roma...

Plates in three groups, each preceded by half title not included in paging.

Fort Stanton-Snowy River National Cave Conservation Area Act : report (to accompany S. 1170).

"October 27, 2005."

Guide leaflet, geological science field trip, Rosiclare area : Hardin County, Golconda, Cave in Rock, Shawneetown, and Equality Quadrangles /

April 12, 1958.

CEG after a morning of cave digging

Loay, Bohol, Philippines

Donovan Bowerbank (left) & Nick K. (in red) at Valentine celebration, February 1987 (date printed by photo lab on back)

We could probably get sharper focus on another scanner with manual focus adjustment

An excursion to the Mammoth Cave, and the barrens of Kentucky : with some notices of the early settlement of the state /

Title on spine: Mammoth Cave of Kentucky.

Overture to The Hebrides (Fingal's Cave) op. 26.

Mode of access: Internet.

Cudjo's cave,

Bound in red cloth; decorated front cover and spine; stamped in yellow and light green.

A late Pleistocene predator-accumulated avifauna from Kids Cave, West Coast, South Island, New Zealand

A fossil deposit excavated from the floor of Kids Cave, West Coast, South Island, New Zealand, is interpreted as having been primarily accumulated by New Zealand falcon Falco novaeseelandiae, with some contribution by Haast's eagle Harpagornis moorei. The fauna is rich: 3699 bones represented 41 bird species, two frog species, unspecified geckoes and skinks, and one bat species. Fossil deposition was mainly within the Last Glacial Maximum from about 22,000 cal yr bp to about 15,000 cal yr bp, with a marked change in sediment characteristics at the onset of the LGM's coldest period. Chronological control is given by three Uranium-series dates for a speleothem and radiocarbon AMS dating of four avian eggshell samples and one bone. The fauna is the first extensive predator accumulation of LGM age described from the West Coast of the South Island, and it indicates a palaeoenvironment of a mosaic of shrublands with forest patches. The onset of the coldest part of the LGM (Aurora 3 glacial advance, 19,500 - 19,000 cal yrs bp) saw marked climate cooling/drying affecting the site, but the avifauna indicates that although open-country taxa became more common in this period, some forest persisted nearby throughout the remainder of the LGM.