# ent

id: 52216
type: ORG
entity:
  the Franklin Institute Of the Appalachian Mountain Club Of the American Philosophical Society Author


id: 52216
type: FAC
entity:
  La Glacière de Saint-Georges 62 Vertical Section of the Glacière de Saint-Georges 64 Vertical Section of Grand Cave de Montarquis


# bib

id: 14012
title: Ice-Caves of France and Switzerland
author: Browne, G. F. (George Forrest)
txt: ./txt/14012.txt
cache: ./cache/14012.txt
extension: .txt
mime: text/plain
summary:
  The existence of natural ice-caves at depths varying from 50 to 200 feet leaving an entrance 2 or 3 feet high to an inner cave--the glacière. the entrance to the cave is by a hole in the roof, which exposes the ice vertical, but sloped the wrong way, caving in under the stream of ice; time that the angle formed by the ice-wall and the slope of stones was lower parts of the cave, and the ice-floor is formed where the frost the lower cave, and the surface of the ice-wall there, gave no lower cave, for the ice-stream reached then a higher point of the wall, taken near the cave, when they either ice the water they have brought find their way back to the ice-cave, and thence to the foot of the rock observations of ''cold caves'', or the account of the mass of ice and


id: 18562
title: Outlines of the Earth''s History: A Popular Study in Physiography
author: Shaler, Nathaniel Southgate
txt: ./txt/18562.txt
cache: ./cache/18562.txt
extension: .txt
mime: text/plain
summary:
  we can readily note very great changes in its form since the land forms and falls in the air, as the streams flow to the sea, and as the Meanwhile the sea, because of the great heat-storing power of water, The great water store of the earth is contained in two distinct water in the beds, which in time is returned to the earth''s surface by land, where a great body of water journeys like an alternating river water tends, of course, to fall downward toward the earth''s surface, their heat through the water, and thus form ice on their surfaces, The crevice water of the earth, although forming at no time more than penetrates far below the earth''s surface or the open-air streams which material at the time when the rocks were formed in the sea. the surface to very great depths, so that not only is the rock water


id: 17354
title: Cave Regions of the Ozarks and Black Hills
author: Owen, Luella Agnes
txt: ./txt/17354.txt
cache: ./cache/17354.txt
extension: .txt
mime: text/plain
summary:
  forming the descent into Mammoth Cave is two hundred and thirty-two feet "The entrance to the cave, being thirty-eight feet lower than this bed of the crystals, show that the cave was completely filled with water passage of seventy feet length, we saw a narrow ledge of fine crystals, Unfortunately the quantity of water in the cave at the time of the The entrance to the cave is through a hole about two feet high by three Where the great spring forces its way to the surface, the water is a water now standing in the cave, and is not more than ten feet long by cave''s first beauty, the Red Room. Lake Room, where is Crystal Lake, the largest body of water in the cave. present natural entrance to the cave were the only way into this room deposits of still water as in other portions of the cave, but the


id: 14999
title: A Briefe Introduction to Geography
author: Pemble, William
txt: ./txt/14999.txt
cache: ./cache/14999.txt
extension: .txt
mime: text/plain
summary:
  1 _The earth and the water doe make one globe, i.e., one round or The naturall place of the water is to bee aboue the earth, and water, and let them both fall downe together vpon the earth from not bee, if the earth and water were two seuerall round bodies globes and let (_a_) bee the Center of the earth and (_b_) the center of the water; fr[~o] (_c_) some high place aboue the earth shadow of the earth and water cast vpon the Moone is round, and let (_X.O.R._) the inward Circle bee the earth, (_Q.S.P._) the Let (_X.O._) bee the Circle of the earth, and the greater the earth stand Eastwards in (_A_) the shadow of any body vpon the Heauens moue in one day, till the same point come to the place place wee aymed at, but let the earth moue, the stone will not


id: 33760
title: Fossil Ice Crystals: An Instance of the Practical Value of "Pure Science"
author: Udden, Johan August
txt: ./txt/33760.txt
cache: ./cache/33760.txt
extension: .txt
mime: text/plain
summary:
  Recently I have found that these ice crystal marks are quite common at one horizon in the Eagle Ford beds of Brewster County, in Texas. that the formation of ice crystals in wet mud has been observed in the in the discovery of the layer which carries ice crystal markings in Photographs of fossil imprints of ice crystals on flags of the Cuesta Blanca in Brewster County, Texas, and shows casts of crystals Photograph of fossil casts of a close tangle of ice crystals than any of the recent ice crystal marks figured here, but equally Photograph of fossil casts of ice crystals seen on some stony Photograph of fossil casts of ice crystals seen on the under of mud in which ice crystals had recently formed, in Rock Island, mud in which ice crystals had formed, in Rock Island, Illinois, soon mud in which ice crystals had recently formed, in Rock Island, Ill., and


id: 43826
title: The Story of the Hills: A Book About Mountains for General Readers.
author: Hutchinson, H. N. (Henry Neville)
txt: ./txt/43826.txt
cache: ./cache/43826.txt
extension: .txt
mime: text/plain
summary:
  a little observation goes a long way to help them to read mountain In old times people looked with awe upon the mountains, and of the rocks of which mountain chains are composed, in observing higher parts of mountain-ranges the cold is so great that the water that valleys were rents in the rocks of the earth''s crust formed forced their way up from subterranean regions into the rocks forming among the rocks of mountains far away. rock-forming materials brought down to the seas at the present day. for mountains _are_ formed of hard rocks; but at the same time we frequently does, buried in mountain rocks the fossil remains of not all; for in every mountain region we find that the rocks have steep valley, and great masses of hard rock stand out as bold hills crumpling of the rocks of mountains produced, is not at present


id: 52216
title: Glacières; or, Freezing Caverns
author: Balch, Edwin Swift
txt: ./txt/52216.txt
cache: ./cache/52216.txt
extension: .txt
mime: text/plain
summary:
  rock walls is sufficiently high to prevent ice from forming in winter rocks, caves without apparent draughts in summer and containing ice, a small cave or hole containing ice near Mapleton, Pennsylvania, but the Farrandsville Cave as near as is possible, as the ice forms in the caves where the temperatures sink so low, that ice forms. the entrance snow and ice slopes of some of the open pit caves such as neighborhood of glacière caves generally believe that the ice of glacière caves, almost always suggest that to form the ice there must caves where the heavy cold air preserves the ice by remaining pent that ice begins to form in a cave as soon as the temperature of the _Ice Caves_, etc., page 1.)--Mr. Browne observed in 1864 a temperature temperature in the cave so much that the water freezes into ice. Ice near entrance of caves, 152


id: 53063
author: Baker, Ernest A. (Ernest Albert)
txt: ./txt/53063.txt
cache: ./cache/53063.txt
extension: .txt
mime: text/plain
summary:
  Near the entrance in Gough''s Cave a fairly deep hole The great Limestone cavern formed by the action of the swallet streams The Long Hole at Cheddar, high in the cliffs above Gough''s Cave, of the caves in the Peak, in Wookey Hole, and in the cavern of Marble [Illustration: IN THE FIRST CHAMBER, WOOKEY HOLE CAVERN. [Illustration: STALACTITE GROTTO: NEW CHAMBERS, WOOKEY HOLE CAVE. he reached a point nearly 500 feet below the cave mouth, and distant the cave, and a few feet above it is a flood-way, a short, low tunnel, From this chamber the stream quickly descends into the great Water Gough''s, or the Great Cavern, a large body of water wells up at the Cheddar Water than about the stream flowing out of Wookey Hole. steep hole into a large cavern through which the stream runs from the presently into an open passage, 25 or 30 feet high, with the stream

title:
  The Netherworld of Mendip Explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere


id: 39621
title: The Jenolan Caves: An Excursion in Australian Wonderland
author: Cook, Samuel
txt: ./txt/39621.txt
cache: ./cache/39621.txt
extension: .txt
mime: text/plain
summary:
  THE FOSSIL BONE CAVE, THE SPARKLING ROCK, AND THE CRYSTAL of a village and a mountain nine miles north of the caves, and, like the arch are caves running obliquely into the mountain 10, 15, and 20 feet, the roof and small stalagmites on ledges near the floor of the cave, and the floor to the roof of the cave; and seeing that it is about 30 feet At the far end of the cave the floor is covered with little The roof is about 100 feet high, and the sides of the cave are the roof above the Fossil Bone Cave is a rare stalactite about 20 feet The Helena Cave is about 60 yards long, 15 to 20 feet high, and varies Another beautiful feature in the Helena Cave is a formation under a mass the rock floor there was in these caves what looked exactly like a


id: 58361
title: Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia
author: Curzon, Robert
txt: ./txt/58361.txt
cache: ./cache/58361.txt
extension: .txt
mime: text/plain
summary:
  Koords, headed in our days by the great chieftains Beder Khan Bey, round towers, with conical roofs, like old-fashioned pigeon-houses, What the Pasha looked like, and what manner of man he was, it was like every body else in this country, and a long nose and a black best places, over round stones as big as a man''s head, with larger a rich man''s house is prodigious, the turfed roof forming a small "One day passes much like another at Erzeroom, and though there Now it came to pass, once upon a time, that the great of the good old times, I one day proceeded to the citadel to see young bears one day, who lived in our house for some time. A curious episode in the history of Armenia took place in the time The country which was called Armenia in ancient times is now divided


