mv: ‘./input-file.zip’ and ‘./input-file.zip’ are the same file Creating study carrel named classification-GB-gutenberg Initializing database Unzipping Archive: input-file.zip creating: ./tmp/input/input-file/ inflating: ./tmp/input/input-file/14012.txt inflating: ./tmp/input/input-file/18562.txt inflating: ./tmp/input/input-file/17354.txt inflating: ./tmp/input/input-file/14999.txt inflating: ./tmp/input/input-file/33760.txt inflating: ./tmp/input/input-file/43826.txt inflating: ./tmp/input/input-file/52216.txt inflating: ./tmp/input/input-file/53063.txt inflating: ./tmp/input/input-file/39621.txt inflating: ./tmp/input/input-file/58361.txt inflating: ./tmp/input/input-file/metadata.csv caution: excluded filename not matched: *MACOSX* === DIRECTORIES: ./tmp/input === DIRECTORY: ./tmp/input/input-file === metadata file: ./tmp/input/input-file/metadata.csv === found metadata file === updating bibliographic database Building study carrel named classification-GB-gutenberg FILE: cache/33760.txt OUTPUT: txt/33760.txt FILE: cache/14999.txt OUTPUT: txt/14999.txt FILE: cache/43826.txt OUTPUT: txt/43826.txt FILE: cache/17354.txt OUTPUT: txt/17354.txt FILE: cache/58361.txt OUTPUT: txt/58361.txt FILE: cache/52216.txt OUTPUT: txt/52216.txt FILE: cache/39621.txt OUTPUT: txt/39621.txt FILE: cache/14012.txt OUTPUT: txt/14012.txt FILE: cache/53063.txt OUTPUT: txt/53063.txt FILE: cache/18562.txt OUTPUT: txt/18562.txt 33760 txt/../pos/33760.pos 33760 txt/../wrd/33760.wrd 33760 txt/../ent/33760.ent === file2bib.sh === id: 33760 author: Udden, Johan August title: Fossil Ice Crystals: An Instance of the Practical Value of "Pure Science" date: pages: extension: .txt txt: ./txt/33760.txt cache: ./cache/33760.txt Content-Encoding ISO-8859-1 Content-Type text/plain; charset=ISO-8859-1 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 2 resourceName b'33760.txt' 14999 txt/../pos/14999.pos 14999 txt/../ent/14999.ent 14999 txt/../wrd/14999.wrd === file2bib.sh === id: 14999 author: Pemble, William title: A Briefe Introduction to Geography date: pages: extension: .txt txt: ./txt/14999.txt cache: ./cache/14999.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 4 resourceName b'14999.txt' 39621 txt/../wrd/39621.wrd 39621 txt/../pos/39621.pos 17354 txt/../pos/17354.pos 39621 txt/../ent/39621.ent 17354 txt/../wrd/17354.wrd 58361 txt/../pos/58361.pos 53063 txt/../pos/53063.pos 53063 txt/../wrd/53063.wrd 17354 txt/../ent/17354.ent 58361 txt/../wrd/58361.wrd 58361 txt/../ent/58361.ent 43826 txt/../pos/43826.pos 53063 txt/../ent/53063.ent 52216 txt/../pos/52216.pos 52216 txt/../wrd/52216.wrd 43826 txt/../wrd/43826.wrd 43826 txt/../ent/43826.ent === file2bib.sh === id: 39621 author: Cook, Samuel title: The Jenolan Caves: An Excursion in Australian Wonderland date: pages: extension: .txt txt: ./txt/39621.txt cache: ./cache/39621.txt Content-Encoding ISO-8859-1 Content-Type text/plain; charset=ISO-8859-1 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 3 resourceName b'39621.txt' 14012 txt/../pos/14012.pos 52216 txt/../ent/52216.ent 14012 txt/../wrd/14012.wrd 14012 txt/../ent/14012.ent === file2bib.sh === id: 17354 author: Owen, Luella Agnes title: Cave Regions of the Ozarks and Black Hills date: pages: extension: .txt txt: ./txt/17354.txt cache: ./cache/17354.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 5 resourceName b'17354.txt' 18562 txt/../pos/18562.pos 18562 txt/../wrd/18562.wrd === file2bib.sh === id: 53063 author: Baker, Ernest A. (Ernest Albert) title: The Netherworld of Mendip Explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere date: pages: extension: .txt txt: ./txt/53063.txt cache: ./cache/53063.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 5 resourceName b'53063.txt' === file2bib.sh === id: 58361 author: Curzon, Robert title: Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia date: pages: extension: .txt txt: ./txt/58361.txt cache: ./cache/58361.txt Content-Encoding ISO-8859-1 Content-Type text/plain; charset=ISO-8859-1 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 4 resourceName b'58361.txt' 18562 txt/../ent/18562.ent === file2bib.sh === id: 43826 author: Hutchinson, H. N. (Henry Neville) title: The Story of the Hills: A Book About Mountains for General Readers. date: pages: extension: .txt txt: ./txt/43826.txt cache: ./cache/43826.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 7 resourceName b'43826.txt' === file2bib.sh === id: 52216 author: Balch, Edwin Swift title: Glacières; or, Freezing Caverns date: pages: extension: .txt txt: ./txt/52216.txt cache: ./cache/52216.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 8 resourceName b'52216.txt' === file2bib.sh === id: 14012 author: Browne, G. F. (George Forrest) title: Ice-Caves of France and Switzerland date: pages: extension: .txt txt: ./txt/14012.txt cache: ./cache/14012.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 11 resourceName b'14012.txt' === file2bib.sh === id: 18562 author: Shaler, Nathaniel Southgate title: Outlines of the Earth's History: A Popular Study in Physiography date: pages: extension: .txt txt: ./txt/18562.txt cache: ./cache/18562.txt Content-Encoding UTF-8 Content-Type text/plain; charset=UTF-8 X-Parsed-By ['org.apache.tika.parser.DefaultParser', 'org.apache.tika.parser.csv.TextAndCSVParser'] X-TIKA:content_handler ToTextContentHandler X-TIKA:embedded_depth 0 X-TIKA:parse_time_millis 10 resourceName b'18562.txt' Done mapping. Reducing classification-GB-gutenberg === reduce.pl bib === id = 18562 author = Shaler, Nathaniel Southgate title = Outlines of the Earth's History: A Popular Study in Physiography date = pages = extension = .txt mime = text/plain words = 146536 sentences = 5038 flesch = 63 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 cache = ./cache/18562.txt txt = ./txt/18562.txt === reduce.pl bib === id = 33760 author = Udden, Johan August title = Fossil Ice Crystals: An Instance of the Practical Value of "Pure Science" date = pages = extension = .txt mime = text/plain words = 3095 sentences = 186 flesch = 71 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 cache = ./cache/33760.txt txt = ./txt/33760.txt === reduce.pl bib === id = 39621 author = Cook, Samuel title = The Jenolan Caves: An Excursion in Australian Wonderland date = pages = extension = .txt mime = text/plain words = 42254 sentences = 2030 flesch = 72 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 cache = ./cache/39621.txt txt = ./txt/39621.txt === reduce.pl bib === id = 53063 author = Baker, Ernest A. (Ernest Albert) title = The Netherworld of Mendip Explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere date = pages = extension = .txt mime = text/plain words = 55469 sentences = 2786 flesch = 75 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 cache = ./cache/53063.txt txt = ./txt/53063.txt === reduce.pl bib === id = 14012 author = Browne, G. F. (George Forrest) title = Ice-Caves of France and Switzerland date = pages = extension = .txt mime = text/plain words = 103583 sentences = 3870 flesch = 70 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 cache = ./cache/14012.txt txt = ./txt/14012.txt === reduce.pl bib === id = 17354 author = Owen, Luella Agnes title = Cave Regions of the Ozarks and Black Hills date = pages = extension = .txt mime = text/plain words = 51780 sentences = 1912 flesch = 66 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 cache = ./cache/17354.txt txt = ./txt/17354.txt === reduce.pl bib === id = 58361 author = Curzon, Robert title = Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia date = pages = extension = .txt mime = text/plain words = 56868 sentences = 2239 flesch = 69 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 cache = ./cache/58361.txt txt = ./txt/58361.txt === reduce.pl bib === id = 52216 author = Balch, Edwin Swift title = Glacières; or, Freezing Caverns date = pages = extension = .txt mime = text/plain words = 82501 sentences = 5340 flesch = 82 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 cache = ./cache/52216.txt txt = ./txt/52216.txt === reduce.pl bib === id = 14999 author = Pemble, William title = A Briefe Introduction to Geography date = pages = extension = .txt mime = text/plain words = 13284 sentences = 1075 flesch = 88 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 cache = ./cache/14999.txt txt = ./txt/14999.txt === reduce.pl bib === id = 43826 author = Hutchinson, H. N. (Henry Neville) title = The Story of the Hills: A Book About Mountains for General Readers. date = pages = extension = .txt mime = text/plain words = 72224 sentences = 3326 flesch = 74 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 cache = ./cache/43826.txt txt = ./txt/43826.txt Building ./etc/reader.txt 52216 14012 18562 18562 17354 39621 number of items: 10 sum of words: 627,594 average size in words: 62,759 average readability score: 73 nouns: ice; water; cave; feet; earth; time; way; air; rock; surface; part; rocks; place; caves; floor; side; meters; sea; snow; page; mountain; point; entrance; temperature; fact; miles; day; work; winter; mountains; distance; action; stream; end; roof; bottom; heat; man; summer; years; mass; height; °; formation; sun; wall; depth; level; parts; year verbs: is; was; are; be; have; been; were; had; has; found; being; made; formed; see; find; seen; called; said; known; do; covered; came; brought; come; make; did; having; take; taken; reached; does; give; seems; took; go; left; cut; know; form; described; say; comes; appear; seemed; become; went; given; filled; show; told adjectives: great; other; many; small; such; large; little; same; more; long; high; first; few; cold; old; several; lower; much; considerable; deep; certain; greater; good; present; natural; different; beautiful; general; whole; own; upper; white; important; various; last; wide; most; volcanic; low; interesting; solid; narrow; fine; higher; due; clear; vast; open; short; possible adverbs: not; so; very; up; down; only; about; more; now; out; then; as; most; also; away; here; well; far; thus; even; much; still; however; there; almost; often; on; probably; again; off; in; once; first; yet; perhaps; sometimes; too; long; soon; nearly; just; generally; never; ever; therefore; rather; together; less; indeed; always pronouns: it; we; they; he; i; its; their; his; them; our; us; my; him; me; you; itself; her; himself; she; themselves; one; ourselves; your; myself; thy; herself; mine; yourself; thee; theirs; ours; oneself; appearance.--his; £600; windhole; wane; vp; vnto; treateth; thyself; jenolan"--that; je; ib; hills,--the; highlander,--they; dufour; ce; by:--; --ice; ''em proper nouns: _; cave; de; mr.; m.; footnote; vol; professor; la; hole; limestone; .; dr.; i.; north; s.; glacière; alps; c.; a.; ice; new; f.; e.; south; river; cavern; mountains; st.; august; great; part; chapter; england; fugger; les; july; eishöhlen; lake; |; america; valley; wookey; europe; nature; hills; caves; ii; photo; pasha keywords: illustration; cave; water; time; rock; great; foot; sea; north; new; mr.; form; earth; chapter; south; professor; place; limestone; july; ice; glacière; georges; find; europe; england; christian; august; wookey; wind; wells; way; wales; vesuvius; turks; turkish; turkey; trebizond; thury; texas; temperature; sydney; switzerland; surface; sunne; sultan; stalactite; st.; spring; shah; september one topic; one dimension: ice file(s): ./cache/14012.txt titles(s): Ice-Caves of France and Switzerland three topics; one dimension: ice; feet; earth file(s): ./cache/14012.txt, ./cache/58361.txt, ./cache/18562.txt titles(s): Ice-Caves of France and Switzerland | Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia | Outlines of the Earth''s History: A Popular Study in Physiography five topics; three dimensions: ice cave meters; earth water great; mountains great earth; cave feet caves; cave feet water file(s): ./cache/14012.txt, ./cache/18562.txt, ./cache/58361.txt, ./cache/53063.txt, ./cache/17354.txt titles(s): Ice-Caves of France and Switzerland | Outlines of the Earth''s History: A Popular Study in Physiography | Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia | The Netherworld of Mendip Explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere | Cave Regions of the Ozarks and Black Hills Type: gutenberg title: classification-GB-gutenberg date: 2021-05-28 time: 22:05 username: emorgan patron: Eric Morgan email: emorgan@nd.edu input: classification:"GB" ==== make-pages.sh htm files ==== make-pages.sh complex files ==== make-pages.sh named enities ==== making bibliographics id: 53063 author: Baker, Ernest A. (Ernest Albert) title: The Netherworld of Mendip Explorations in the great caverns of Somerset, Yorkshire, Derbyshire, and elsewhere date: words: 55469 sentences: 2786 pages: flesch: 75 cache: ./cache/53063.txt txt: ./txt/53063.txt 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 id: 52216 author: Balch, Edwin Swift title: Glacières; or, Freezing Caverns date: words: 82501 sentences: 5340 pages: flesch: 82 cache: ./cache/52216.txt txt: ./txt/52216.txt 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: 14012 author: Browne, G. F. (George Forrest) title: Ice-Caves of France and Switzerland date: words: 103583 sentences: 3870 pages: flesch: 70 cache: ./cache/14012.txt txt: ./txt/14012.txt 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: 39621 author: Cook, Samuel title: The Jenolan Caves: An Excursion in Australian Wonderland date: words: 42254 sentences: 2030 pages: flesch: 72 cache: ./cache/39621.txt txt: ./txt/39621.txt 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 author: Curzon, Robert title: Armenia: A year at Erzeroom, and on the frontiers of Russia, Turkey, and Persia date: words: 56868 sentences: 2239 pages: flesch: 69 cache: ./cache/58361.txt txt: ./txt/58361.txt 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 id: 43826 author: Hutchinson, H. N. (Henry Neville) title: The Story of the Hills: A Book About Mountains for General Readers. date: words: 72224 sentences: 3326 pages: flesch: 74 cache: ./cache/43826.txt txt: ./txt/43826.txt 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: 17354 author: Owen, Luella Agnes title: Cave Regions of the Ozarks and Black Hills date: words: 51780 sentences: 1912 pages: flesch: 66 cache: ./cache/17354.txt txt: ./txt/17354.txt 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 author: Pemble, William title: A Briefe Introduction to Geography date: words: 13284 sentences: 1075 pages: flesch: 88 cache: ./cache/14999.txt txt: ./txt/14999.txt 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: 18562 author: Shaler, Nathaniel Southgate title: Outlines of the Earth''s History: A Popular Study in Physiography date: words: 146536 sentences: 5038 pages: flesch: 63 cache: ./cache/18562.txt txt: ./txt/18562.txt 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: 33760 author: Udden, Johan August title: Fossil Ice Crystals: An Instance of the Practical Value of "Pure Science" date: words: 3095 sentences: 186 pages: flesch: 71 cache: ./cache/33760.txt txt: ./txt/33760.txt 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 ==== make-pages.sh questions ==== make-pages.sh search ==== make-pages.sh topic modeling corpus Zipping study carrel