A system of mineralogy
- Autor
- Jameson, Robert
- Erscheinungsort
- Edinburgh
- Bandzählung
- 1
- Erscheinungsdatum
- 1816
- Umfang
- XIX, 537 S., V gef. Taf.
- Sprache
- Englisch
- Signatur
- VI 335 8. (1)
- Vorlage
- Universitätsbibliothek Freiberg
- Digitalisat
- Universitätsbibliothek Freiberg
- Digitalisat
- SLUB Dresden
- Lizenz-/Rechtehinweis
- Public Domain Mark 1.0
- URN
- urn:nbn:de:bsz:14-db-id4776996772
- PURL
- http://digital.slub-dresden.de/id477699677
- OAI
- oai:de:slub-dresden:db:id-477699677
- SLUB-Katalog
- 477699677
- Sammlungen
- Projekt: Bestände der Universitätsbibliothek Freiberg
- LDP: UB Freiberg Druckschriften
- Ausgabe
- Second Edition
- Strukturtyp
- Band
- Parlamentsperiode
- -
- Wahlperiode
- -
- Titel
- VI. Quartz Family
- Digitalisat
- SLUB Dresden
- Strukturtyp
- Kapitel
- Parlamentsperiode
- -
- Wahlperiode
- -
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Mehrbändiges Werk
A system of mineralogy
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Band
Band 1
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- Einband Einband -
- Titelblatt Titelblatt III
- Kapitel Preface V
- Kapitel List Of Works Quoted in this Treatise, and of the ... IX
- Inhaltsverzeichnis Inhaltsverzeichnis XV
- Kapitel I. Diamond Family 1
- Kapitel II. Zircon Family 15
- Kapitel III. Ruby Family 23
- Kapitel IV. Schorl Family 48
- Kapitel V. Garnet Family 107
- Kapitel VI. Quartz Family 142
- Kapitel VII. Pitchstone Family 270
- Kapitel VIII. Zeolite Family 290
- Kapitel IX. Azurestone Family 337
- Kapitel X. Felspar Family 348
- Kapitel XI. Clay Family 405
- Kapitel XII. Clay-Slate Family 431
- Kapitel XIII. Mica Family 449
- Kapitel XIV. Lithomarge Family 466
- Kapitel XV. Soapstone Family 480
- Kapitel XVI. Talc Family 503
- Abbildung Plate I -
- Abbildung Plate II -
- Abbildung Plate III -
- Abbildung Plate IV -
- Abbildung Plate V -
- Einband Einband -
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Band
Band 1
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- Titel
- A system of mineralogy
- Autor
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Volltext Seite (XML)
FLINT. m Chemical Characters. before the blow-pipe, it is infusible without addition. Constituent Parts. Silica, 98.0 98. Lime, 0.50 0.50 Alumina, 0.25 0.25 Oxide of Iron, 0.25 0.25 Loss, 1.00 1. 100 loo Klaproth, Beit. b. i. s. 46. Vauquelin, Journ. de Mines, n. xxxiii. p. 702. Physical Characters. When two pieces of flint are rubbed together in the *Wk, they phosphorise very much, and emit a peculiar •niell. Georrnostic Situation. © !• It occurs in primitive, transition, flcetz, and alluvial tocks. In primitive and transition rocks, it occurs in Metalliferous and agate veins. The metalliferous veins ^°ntain in some instances ores of silvet or of cobalt, ln others ores of iron; and the agate veins are com posed of flint, calcedony, jasper, amethyst and quartz. n floetz countries, where this mineral occurs in great- e *t abundance, it is found in sandstone, limestone, chalk, “Ml amygdaloid. The sandstone is that variety known Under the name of Puddingstons: the limestone is one of the newer floetz rocks, in which the flint appears in °ds, imbedded masses, and veins: in chalk' it occurs N 3 in
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