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Géologie appliquée de l'Algérie. Métallogénie - Hydrogéologie - Agrogéologie
Masson et Cie, 1939, in-8 rel. 1/2 toile bleu (19 x 25), 888 p., coll. du "Centenaire de l'Algérie / Etudes Scientifiques et Mise en valeur", 8 planches h.-t. dont 5 cartes repliées en coul. in-fine, reliure récente, dos muet, très bon état.
Un essai de synthèse sur la géologie appliquée de l'Algérie. Voir le sommaire sur photos jointes.
Géologie Appliquée de L'Algérie - Métallogénie-Hydrogéologie-Agrogéologie
Masson / Collection du centenaire de l'Algérie 1830-1930 - ÉTUDE SCIENTIFIQUE ET MISE EN VALEUR- 1939 - Fort et grand In Octavo broché de 888 pages , bien complets des 8 planches dont 4 cartes dépliantes in fine , trois portrait en manière de frontispice présentant les scientifiques ayant collaboré à l'ouvrage. Bon ensemble . Plats défraîchis , Tampon de l'ingénieur des mines; pagination remarquablement fraîche .Bon et bel ensemble dans un bien convenable état d'usage.
Bon Etat Mise à jour du Samedi 27 Juin 2026. Paiement PayPal immédiat, Mondial Relay pour : France, Allemagne, Autriche, Belgique, Espagne, Italie, Portugal, Luxembourg, Pays-Bas, Pologne (Communiquer votre point ou locker si connu). Une participation supplémentaire peut être demandée pour les colis lourds hors France où les envois compris entre 5 et 25 kg sont dégressifs : 2 à 4 kilogrammes - 7.99 / 5 à 10 kg - 15.99 / 15 -25 kg - 25.99. Certaines de nos collections ( Vian, Céline, Camus (...) peuvent être expédiées en Franco de port. Pour linternational hors Europe (Suisse, Canada, Japon, Etats-Unis, les frais dexpéditions peuvent varier selon le poids (mise à jour : 1 juin 2026).
Les Hautes-Chaumes du FOREZ ou l'histoire des bois et des montagnes pastorales de cette province à l'entour de PIERRE-SUR-HAUTE avec des considérations botaniques, géologiques, historiques, archéologiques, économiques, sylvicoles, agricoles, fromagères, ennuyeuses mais brèves, et une belle image.
Emile Faure Laveur 1907 Montbrison, Emile Faure / Paris, L. Laveur, 1907, 77 p., broché, complet de la photographie et du calque. Couverture insolée et un peu salie. Bon état pour le reste et intérieur bien propre.
Merci de nous contacter à l'avance si vous souhaitez consulter une référence au sein de notre librairie.
Genesi e metamorfosi delle rocce basiche e ultrabasiche nell'ambiente mesozonale dell'orogene pennidico. Studio geologico -petrografico della catena Gaggio-Basal (Cantone Ticino). Diss.
Zurigo 1953, in-8vo, p. 173 à 480 p. (= 306 p.), con 70 fig. brochure originale.
(SLACES, NVVA)
Phone number : 41 (0)26 3223808
Die Stieger Schichten im Westharz
Berlin, 1960 107pp. with 2 folding plates + 2 folding maps loose in rear pocket, 21cm., Doctoral Dissertation (Von der Fakultät für Allgemeine Ingenieurswissenschaften der Technischen Universität Berlin zur Verleihung der akademischen Würde 'Doktor der Naturwissenschaften' genehmigte Dissertation), softcover, text is clean and bright, good condition, W112015
Die Vaulruz-Molasse. Das Kalkgebirge bei Châtel-St.-Denis. Diss.
Freiburg S., St-Paulus 1909, 220x145mm, 52Seiten, broschiert.
5 S/W Photographien, Pour un paiement via PayPal, veuillez nous en faire la demande et nous vous enverrons une facture PayPal
Die Vaulruz-Molasse. Das Kalkgebirge bei Châtel-St.-Denis. Diss. Univ. Freiburg.
Freiburg in der Schweiz, 1909, gr. in-8°, 54 S. mit 6 Fig. + 6 Photogr. Tafeln, Stempel a/d. Titelbl., broschiert.
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Neuere Untersuchungen im Tertiärgebiet am Nordrand der Freiburger Alpen. Diss. Univ. Freiburg.
Bern, Lith. Armbruster Söhne, 1911, in-8°, 46 S., 1 Photogr.-Tafel, Stempel, broschiert.
(SLACES, NVVA)
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On the conditionof Vesuvius in July, 1834.
New Haven, Hezekiah Howe & Co., 1835. 8vo. Contemp. hcalf. Gilt spine. In: ""The American Journal of Science and Arts. Conducted by Benjamin Silliman"". Vol. XXVII. (Entire volume offered). VIII,424 pp,. a. 3 engraved plates. Plates a bit brownspotted. Dana's paper: pp. 281-88.
First appearance of Dana's first paper.""Dana served as an instructor on a U.S. Navy vessel that sailed to the Mediterranean, where he saw Vesuvius in eruption and pursued entomological studies. His account of the eruption in a letter, published by Silliman in the Journal, was Dana’s first scientific paper. In 1834, Dana returned to Yale, where he developed a new mineral classification based on chemistry and crystallography and using Silliman’s cabinet of minerals and his own."" (DSB).The volume contains another notable paper by GIDEON MANTELL ""Notice of the discovery of the remains of the Iguanodon in the Lower Green Sand Formation of the South-east of England. Communcated for this Journal. Pp. 355-360, textillustrations in woodcut.
A new System of Crystallographic Symbols.
New Haven, Hezekiah Howe & Co., 1835. Contemp. hcalf. Spine gilt and with gilt lettering. In ""The American Journal of Science and Arts. Conducted by benjamin Silliman"", Vol. 38 - July, 1835. VII,404 pp. (Entire volume offered). Dana's paper: pp. 250-262 and 1 engraved plate. A few marginal brownspots. Internally clean.
First appearence of Dana' first paper on the classification of minerals which 2 years later became his great work ""A System of Mineralogy"" containing his famous and widely accepted classification system.Poggendorff I, 516.
La géologie mise à la portée de tous ; ses rapports avec la géographie physique et son utilisation pour la recherche des minerais, des combustiles, des engrais et des eaux
, Bruxelles, G.Bothy 1921, 218 + vii pp. avec 178 fig.dans le texte, br., A23232
La Normandie
Paris, Hermann, 1951. 445 g In-8 broché, 241 pp.. Avec 22 figures, 5 cartes, 7 planches et 7 tableaux. Ouvrage de géologie par Louis Dangeard, professeur de géologie et de paléoontologie à l'université de Caen. De la collection de la Géologie régionale de la France. Exemplaire non coupé. Assez rare. . (Catégories : Normandie, Géologie, )
Observations De Géologie Sous-Marine et D'océanographie Relatives à La Manche
Paris et Lyon Ed. Blondel La Rougery 1928 Grand In-8 Ecu 295 pp, envoi de l'auteur, Annales de L'Institut Océanographique, nouvelle série, tome VI, fascicule I. VIII planches hors-texte, 27 figures et XVIII cartes. Dos muet insolé.
Signée par L'auteur Bon Broché à raba
Analyse tectonique de formations précambriennes étude du Nord-Est de la Bretagne - Science géologiques mémoire n°36 1972
C.N.R.S 1972 in4. 1972. Broché.
Bon état couverture assez frottée intérieur propre 5 documents séparés
Exposé sur les marbres de carrières et les marbres reconstitués.
Tours, imp. Deslis, 1899, 1 br., couverture marbrée, 4ème de couverture en partie manquante. in-8 de f.t., titre, 60 pages non coupées, illustrations ;
Geologie der Steinkohlenlager. Erster Band - Erster Teil (2nd ed. 1941!), Zweiter Band, Dritter Band.
1921-1941 3 vols. iv, 317, viii, 582, xi, 682 p., 79, 34, 209 figs, 3 pls, hcloth. Library stamps & number on spine. Missing part 2 of the first volume, but with the scarce third volume. With author's dedication to Dr. Jongmans.
Bibliographie des thèses et mémoires géographiques belges, 1904-1953. Bibliographie Belgica, 3.
Bruxelles, Commission Belge de Bibliographie, 1953. 14 x 21, 35 pp., broché, bon état (couverture défraîchie).
Denkschrift über die Wasserversorgung von Darmstadt : mit einer Übersichtskarte.
Darmstadt : Jonghaus, 1871, gr. in-8vo, 152 S. + gef. lithogr. ÜIbersichtskarte der Umgebung von Darmstadt, Ausgebunden. Umschlag vorne v. Original-Broschüre vorhanden.
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Phone number : 41 (0)26 3223808
"La géologie (Collection ""Que sais-je ?"", n°525)"
Presses Universitaires de France. 2000. In-12. Broché. Etat d'usage, Couv. légèrement passée, Dos fané, Intérieur frais. 127 pages. Quelques illustrations monochromes et en couleurs dans et hors texte.. . . . Classification Dewey : 551-Géologie
"Collection ""Que sais-je ?"", n°525. Classification Dewey : 551-Géologie"
Que sais-je? N° 2862 Les applications de la géologie
Presses Universitaires de France Edition originale Première édition Juin 1994. 1994. In-12. Broché. Bon état, Couv. convenable, Dos satisfaisant, Intérieur frais. 128 pages illustrées de quelques dessins en noir et blanc. . . . Classification Dewey : 551-Géologie
La première encyclopédie de poche fondée en 1941 par Paul Angoulvent, traduite en 43 langues, diffusée, pour les éditions françaises, à plus de 160 millions d'exemplaires, la collection Que sais-je? est l'une des plus importantes bases de données internationnales, construite pour le grand public par des spécialistes. 3800 titres ont été publiés depuis l'origine par 2500 auteurs. Classification Dewey : 551-Géologie
Les roches phosphatées d’Angola.
Lisboa, Ministerio do Ultramar, Junta de Investigaçoes do Ultramar 1956, 250x180mm, 61pages, reliure chagrin. Bel exemplaire.
Cachet de bibliothèque. Pour un paiement via PayPal, veuillez nous en faire la demande et nous vous enverrons une facture PayPal
Story of the Grand Canyon of Arizona. A popular illustrated account of its rocks and origin.
Kansas City, Fred Harvey, sans date. In-8 broché de 74-[6] p., couverture grise imprimée noir et argent.
Illustré de nombreux documents en noir, photographies, cartes... HORAIRE ESTIVAL : DU LUNDI 27 JUILLET AU SAMEDI 21 AOUT NOUS SERONS OUVERTS UNIQUEMENT SUR RENDEZ-VOUS.
LES AMPHIBOLES ET LES MINERAUX ASSOCIES DANS LES LAVES BASALTIQUES DU MASSIF CENTRAL FRANCAIS
COLOGNE UNIVERSITE 1971 COPIE THESE PRESENTEE LE 27 JUILLET 1971 , UNIVERSITE DE CLERMONT-FERRAND POUR OBTENIR LE GRADE DE DOCTEUR DE TROISIEME CYCLE , MENTION PETROGRAPHIE , un volume in-4 broché de 160 pages + annexes , spirale plastique pour le dos , ex-libris , bon exemplaire , RARE . Bon Couverture souple
Notes on the Effects produced by the Ancient Glaciers of Caernarvonshire, and on the Boulders transported by Floating Ice.
London, University of London, 1842. 8vo. In contemporary half calf. In ""The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science"", Vol. XXI. July - December, entire volume offered. Spine with wear and lacking bits of the leather especially affecting front hinge. Leather brittle. Front hindge loose. Exlibris pasted on to pasted down front end-paper. Internally nice and clean. [Darwin's paper:] Pp. 180-88. [Entire volume: viii, 568 pp.].
First appearance of Darwin’s paper on the effects produced by the glaciers of Caernarvonshire. In 1831 Charles Darwin came to Cwm Idwal and failed to perceive the evidence of glaciation there. In 1842, Darwin then went on to describe the glaciation of Cwm Idwal in some detail. He recorded both his first visit with the Cambridge geologist Adam Sedgwick and his second, more aware, visit in his autobiography: “Next morning we started for Llangollen, Conway, Bangor, and Capel Curig. This tour was of decided use in teaching me a little how to make out the geology of a country. Sedgwick often sent me on a line parallel to his, telling me to bring back specimens of the rocks and to mark the stratification on a map. On this tour I had a striking instance of how easy it is to overlook phenomena, however conspicuous, before they have been observed by any one. We spent many hours in Cwm Idwal, examining all the rocks with extreme care, as Sedgwick was anxious to find fossils in them" but neither of us saw a trace of the wonderful glacial phenomena all around us we did not notice the plainly scored rocks, the perched boulders, the lateral and terminal moraines. Yet these phenomena are so conspicuous that, as I declared in a paper published many years afterwards in the ‘Philosophical Magazine’ [Darwin, 1842], a house burnt down by fire did not tell its story more plainly than did this valley. If it had still been filled by a glacier, the phenomena would have been less distinct than they now are. (Darwin, 1887)” “By 1842, not only had Darwin travelled widely (Herbert, 1991) but Agassiz (1840) had published his theory of glaciation. Darwin was also then apprised of the arguments of the geologist William Buckland. Buckland was known for his penchant for eating every variety of animal, a trait which his son inherited (Burgess, 1967: Chapter 1 Chorley et al., 1964: 100–118 see also Lewry, 2008) but he also developed highly significant ideas on glaciation and the limitations of the diluvial theory (Chorley et al., 1964: 207–210). A key realization is that water-lain flood deposits are normally laid down in stratified layers, with the coarser material below the fine, while the glacial deposits are unstratified and mixed in size. Thus, in contrast to his earlier 1831 lack of glacial observation” (Trudgill, Do theories tell us what to see? The 19th-century observations of Darwin, Ramsay and Bonney on glacial features), Darwin wrote: “Guided and taught by the abstract of Dr. Buckland’s memoir ‘On Diluvio-Glacial Phænomena in Snowdonia and the adjacent parts of North Wales’ I visited several of the localities there noticed, and ... I have been enabled to make a few additional observations. Dr. Buckland has stated that a mile east of Lake Ogwyn there occurs a series of mounds, covered with hundreds of large blocks of stone, which approach nearer to the condition of an undisturbed moraine, than any other mounds of detritus noticed by him in North Wales. By ascending these mounds it is indeed easy to imagine that they formed the north-western lateral moraine of a Trudgill 559 Downloaded from ppg.sagepub.com at PENNSYLVANIA STATE UNIV on September 16, 2016 glacier, descending in a north-east line from the Great Glyder mountain. But at the southern end of Lake Idwell the phænomena of moraines are presented, though on a much smaller scale, with perfect distinctness. (From the present paper, p. 180)” Darwin then gives a detailed description of the glacial features: “On entering the wild amphitheatre in which Lake Idwell lies, some small conical, irregular little mounds, which might easily escape attention, may be seen at the further end. The best preserved mounds lie on the west side of the great black perpendicular face of rock, forming the southern boundary of the lake. They have been intersected in many places by streams, and they are seen to consist of earth and detritus, with great blocks of rock on their summits. They at first appear quite irregularly grouped, but to a person ascending any one of those furthest from the precipice, they are at once seen to fall into three (with traces of a fourth) narrow straight linear ridges. The ridge nearest the precipice runs someway up the mountain, but the outer one is longer and more perfect, and forms a trough with the mountain-side, from 10 to 15 feet deep. On the eastern and opposite side of the head of the lake, corresponding but less developed mounds of detritus may be seen running a little way up the mountain. It is, I think, impossible for any one who has read the descriptions of the moraines bordering the existing glaciers in the Alps, to stand on these mounds and for an instant to doubt that they are ancient moraines nor is it possible to conceive any other cause which could have abruptly thrown up these long narrow steep mounds of unstratified detritus against the mountain-sides. (From the present paper, p. 180)”
