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Trailer The Lion King. The Lion King CA. Lion King Trailer Canada 2. Watch Trailer. Official Teaser Trailer. Clip Hollywood's Shared History with Broadway. Weekend Box Office: Sept. Weekend Box Office: July 26 to Weekend Box Office: July 19 to Photos Top cast Edit. Donald Glover Simba as Simba voice. Seth Rogen Pumbaa as Pumbaa voice.


Chiwetel Ejiofor Scar as Scar voice. John Oliver Zazu as Zazu voice. James Earl Jones Mufasa as Mufasa voice. John Kani Rafiki as Rafiki voice. Alfre Woodard Sarabi as Sarabi voice. Penny Johnson Jerald Sarafina as Sarafina voice.


Keegan-Michael Key Kamari as Kamari voice. Florence Kasumba Shenzi as Shenzi voice. Billy Eichner Timon as Timon voice. Jon Favreau. More like this. Watch options. Storyline Edit. Mufasa prepares Simba to be the next king of the jungle. Au plan national a. Sources publiques a. Les ceurs erganisls ne sent d'aucune utilitl peur les clubs. Il suffisait de refuser la pluralitl fSdlrale.


La selutien actuelle maintient un esprit de cempltivit! Les meniteurs natienaux apparaissent cemmt des super meniteurs, privillgils par le tarif de rerabsursement. Ceci sorait rendu possible par l'attribution de mandats aux groupes locaux. CF archives chez djvars? On pourra consulter aussi les Chercheurs de la Wallonie.


Teus les belges ne parlaient donc pas. Au plan. Stereophotography makes possible to present the space expressively even in the situation, when for the natural vision it is quite impossible. Certainly, the procedure of every photo must be individually adapted to the object; so the stereocameras with two objectives are not suitable, bevouse their base is not variable. Methodical rules of this technic for karstic documentation are presented.


The third dimension is presented only indirectly and percepted subjectively; correctly often only by the author of the photo and by those people who know the object personally. Another observer can make his own incorrect picture. Man often completes the absent dimension with reminiscence of similar objects, that he has seen before, if the object of the image is not conform with the precedents of his mind, or the mind has no precedent, the'image he forms is often false, or the photo may be spatial y quits unintelligible.


When the distance is longer, the perception is quite flat and the distance is estimateabls only indirectly. But defocusing reduces the basic factographical function of photography and is not suitable for documentation that needs presentation of maximal quantity of information.


Sfareophoto is a pair of photos, made from two different positions. The difference between the two parts of stereoimage is of the same character as the difference between the images perceived by left and right eye.


The main factor for realization of a perfect stereophato is a determination of an optima] base. The base is a distance between the two positions of the camera, perpendicular to the optic axis of the objective. So it seems that this natural eye-base is universally optimal. This opinion, which is very popular, is a mistake. For the documentation of karst the optimal base changes its magnitude from a few millimetres to hundreds of metres.


An important result is that the stereocameras with two objectives are not goad for universal use; they are useful only for moving objects. For karst, every type of standard camera is better.


It does not matter if the pair of photos is not made simultaneously. Spatial effect of the stereoimage changes with the change of the base. When the base limits to zero the effect limits to normal two-dimensionsal photography or the natural view to a very long distance.


Enlarging the base makes the perception of space more expressive, and the discrimination of a small difference of the distance makes it easier. It makes a spatial view on a very large and distant object possible, which we see only as a flat scene. Stereoimage of a far landscape, made by using a big base, is impressive like a view from a short distance on a small mode] a plastic relief map.


Enlargement of the base is, of course, limited. The main limiting effect is duplication. The eyes feel the view unpleasantly with strain. Parallactic angle is an angular magnitude of the base in the place of the object. Parallactic difference an important parameter of the stereophoto, is the differende between the parallax of the nearest foreground and farthest background see also picture 1. Q2; cotg is about 50, Maximal displacement on the negatives is consequently 0.


The magnitude of the maximal acceptable displacement on negative is the same also for wide-angle objectives or teleobjectives because the system of presentation is universal so the maximal acceptable parallactic difference angle is inversely proportional to the focal length of the objective.


It needs so large a base that the perspective of the left and right image is so different that the parts cannot join in the stereoscope. The same situation can also appear in stereomacrophotography. When we do not want to diminish the base and so the expressivity, we can diminish the perspective distortion difference by using an objective with longer focal distance.


The base must be then proportionally larger. Far practice it is possible to divide karstic objects into three main types: 1. Without a far background for example the subterranean documentation: a natural eye base about 6 cm is usual without variations of order. Very flat objects structural studies : relatively large base even of the same order as the magnitude of the object danger of the perspective difference depends on the focal length of the objective. To this type belongs also stereomacrophotography.


For norma] foca! OF 0B 1 where OF is the distance abjective foreground, 03 is the distance from objective to background. O F 2 A simple arrangement of relalior l far another focal length is not possible. For the base there are three basic alternatives: 1. E is a point excessively proximate, that we must eliminate from the scene, or diminish the base. When the base is the same, ws can accept this point E, when wide-angle objective with short focus is applied; the displacement E'A' is smaller than critical.


When the point E is eliminated, the base for short focus can be larger. The base in this case is constant , but the distance from the main object OF is directly proportional to focal length. The case without configuration of separate formations in foreground and background, but only one flat object see picture 3 : The distance from the object and the base also are directly proportional to the focal length.


The systems for demonstration of the stereoimages can be divided into these groups: a Direct-vision stereoscopes for photos or dia slides b Mirror stereoscopes very serviceable and the only possibility for using enlarged photos of unlimited size; images of the stereapair can be used separately also. Everybody must have his own polarizing spectacl e s. A detailed description of the demonstration systems is available in photographic literature.


Lits s. Photos de l'auteur 2,4,5,6,7 et de G. PAGE 25 P? De 30 I 35 mitres de prefendeur au contraire privaient les cavltls mixtes eu bien horizontales.


La ferme des dslines ne varie pas excessivement. Carta gealagica d 1 Italia, fag H s 47 Brescia. Rev, Glagr. PR,, Cans. Atti Csnv. Massen td. September in Laibach abgehalten. Ober das Ergebnis der Beratungen haben H.


Trimmel und H. Fink, H. Paloc und M. Vianello besonders zu danken. Prosanto quindi una proposta; che il Congresso noraini una Commissione internazionale con un buen numero di rappressr. Inoltre faccio voti che ogni sodalizio, anche regionale o provinciale, tenga una accurata cronaca delle sus. Vedi anche : P. Anno Genova, , pag. E inoltre: P.


Man arbeitet im Laufe der Messungen in den drei Dimensionen des Raumes, deshalb ist es netwendig, auch in drei Dimensienen darzustellen. Abmessungsbl att 2. Tepographisches Blatt a. Pcajsktisnsgrundriss b.


Bleckabschnitt d. Auf dem Vermessungsblatt gibt man die palygsnen Punkte an, die pelyganen Linien, die Stellen der Querschnitte mit Daten. Der Zweck des Vermessungsblattes ist die Darstellung und Dekumentatien der vom Kartierenden aufgenommenen Angaben zusammen mit dem Vermessungsprotekel 1. Felsgestein, Ten, Ichutt usw. Mit der Angabe letzterer kann man die etwaigen Fehler in den bezeichneten Instrumenten finden. Dies zu vermeiden, ist eine gute Hethode die Darstellung der Beschaffenheit des Gesteins entlang der Kenturlinien.


Cio era possibile per il li v eils medio non eccessivantante impegnativo dells esplorazioni in Italia. II CiN. Gli appartsnenti alla Sezione Speleologlca del Csfl.


Smangsno da ri s olvers divers! Si prefer! After examining the Organisas dealing with Speleology, the A. The Italian bibliography about the subject concludes the work. L'attiviti speleologica, prima delle'ultimo cenflitto mondiale, costituiva in Italia un fatts localizzate nelle regioni car siche abitade dalle popolazioni pirt evolute, quale ad esempia la parte di Venezia Giulia gravitants su Trieste. In un suo lavoro del , eseguito per l'E. Nell'estate G. Di contro a costero, stanno le schiere degli speleologi seri e preparati, che senza alcun compensa compiono anche lungho esplorazioni coscienzisse, e trascorrono pei moite ore a tavolino per la elaborazione, pure gratuita, dei dati raccol ti e per la stesura della relazione.


Per quanto si riferisce alla speleologia di livello univers! Qortani si veda su "Ene. Esiste infatti ormai da tempo una "spelea-divulgazione", quale viene effettuata da giornalisti pid o meno competent! Esiste infine uno "speleo-escursianismo", del tutto occasionale, che nei riguardi della salvaguardia delle bellezze natural!


Genova Biblioteca di Speleologia 1st. Badin A. Bertarell i Brea L. Capella C. Caselli C. Fureddu A. Ghidini G. Ghidini 3. Laeng G. Lioy P. Parenzan P Pavan M. Perca G. Scatti P. Segre A. Bari, Milano, Traduz. Boegan E. Mil ano, "Le caverne de! Finale" Bordighera, F. Belle caverne" La Scuola edi t rice-3rescia, Studi Liguri Bordighsra, Gruppo Spel. CAI Genova,.


Brescia, Torino, Lui di seguito, vengono elencati i periodic! Walter Maucci-Trieste. Pisa, Via 3. Anelli: continua la testata della rivista fondata a Postumia ed oggi pubblicata a Castellana Grotte "L'Universo", Bell 1 1 s t!


Sen maggiore potrebbe essere la collaborazione fra. Barro-Roma, Via Aldrovandi Si stampa a Como Via Mentana, 22 , dove venne fendato nel da S. Ricordiamo : "Speleologia lombarda" di M. DeMatteis e C. Contributi di P. Si pubblica a Bologna, Via Indipendanza D'Azegl 1 o, Diversi altri Gruppi Speleologici pubblicano lavori anche di un certo rilievo in fascicoli ciclostilati, quali il Gruppe Speleologies Versiliese e l'Unione speleologica Bolognese.


It works by the reflection of acustic not seismic waves. The results are recorded by a magnetic tape. Das einfachste Mittel ist das Ansetzen von Bohrungen. Was jedoch meist den Einsatz von Bohrungen verbietet, ist die Aufwendigkeit des Verfahrens. Eine weitere Methode sind die geoelektrischen Sondierungen. Der Nachweis der refraktierten und reflektierten Well enfronten erfolgt mittels empfindlicher Mikrofone Geophone, Seifmometer ihre Auszeich. Gemessen werden die Laufzeiten der Wellen, fronten.


Ein solcher Schwinger, der also fest an den Boden gekoppelt ist, sendet praktisch Kugelwellenfronten in das Gestein. Normalerweise wird jedoch beim Geosonar ein Luftschall schwingen, also im Grunde ein Lautsprecher hoher Leistung verwandt. Die Schallquelle ist damit in das Energiemaximum abgebildet und wiederum fest an den Boden angekoppel t. Leider ist das ein Ausnahmefall.


Das tiefste von uns in der Praxis vermessene Echo stammte aus einer Tiefe von etwa 60 Metern. Ein solches Bild kann automatisch vom Geasonar erzeugt werden und liefert ganz erstaunliche Schnittbilder des Untergrundes. Nichtsdestoweniger ist auch beim Geosonar die Auswertung der Lotungen, die auf Magnetband gespeichert werden und an einem Oszillografen zur Messung kommen, eine sehr aufwendig!


Alb Feststellung der Kalktuff-Untergrenze. Franke 3 P. Henne, B. Krauthausen 4 P. Krauthausen 5 K. Bleich 6 H. Henne und 8. Berb Dt. Vereine, die sich z. Wird aber eine solche zentrale Sammlung der Forschungsergebnisse, wie es z. Es sind dies 1. Wie schwierig hat es doch auch z.


Eine der schwierigsten, aber auch wichtigsten Aufgaben ist es, besonders junge Amateure zur Aufzeichnung reiner Beobachtungstatsachen hinzulenken. Was die Richtigkeit der Angaben betrifft, muss man sich freilich auf die sicher vorhandene Ehrlichkeit der Forscher verlassen. Wenn praktisch den Zeitraum einer Generation hindurch mit ganz kleinen Schwankungen immer ca. Gruber bis , sowie seither Herrn Oberferstrat Dipl.


Der Blattschnitt nimmt auf das Landes-Keerdinatennetz Bezug. Akten des 3. II, Wien , 3. Trimmei u. Organisation der Arbeit der Kommission; 2. Das Sekretariat der Kommission hat damit begonnen, die gesammelten Daten in einer Kartei auszuwerten. DoS ist 7 3. Schauberger und H. Klappacher und H.


Morocutti, Verbandsexpedition ins Bergeralpei Tennengebirge. Trimmel Red. Wien , Akten des V. Deux oeuvres importantes de A.


Brodar begann mit intensiven Grabungen und setzte sie bis fort. Man versucht auch bei uns. Nach verschiedenen unzureichenden Planungen sucht man nun das Wasser des unter! Im Winter kann z. Etage versinkt, in den Quellen der Vipava wieder zutage tritt Interessant ist hier die Inversion der Temperaturen, mit der auch eine Umkehrung der Pf I anzenweil t verbunden ist.


B' e c k beschrieben 35 , neuerdings aber von Anton Melik 36 und Franz H r i b a r 37 aufs neue untersucht worden.


Hehrere unsererXExpeditionen reduzierten diese Zahl wiederholt und blieben zuletzt bei m stehen Viele Tonnen von Eis versperren das weitere Vordringen.


Es ist dies die Ihre Erforschung wird fortgesetzt. Der Mittelpunkt dieser Fauna befindet sich jetzt etwa bei den Plitvicer Seen, also mitten in Korati e n. PAGE 66 2. Ljubjana 1 Serko, A. Ljubljanica engl. Ibid, 23, , Ljubljana. In mehreren Sprachen und Auflagen; 6 dt. Pliocenska Pivka engl. Kraska polja Slovenije v pleistocenu frz. Slovenija I, 2. Beialov spodmol pri Postojni ponovno zatocWife ledenodobnega cloveka. Iz Betalovega spodmola pri Postojni, Varstvo spcmenikov 2, PI eistocenski sediment!


Acta carsologica IV, Cpp,j kal, nova paleolitska postaja v Slovenskem Primorju dt. H a b i tf, 1 Crni potok in Lekinka v sistemu podzemel jskega odtoka iz Pivske kotline engl. Nase jame 8, Acta carsologica I! Proteus 22, 8, Nase jame 2,. Ljubljana 1 Gams, I. Ill, , Ljubljana Ljubl jana Ibid, Ljubljana Jenko, F. Ill, Ljubl jana 1 Nase jame 10, 61] Gospodaric, R. Habe, Zelske jame zacetek jamskega turizma v cerknfski obcini.


Habe, F. Hribar S i fren, M. Mitt, d. Wien, Lippertova in Najdena jama frz. Nase jameiS,. Nova odkritja v Najdeni jami. Acta carsologica 5. Velika in Mala ledena jama v Trnovskem,gozdu. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent.


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