volcanic wines types of volcano - wein-welten · 2019. 2. 4. · their eruptions are characterized...

1
TYPES OF VOLCANO HAWAIIAN STROMBOLIAN VULCANIAN PELEAN PLINIAN Characterized by lows of very luid basaltic lava. Explosions are limi- ted, creating gushes of incandescent lava. Basaltic plateaux may be formed when the lava emerges from lateral issures. The form of the volcano is fairly lat because of the extreme luidity of the lava, which lows even when the slopes are not very steep. Apart from active volcanoes in Hawaii and in Iceland, volcanoes of this type are to be found in the areas of Soave and the Lessini Mountains, but these have been inactive for at least 40 million years. The lava in such cases is rich in gas and rather viscous, so that it forms blockages in the crater, thus creating more powerful explosions. Here outlows of lava alternate with pyroclastic surges. Usually these volcanoes have more accentuated slopes. (Example: Stromboli). These volcanoes emit lava that is very viscous and contains little gas, so that they generate powerful explosions, with emissions of gas and ash. Their form is the typical one of cones of ash created by several strata of pyroclastic emissions. (Example: Etna). The formation typical of Mount Pelée in Martinique. The lava is so viscous that it solidiies even inside the crater. Blockages are crea- ted that cause very violent explosions, with the emission of burning clouds (“nuées ardentes”) that descend along the sides of the vol- cano. Here eruptions are extremely explosive, usually following long pe- riods of inactivity. Indeed, the crater is usually obstructed by solid lava. Their eruptions are characterized by tall volcanic cones with descending burning clouds. This generates volcanic chimneys and calderas caused by the collapse of the entire structure of the volca- no. (Example: Vesuvius). DURELLA 450 ha LESSINI DURELLO LESSINI DURELLO DOC, MONTI LESSINI GARGANEGA 1.200 ha GAMBELLARA GAMBELLARA, GAMBELLARA CLASSICO, GAMBELLARA CLASSICO VIN SANTO, RECIOTO DI GAMBELLARA DOCG CAMPI FLEGREI CODA DI VOLPE, FALANGHINA, GRECO 160 ha VESUVIO FORASTERA, BIANCOLELLA 130 ha ISCHIA MALVASIA DI LIPARI, CORINTO, GRILLO, CATARRATTO, ANSONI - CA, DAMASCHINO 27 ha EOLIE MALVASIA DELLE LIPARI CARRICANTE, CATARATTO, MINNELLA 100 ha ETNA ETNA BIANCO, ETNA BIANCO SUPERIORE SOAVE GARGANEGA, TREBBIANO DI SOAVE 6.700 ha SOAVE, SOAVE CLASSICO, SOAVE SUPERIORE DOCG, RECIOTO DI SOAVE DOCG MALVASIA BIANCA DI CANDIA, TREBBIA- NO TOSCANO, MAL - VASIA DEL LAZIO 1.600 ha FRASCATI FRASCATI CANNELLINO, FRASCATI SUPERIORE 640 ha COLLI EUGANEI GARGANEGA, MANZO- NI BIANCO, SERPRINO, TAI, SAUVIGNON, PINOT BIANCO, CHARDONNAY, PINELLA, FIOR D’ARANCIO COLLI EUGANEI BIANCO, COLLI EUGA- NEI FIOR D’ARANCIO, COLLI EUGANEI CHARDONNAY, COLLI EUGANEI PINELLO, COLLI EUGANEI SERPRINO, COLLI EUGANEI TAI FALANGHINA, CODA DI VOLPE, GRECO 170 ha VESUVIO BIANCO, LACRYMA CHRISTI BIANCO CAMPI FLEGREI BIANCO, CAMPI FLEGREI FALANGHINA ISCHIA BIANCO, ISCHIA BIANCO SUPERIORE TREBBIANO MALVASIA GRECO VIGNANELLO BIANCO, VIGNANELLO BIANCO SUPERIORE VIGNANELLO PROCANICO, MALVASIA, ROSSETTO EST! EST!! EST!!! DI MONTEFIASCONE EST EST EST DI MONTEFIASCONE, EST EST EST DI MONTEFIASCONE CLASSICO, EST EST EST DI MONTEFIASCONE SPUMANTE TREBBIANO TOSCANO, MALVASIA BIANCA TOSCANA 400 ha PITIGLIANO BIANCO DI PITIGLIANO ALEATICO ALEATICO DI GRADOLI ALEATICO DI GRADOLI, ALEATICO DI GRADOLI LIQUOROSO ALEATICO DI GRADOLI PASSITO PROCANICO, GRECHETTO 1.600 ha ORVIETO ORVIETO PROCANICO, GRECHETTO, ROSSETTO, MOSCATELLO, SANGIOVESE, VIOLONE, CANAIOLO 2.500 ha TUSCIA TUSCIA BIANCO, TUSCIA ROSSO E RO- SATO, T. PROCANICO, T. GRECHETTO, T. ROSSETTO, T. MOSCATELLO, T. SAN- GIOVESE, T. VIOLONE, T. CANAIOLO VOLCANIC WINES MAP OF ITALY’S VOLCANIC WINES ACTIVE VOLCANO INACTIVE VOLCANO (formation of lake of volcanic origin) INACTIVE VOLCANO PLUTONIC ROCKS VENEZIA ETNA MARE LAGO D’AVERNO REGIONAL CAPITAL VOLCANO SEA LAKE OF VOLCANIC ORIGIN LEGEND ZONE OF VOLCANIC ORIGIN GRAPE VARIETIES GROWN HECTARES UNDER VINE TYPES OF WINE SOAVE ZIBIBBO 64 ha PANTELLERIA MOSCATO DI PANTELLERIA DOC, PASSITO DI PANTELLERIA DOC, PANTELLERIA DOC SEMIDANO, NURAGUS, BOVALE MOGORO SARDEGNA SEMIDANO CAMPIDANO DI TERRALBA AGLIANICO VULTURE AGLIANICO DEL VULTURE 1.200 ha

Upload: others

Post on 30-Jan-2021

0 views

Category:

Documents


0 download

TRANSCRIPT

  • TYPES OF VOLCANO

    H A W A I I A N

    S T R O M B O L I A N

    V U L C A N I A N

    P E L E A N

    P L I N I A N

    Characterized by lows of very luid basaltic lava. Explosions are limi-ted, creating gushes of incandescent lava. Basaltic plateaux may be formed when the lava emerges from lateral issures. The form of the volcano is fairly lat because of the extreme luidity of the lava, which lows even when the slopes are not very steep. Apart from active volcanoes in Hawaii and in Iceland, volcanoes of this type are to be found in the areas of Soave and the Lessini Mountains, but these have been inactive for at least 40 million years.

    The lava in such cases is rich in gas and rather viscous, so that it forms blockages in the crater, thus creating more powerful explosions. Here outlows of lava alternate with pyroclastic surges. Usually these volcanoes have more accentuated slopes. (Example: Stromboli).

    These volcanoes emit lava that is very viscous and contains little gas, so that they generate powerful explosions, with emissions of gas and ash. Their form is the typical one of cones of ash created by several strata of pyroclastic emissions. (Example: Etna).

    The formation typical of Mount Pelée in Martinique. The lava is so viscous that it solidiies even inside the crater. Blockages are crea-ted that cause very violent explosions, with the emission of burning clouds (“nuées ardentes”) that descend along the sides of the vol-cano.

    Here eruptions are extremely explosive, usually following long pe-riods of inactivity. Indeed, the crater is usually obstructed by solid lava. Their eruptions are characterized by tall volcanic cones with descending burning clouds. This generates volcanic chimneys and calderas caused by the collapse of the entire structure of the volca-no. (Example: Vesuvius).

    DURELLA450 ha

    LESSINI DURELLO LESSINI DURELLO DOC,MONTI LESSINI

    GARGANEGA1.200 ha

    GAMBELLARAGAMBELLARA, GAMBELLARA CLASSICO, GAMBELLARA CLASSICO VIN SANTO, RECIOTO DI GAMBELLARA DOCG

    CAMPI FLEGREI

    CODA DI VOLPE,FALANGHINA, GRECO 160 ha

    VESUVIO

    FORASTERA,BIANCOLELLA

    130 haISCHIA

    MALVASIA DI LIPARI, CORINTO, GRILLO, CATARRATTO, ANSONI-CA, DAMASCHINO 27 ha

    EOLIE MALVASIA DELLE LIPARI

    CARRICANTE,CATARATTO,MINNELLA 100 ha

    ETNA ETNA BIANCO,ETNA BIANCO SUPERIORE

    SOAVE GARGANEGA,TREBBIANO DI SOAVE 6.700 haSOAVE, SOAVE CLASSICO,SOAVE SUPERIORE DOCG,RECIOTO DI SOAVE DOCG

    MALVASIA BIANCA DI CANDIA, TREBBIA-NO TOSCANO, MAL-VASIA DEL LAZIO 1.600 ha

    FRASCATI FRASCATI CANNELLINO,FRASCATI SUPERIORE

    640 haCOLLI EUGANEI

    GARGANEGA, MANZO-NI BIANCO, SERPRINO, TAI, SAUVIGNON, PINOT BIANCO, CHARDONNAY, PINELLA, FIOR D’ARANCIO

    COLLI EUGANEI BIANCO, COLLI EUGA-NEI FIOR D’ARANCIO, COLLI EUGANEI CHARDONNAY, COLLI EUGANEI PINELLO, COLLI EUGANEI SERPRINO, COLLI EUGANEI TAI

    FALANGHINA,CODA DI VOLPE, GRECO 170 ha

    VESUVIO BIANCO,LACRYMA CHRISTI BIANCO

    CAMPI FLEGREI BIANCO,CAMPI FLEGREI FALANGHINA

    ISCHIA BIANCO,ISCHIA BIANCO SUPERIORE

    TREBBIANOMALVASIAGRECO

    VIGNANELLO BIANCO, VIGNANELLO BIANCO SUPERIORE

    VIGNANELLO

    PROCANICO,MALVASIA,ROSSETTO

    EST! EST!! EST!!!DI MONTEFIASCONE

    EST EST EST DI MONTEFIASCONE, EST EST EST DI MONTEFIASCONE CLASSICO, EST EST EST DI MONTEFIASCONE SPUMANTE

    TREBBIANO TOSCANO,MALVASIA BIANCA TOSCANA 400 ha

    PITIGLIANO BIANCO DI PITIGLIANO

    ALEATICOALEATICODI GRADOLIALEATICO DI GRADOLI, ALEATICO DI GRADOLI LIQUOROSOALEATICO DI GRADOLI PASSITO

    PROCANICO,GRECHETTO

    1.600 haORVIETO ORVIETO

    PROCANICO, GRECHETTO, ROSSETTO, MOSCATELLO, SANGIOVESE, VIOLONE, CANAIOLO 2.500 ha

    TUSCIATUSCIA BIANCO, TUSCIA ROSSO E RO-SATO, T. PROCANICO, T. GRECHETTO, T. ROSSETTO, T. MOSCATELLO, T. SAN-GIOVESE, T. VIOLONE, T. CANAIOLO

    V O LC AN IC W IN ES MAP O F

    I T ALY ’ S V O LC AN I C W I N ES

    ACTIVE VOLCANO

    INACTIVE VOLCANO (formation of lake of volcanic origin)

    INACTIVE VOLCANO

    PLUTONIC ROCKS

    VENEZIA

    E T N A

    M A R E

    LAGO D’AVERNO

    REGIONAL CAPITAL

    VOLCANO

    SEA

    LAKEOF VOLCANIC ORIGIN

    L E G E N D

    ZONE OF VOLCANIC ORIGIN

    GRAPE VARIETIES GROWN

    HECTARES UNDER VINE

    TYPES OF WINE

    SOAVE

    ZIBIBBO64 ha

    PANTELLERIA MOSCATO DI PANTELLERIA DOC, PASSITO DI PANTELLERIA DOC, PANTELLERIA DOC

    SEMIDANO,NURAGUS,BOVALEMOGORO SARDEGNA SEMIDANOCAMPIDANO DI TERRALBA

    AGLIANICOVULTURE AGLIANICO DEL VULTURE1.200 ha