Destagionalizzare. Diktat per il Turismo. Studi del Territorio per evidenziarne le peculiarità ed attrattive commerciali. Focus sul tema di una piccola cittadina situata in un Territorio simile ad una Barriera Corallina completamente a cielo aperto.
La valle dei trulli ( Enviromental Data Mining) Plantone LucioPlantone Lucio
Come può un piccolo Comune in Puglia essere promotore di una "esperienza" turistica unica al mondo? Estrazione di ogni singolo dato. Big Data e Dati Ambientali; sommati ed analizati.
Alberobello : paese in Puglia non protagonista della propria organizzazione economica del Turismo. Gli ospiti soggiornano mediamente 2 giorni presso le strutture ricettive. Come offrire un prodotto sempre diverso per 14 giorni, oppure, pubblicizzare la zona come esperienza a lungo termine. Enviromental Data Mining. Studiare il Territorio e interpretare nuovi modi di raccontare oppure offrire nuove storie ai nostri turisti. Diventare protagonisti della propria programmazione economica.
Presentazione tenuta al Convegno Nazionale “Il Patrimonio Geologico: una risorsa da proteggere e valorizzare” 29 e 30 aprile 2010 - Sasso di Castalda (PZ)
Paleoecologia 1: mobilità degli organismiAndrea Baucon
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai cos'è la paleoecologia e come si muovevano gli organismi. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn what palaeoecology is and how did organisms move. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Progetto di ricognizione e verifica del patrimonio geologico esistente, con individuazione dei geositi e delle emergenze geologiche della Regione Puglia.
Progetto di ricognizione e verifica del patrimonio geologico esistente, con individuazione dei geositi e delle emergenze geologiche della Regione Puglia.
Andrea baucon, corso di paleoecologia lezione 1 - la paleoecologia ed i suo...Andrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 7 - piane di mareaAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai la struttura dell'ecosistema marino. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn the structure of the marine ecosystem. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
La valle dei trulli ( Enviromental Data Mining) Plantone LucioPlantone Lucio
Come può un piccolo Comune in Puglia essere promotore di una "esperienza" turistica unica al mondo? Estrazione di ogni singolo dato. Big Data e Dati Ambientali; sommati ed analizati.
Alberobello : paese in Puglia non protagonista della propria organizzazione economica del Turismo. Gli ospiti soggiornano mediamente 2 giorni presso le strutture ricettive. Come offrire un prodotto sempre diverso per 14 giorni, oppure, pubblicizzare la zona come esperienza a lungo termine. Enviromental Data Mining. Studiare il Territorio e interpretare nuovi modi di raccontare oppure offrire nuove storie ai nostri turisti. Diventare protagonisti della propria programmazione economica.
Presentazione tenuta al Convegno Nazionale “Il Patrimonio Geologico: una risorsa da proteggere e valorizzare” 29 e 30 aprile 2010 - Sasso di Castalda (PZ)
Paleoecologia 1: mobilità degli organismiAndrea Baucon
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai cos'è la paleoecologia e come si muovevano gli organismi. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn what palaeoecology is and how did organisms move. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Progetto di ricognizione e verifica del patrimonio geologico esistente, con individuazione dei geositi e delle emergenze geologiche della Regione Puglia.
Progetto di ricognizione e verifica del patrimonio geologico esistente, con individuazione dei geositi e delle emergenze geologiche della Regione Puglia.
Andrea baucon, corso di paleoecologia lezione 1 - la paleoecologia ed i suo...Andrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 7 - piane di mareaAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai la struttura dell'ecosistema marino. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn the structure of the marine ecosystem. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Andrea baucon, corso di paleoecologia lezione 6 - delta ed estuariAndrea Baucon
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 4 - ambienti lacustriAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 2 - ambienti glacialiAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 5 - ambienti deserticiAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Andrea baucon, corso di paleoecologia lezione 8 - laguneAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 9 - coste roccioseAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea Baucon, corso di paleontologia - lezione 9 - paleoecologia 6 (forma e ...Andrea Baucon
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai come dedurre la funzione delle strutture fossili dalla loro forma. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn how to understand the function of fossil structures from their form. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
2016 - 096345 - CI QUALITÀ DEGLI AMBIENTI INSEDIATIVI - Libro di testo per il...Luca Marescotti
Politecnico di Milano, 2015-2016 - secondo semestre.
Libro di testo per il corso tenuto dalla prof.a Floriana Pergalani: 094933 Geologia.
Il corso è tenuto all'interno del corso integrato:
096345 - CI QUALITÀ DEGLI AMBIENTI INSEDIATIVI
Docenti Marescotti Luca Piero , Pergalani Floriana
I Tarantini hanno il Mar Piccolo davanti agli occhi tutta la vita. ...Ma siamo sicuri di conoscere questo particolarissimo ambiente naturale? Lasciamoci guidare dal gruppo di lavoro del progetto Posidonia del Comune di Taranto, coordinato dalla prof.Silvia De Vitis, dedicato agli alunni delle Scuole primarie....e in fondo, anche a tutti noi......
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Andrea baucon, corso di paleoecologia lezione 6 - delta ed estuariAndrea Baucon
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 4 - ambienti lacustriAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 2 - ambienti glacialiAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 5 - ambienti deserticiAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Andrea baucon, corso di paleoecologia lezione 8 - laguneAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea baucon, corso di paleoecologia lezione 9 - coste roccioseAndrea Baucon
The slides are part of the "Palaeoecology: methods and applications" course taught by Andrea Baucon at the University of Genoa.
OVERVIEW
The activities are aimed at providing practical and theoretical tools to reconstruct the depositional environment based on the paleontological aspects (fossils, ichnofossils) of sedimentary successions. The teaching program follows a paleoecological transect from continental environments to abyssal plains, passing through deserts and coral reefs. For each depositional environment, the characteristic paleoecological properties are discussed, illustrating how to recognize, describe and interpret them.
LEARNING OUTCOMES
The student will acquire the ability to reconstruct the depositional environment based on the paleontological aspects (fossils, icnofossils) of a sedimentary succession.
SYLLABUS / CONTENT
1. PALEOENVIRONMENTAL TOOLS: the paleoecological investigation; taphonomy applied to environmental reconstruction; ichnofacies; ichnofabric; facies analysis; technical-scientific reports;
2. CONTINENTAL ENVIRONMENTS: paleoecology and paleoenvironments of desert, lake, river, alluvial plain, glacial and volcanoclastic settings;
3. SHALLOW MARINE ENVIRONMENTS: paleoecology and palaeoenvironments of beach, tidal plain, lagoon, strandplain, chenier plain, rocky coast, shelf, and carbonatic settings;
4. TRANSITIONAL ENVIRONMENTS: paleoecology and paleoenvironments of estuarine and deltaic settings;
5. DEEP MARINE ENVIRONMENTS: paleoecology and paleoenvironments of slope and abyssal plain settings;
Fieldwork activity: paleoecological analysis of fossil-bearing sedimentary successions
AIMS AND LEARNING OUTCOMES
The student will be able to:
• Define the ecological characteristics of a fossil association and their paleoenvironmental implications;
• Recognize, classify and interpret the main ichnofossils present in marine, transitional and continental sedimentary successions;
• Integrate paleontological and sedimentological information;
• Interpret the depositional environment of a sedimentary succession, based on both outcrop and core data;
• Compile summary documents such as technical-scientific reports and graphic representations of paleoenvironments
Andrea Baucon, corso di paleontologia - lezione 9 - paleoecologia 6 (forma e ...Andrea Baucon
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! In questa presentazione apprenderai come dedurre la funzione delle strutture fossili dalla loro forma. La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! In this presentation you will learn how to understand the function of fossil structures from their form. The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
Impara i concetti, gli strumenti e le tecniche per esplorare il registro fossile! La presentazione fa parte del corso di Paleontologia tenuto da Andrea Baucon presso l'Università di Trieste.
---
Learn the concepts, tools and techniques to explore the fossil record! The presentation is part of the palaeontology course taught by Andrea Baucon at the University of Trieste, Italy.
2016 - 096345 - CI QUALITÀ DEGLI AMBIENTI INSEDIATIVI - Libro di testo per il...Luca Marescotti
Politecnico di Milano, 2015-2016 - secondo semestre.
Libro di testo per il corso tenuto dalla prof.a Floriana Pergalani: 094933 Geologia.
Il corso è tenuto all'interno del corso integrato:
096345 - CI QUALITÀ DEGLI AMBIENTI INSEDIATIVI
Docenti Marescotti Luca Piero , Pergalani Floriana
I Tarantini hanno il Mar Piccolo davanti agli occhi tutta la vita. ...Ma siamo sicuri di conoscere questo particolarissimo ambiente naturale? Lasciamoci guidare dal gruppo di lavoro del progetto Posidonia del Comune di Taranto, coordinato dalla prof.Silvia De Vitis, dedicato agli alunni delle Scuole primarie....e in fondo, anche a tutti noi......
Archeomolise n.1, sett./ott. 2009 - I bifacciali di monteroduniGea Monteroduni
L’area indagata è stata oggetto di segnalazione
nel 2005 da parte della sig.ra Concetta
Leone, proprietaria del terreno in cui lei stessa
casualmente raccolse, proprio nello stesso
anno, un bifacciale, insieme a diversi manufatti
litici.
Relazione geologica e idrogeologica impianto geotermico AndranoTutor Casa
Relazione geologica e idrogeologica impianto geotermico Andrano. www.tutorcasa.it pubblica la progettazione completa di un impianto geotermico e segue passo passo la sua realizzazione. L'indice del progetto a questo link:
http://www.tutorcasa.it/progetto-completo-impianto-geotermico/progetto-completo-impianto-geotermico-15443.html
Il Piano di gestione della Riserva Naturale Statale Litorale Romanocirili_web
M. Tufano-L. dell'Anna, Il Piano di gestione della Riserva Naturale Statale Litorale Romano e la futura programmazione e progettazione infrastrutturale
Un approccio olistico per le Cinque Terre. Una presentazione di Barbara Raffellini all'ICCROM - l'ente creato dall'UNESCO per la tutela di monumenti e siti di maggior importanza a livello storico, culturale ed architettonico. 1999
Enviromental Data Mining . Murgia : Calcare come atomo di un territorio.
1. IL CALCARE COME ATOMO DI UN TERRITORIO
Relatore: Dott. Plantone Lucio
“Storia consapevole, arte popolare e
turismo sostenibile”
2. DEFINIZIONI
DEFINIZIONI:
La GEOLOGIA si occupa dell’origine e
della morfologia del pianeta Terra,
nonché dei materiali che lo
costituiscono e dei processi che si sono
svolti o che tutt’ora si svolgono su di
esso.
STRATIGRAFIA: Parte della geologia
che attraverso lo studio delle rocce
sedimentarie, per lo più stratificate,
intende ricostruire la storia geologica
della Terra.
STRATIGRAFIA: Parte della geologia che attraverso lo studio delle rocce sedimentarie, per lo più stratificate, intende ricostruire la storia geologica dell
3. DEFINIZIONI
2
ROCCIA: QUALUNQUE AGGREGATO NATURALE DI
MINERALI
MINERALE: E’ UN COMPOSTO CHIMICO CHE SI
PRESENTA IN NATURA IN UNA SINGOLA FASE
SOLIDA DEFINITA PER COMPOSIZIONE E
STRUTTURA CRISTALLINA, VALE A DIRE
ESPRIMIBILE CON UNA FORMULA
Le rocce possono essere raggruppate in t
categorie ben distinte come genesi: rocce
ignee (o magmatiche), rocce sedimentarie
rocce metamorfiche
4. TIPI DI ROCCE
Le rocce ignee si formano attraverso processi di
cristallizzazione, per raffreddamento, di materiali
fusi(magmi) che risalgono dall’interno della Terra.
ce sedimentarie sono il prodotto finale dei processi di
zione, erosione, trasporto e accumulo operati sulla
icie terrestre
siddetti agenti esogeni( acqua, vento ghiaccio)
Le rocce metamorfiche derivano da
trasformazioni più o meno profonde di altre rocce
5. ROCCE SEDIMENTARIE (DETRITICHE,ORGANOGENE, CHI
Il territorio della Valle D’Itria ed “enclavi” è dominato da rocce
sedimentarie carbonatiche: i calcari e le dolomie.
Le rocce carbonatiche sono in gran parte di origine bioge
I principali componenti dele rocce carbonatiche sono:
1) Il carbonato di calcio (CaCO3) ;
2) Il carbonato di magnesio (MgCO3) .
QUESTI COMPOSTI POSSONO PRESENTARSI
ISOLATAMENTE IN VARI STATI CRISTALLINI
(CASO FREQUENTE
PER IL CARBONATO DI CALCIO,
CHE COSTITUISCE IL MINERALE DETTO CALCITE O, PIU’ RARAMENTE
L’ARAGONITE)
O COMBINATI A FORMARE UN SALE DOPPIO
(CARBONATO DOPPIO DI CALCIO E MAGNESIO:
DOLOMITE)
6. IMMAGINI DI ROCCE SEDIMENTARIEIMMAGINI DI ROCCE SEDIMENTARIE
CALCITE SECONDARIA CALCITE MICROCRISTALLINA
CALCARE A NUMMULITI
7. ROCCE SEDIMENTARIE ORGANOGENE
Il corallo, appartiene alla classe degli Antozoi, phylum degli
cnidari, è un animale costituto da "polipi", cioè organismi
animali eterotrofi e da organismi simbionti "Zooxantellae",
alghe, vegetali.
Le Zooxantellae,sono organismi dinoflagellati
endosimbiontiche hanno una relazione mutualistica, e
possono vivere solo in questo modo, con i polipi dei coralli e
quindi per estensione coi coralli stessi.
Il nome “antozoi” deriva da ánthos + zôion = fiore + animale.
CREAZIONE BARRIERE CORALLINE ATTUALI
ESACORALLI-
MADREPORE
8. CARSISMO
Il paesaggio carsico è dato da un insieme di forme “anomale”
rispetto ai paesaggi “normali” di tipo fluviale.
Queste forme sono determinate dalla solubilità della roccia nelle acque naturali.
Grazie a questa solubilità le
Acque tendono a penetrare all’interno delle masse rocciose allargando delle
vie di circolazione sotterranea.
Ne deriva una scarsità od assenza di idrografia superficiale.
Pressuposti fondamentali perché si individuino dei paesaggi
Carsici sono: a) presenza di rocce solubili;
b) abbondanza di precipitazioni meteoriche
9. PROCESSO DI SOLUZONE E PRECIPITAZIONE DEI CALCARI
Processi di soluzione interessano prevalentemente i seguenti gruppi di rocce:
a) Le rocce carbonatiche (calari, dolomie e rocce intermedie);
b) Le evaoriti (anidrite, gesso, salgemma, ecc…)
CO2 + H2O + CaCO3 Ca(HCO3)2
Carbonato di
calcio
Bicarbonato di
calcio
10. MORFOLOGIE CARSICHE epigee
DOLINA: è una conca chiusa, un bacino che si riempirebbe
di acqua a originare un laghetto
se le pareti ed il fondo fossero impermeabili;
Invece, di solito, l’acqua viene assorbita attraverso vie sotterranee
POLJE: è una forma carsica molto grande. Di dimensioni chilometrica.
Un polje è definito tale se ha una lunghezza di almeno un
Chilometro. Un polje tipico presenta un fondo piano ed orizzontale e
versanti relativamente ripidi. Nei polje attivi il fondo viene allagato
Stagionalmente, quando gli inghiottitoi non riescono a smaltire tutta
l’acqua che affluisce nel bacino
13. FORME CARSICHE IPOGEE
Si possono definire “grotte” tutte le cavità
accessibili all’uomo
queste però cpstituiscono solo
una piccola parte del reticolo di cavità
sotterranee
presenti all’interno dei rilievi calcarei
16. IL TERRITORIO - STRATIGRAFIA
Notizie stratigrafiche sul territorio
Il complesso dei calcari affioranti nelle Murge è distinto in due unità
litostratigrafiche denominate: “Calcare di Bari” e “Calcare di Altamura”,
dalle località nei cui dintorni esse si mostrano con litofacies tipica.
Livello Corato: calcare bianco-rosato a grana
fine con grossi Lamellibranchi,
la cui base è costituita da un banco ci calcare
giallastro ad Orbitoline (Foraminiferi);
spessore 15 metri. Età: Barremiano (Cretaceo inferiore);
Livello Palese: calcari detritici bianchi
con Toucasie (Rudiste);spessore 30 metri circa.
Età: Albiano (Cretaceo inferiore);
Livello Sannicandro: banco di calcare bianco coroide
con grossi Bivalvi; spessore 4-5 metri.
Età: Albiano (Cretaceo inferiore)
Livello Toritto : bancata di calcare con Lamellibranchi
ed altri macrofossili,spessore compreso
tra 30 e 80 metri.
Età: Turoniano (Cretaceo superiore).
Colonna stratigrafica del gruppo dei calcari delle Murge
17. IL TERRITORIO ESAMINATO
La geologia di Alberobello
Principali caratteristiche fisico-meccaniche delle lastre utilizzate nella copertura dei trulli:
valori medi per ciascuna campione esaminato ; prove eseguite presso
il laboratorio di Geologia applicata e Geotecnica del Dipartimento di
Geologia e Geofisica dell’Università di Bari (da Ricchetti et al.,1985).
18. IL TERRITORIO ESAMINATO
La geologia di Alberobello
Fasce di saturazione; prove eseguite presso il
laboratorio di Geologia applicata e Geotecnica del
Dipartimento di Geologia e Geofisica
dell’Università di Bari (da Ricchetti et al.,1985).
19. APPROCCIO OLISTICO AL PROBLEMA
IL TERRITORIO ITALIANO E’ STATO
STUDIATO INTERAMENTE.
MOLTI DATI SONO NON UTILIZZATI O
RESI DI PUBBLICO DOMINIO.
COME UNIFICARE E NORMALIZZARE
TUTTE QUESTE INFORMAZIONI?
20. GEOGRAPHICAL INFORMATION SYSTEM
LA RISPOSTA
GIS è l'acronimo di Sistema Informativo Geografico. Si tratta di un
prodotto software realizzato attraverso programmi specifici (es. ArcView,
Grass) che gestiscono grandi quantità di dati in relazione alle coordinate
geografiche. Le applicazioni di questa tecnologia sono davvero tante e
forse limitate solo dalla fantasia.
È possibile creare nuovi temi personalizzati dall'interazione degli elementi di
diversi temi attraverso operazioni logiche di vario tipo (es. ritagliare i limiti
geologici contenuti all'interno di un determinato limite amministrativo). Queste
operazioni possono essere estese ai relativi database.
21. Stralcio TAV. I.G.M.
M.te Torre Moscia
Tabella Valutativa
Valore ecologico: 9
Valore scientifico/didattico: 9
Potenzialità turistiche: 9
Accessibilità: 9
Stato di conservazione: 7
Vincoli esistenti: incluso nell’elenco S.I.C.
Vincolo antropologico
Vincolo paesaggistico
Ubicazione
Provincia: BARI - BRINDISI
Comune: Alberobello-Fasano-Castellana Grotte
Foglio: 190 TAV. IGM Alberobello II N.O.
Toponimo: Canale di Pirro
Coordinate geografiche: da
(40°49’23’’N;4°44’33’’E)
a (40°48’21’’N; 4°44’46’’E) rispetto M.teMario
SCHEDA 1 CANALE DI PIRRO (FAC-SIMILE POWERPOINT)
.
Stralcio Tav. I.G.M
22. IL CANALE DI PIRRO
Panorama sul CANALE DI Pirro da Paretano Nuovo
Panorama sul Canale di Pirro da Torre Moscia
Sentiero per Torre Moscia (accesso dal Canale di Pirro)
23. IL CANALE DI PIRRO
“Torre” monumentale principale C.da Cuccumo
Chiesa SS. Addolorata a Cuccolicchio
Particolare del gradino di accesso
ad una torre monumentale
Fontana pubblica a Cuccolicchio
24. UTILIZZO G.I.S.
CARTA RASTER TRACCIAMENTO ISOIPSE
UTILIZZO G.I.S. PER DATI SOCIO-
COMPORTAMENTALI E PIANIFICAZIONE
TERRITORIALE
25. ENVIROMENTAL DATA
MINING
COSA E’:
-L’ESTRAZIONE DI OGNI SINGOLA INFORMAZIONE DA UN
TERRITORIO:
Storia; Flora; Fauna; Tradizioni; Folklore; Dati Geologici; ecc.
COSA PRODUCE DE FACTO :
-CONOSCENZA DEL TERRITORIO DEL PRODOTTO:
-Schede identificatrici e valutative dei Luoghi ; dossier
interni; documenti pubblicitari e comunicativi; schemi di
interconnessione dei dati per Nuovi Business; Mappe
Tematiche e Divulgative; ecc.
26. OBBIETTIVI:
MERCATO OBBIETTIVO
PRIMARIO : INCOMING
ENVIROMENTAL DATA
MINING
→ PUBBLICIZZARE OGNI PIU’ PICCOLO PARTICOLARE DELL’ITALIA: UNA VERA
E PROPRIA SCANSIONE
→ UNIRE I PUNTI: CREARE UN NETWORK DEI DATI
→ CREAZIONE NUOVI BUSINESS CON SINERGIE IN TERRITORIO.
→ COLLABORAZIONI CON AMMINISTRAZIONI LOCALI
→ NUOVE TIPOLOGIE DI ESCURSIONI ( SPECIFICHE PER FRANCESI; RUSSI;
INGLESI…)
→ CREAZIONE DI UNA IMMAGINE “VERDE” E SENSIBILE DELLA EDENVIAGGI
27. LE CARTE TEMATICHE
CARTA TEMATICA DEGLI ITINERARI TURISTICI (scala 1:25000):
vi sono segnalati
i punti rilevati durante i sopralluoghi in campagna.
Contiene tutte le Informazioni su particolari che hanno una valenza
turistico-ricreativa(masserie abbandonate,viste panoramiche,
particolari geologici, ecc.).
E’ molto utile nella progettazione di itinerari turistici.
E’ possibile creare degli itinerari tematici e molto vari con una metodologia di
network dei punti ivi segnalati.
CARTA TEMATICA GEOMORFICA (scala 1:25000): vi sono evidenziate le
caratteristiche
geomorfologiche del territorio esplorato ed interpretato con foto aeree.
Con simboli lineari e puntuali e aree colorate vi sono segnalati i “geositi” considerati
nelle schede.
Rispetto alla Carta Tematica degli Itinerari Turistici ha una valenza prettamente
geologica.
28. ESEMPIO: ITINERARIO NELLA GRAVINA ROTOLO
PARTENZA DA ALBEROBELLO
ARRIVO ALL’INGRESSO DELLA GRAVINA
(SEGNALATO PUNTO 24 SULLA CARTA)
…PERCORRENDO LA GRAVINA
SI ARRIVA AL SOLCO EROSIVO SEGNALATO
COL N.18 SULLA CARTA
PROSEGUENDO ANCORA PER LA GRAVI
RAGGIUNGE LA “BRIGLIA” IDRAULICA
SEGNALATA COL NUMERO 19 SULLA
CARTA
SI PERCORRE DAL BELVEDERE LA STRADA
CHE CONDUCE DA ALBEROBELLO A MONOPOLI
SI PRATICA IL SENTIERO SEGNALATO COL
PUNTO 23 SULLA CARTA TEMATICA
ESEMPIO DI CREAZIONE DI UN ITINERARIO CON NETWORK DI PUNTI