Digi school Geomorphology
Description: Digi school Geomorphology 2020-1-SK01-KA226-SCH-094350 2 2020-1-SK01-KA226-SCH-094350 SUBJECT: Geography SPECIFICATION: may be used for presentation and self-education AGE OF STUDENTS: 15 16 1 LESSON : 45 min Orogeny 6 3 Lesson content 01
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slide1. Digi school Geomorphology 2020-1-SK01-KA226-SCH-094350<br>
slide2. 2 2020-1-SK01-KA226-SCH-094350 SUBJECT: Geography
SPECIFICATION: may be used for presentation and self-education
AGE OF STUDENTS: 15 – 16
1 LESSON : 45 min<br>
slide3. Orogeny 6 3<br>
slide4. Lesson content 01 02 Types of mountains 03 Tasks 04 4 Orogeny<br>
slide5. Orogeny Orogeny (mountains formation) = series of processes in the crust that result in formation of mountains
Long-term process (may be even tens of millions of years)
Related to plate tectonics 5<br>
slide6. Types of mountains According the type of formation:
Fold mountains
Block mountains
Volcanic mountains 6<br>
slide7. Fold mountains Are formed on convergent plate margins
When plates collide, they tend to buckle and form fold mountains in the process called orogeny (thrusting and folding of rock) e. g. the Appalachian mountains
Sometimes a large sheet-like body of rock is moved above a thrust fold from its original position creating a nappe; examples of such mountains the Alps, the Carpathians, the Himalayas
Important orogenies 7<br>
slide8. Alpine orogeny
Cenozoic era Important orogenies Hercynian (Variscan) orogeny
Paleozoic era 8<br>
slide9. 9 Orogeny - video<br>
slide10. Block mountains the crust can be broken into block by friction faults
the blocks can be raised or tilted along the faults
block mountains is a series of horsts and grabens (the Krušné hory, the Hrubý Jeseník, the Harz) 10<br>
slide11. Volcanic mountains Are formed by volcanic activity
e. g. the Doupovské hory, the České středohoří, the Massive Central 11 Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC<br>
slide12. Tasks https://wordwall.net/play/25558/107/641
https://wordwall.net/play/25558/344/193 12 Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC<br>
slide13. Resources: 13 2020-1-SK01-KA226-SCH-094350 MS Office gallery<br>
slide14. 2020-1-SK01-KA226-SCH-094350 DIGI SCHOOL 14 2020-1-SK01-KA226-SCH-094350 Délka projektu: 01. 03. 2021 – 28. 02. 2023
Rozpočet partnerství: 101.092,-€
Rozpočet GJŠ Zlín: 20.829,- €
Intelektuální výstupy všech partnerů: ANJ, NEJ, FRJ,SPJ, DEJ, OBN, CHE, GEO, MAT, BIO, EKN, ITK,
HUV, ETV
Intelektuální výstupy GJŠ Zlín v předmětech MAT, GEO, CHE, SPJ<br>
slide15. EN The European Commission's support for the production of this publication does not constitute an endorsement of the contents, which reflect the views only of the authors, and the Commission cannot be held responsible for any use which may be made of the information contained therein. 15 2020-1-SK01-KA226-SCH-094350 ČR Podpora Evropské komise na zhotovení této práce nevyjadřuje názor Komise, obsah je názorem autora a Komise není zodpovědná za informace v práci obsažené.<br>
slide2. 2 2020-1-SK01-KA226-SCH-094350 SUBJECT: Geography
SPECIFICATION: may be used for presentation and self-education
AGE OF STUDENTS: 15 – 16
1 LESSON : 45 min<br>
slide3. Orogeny 6 3<br>
slide4. Lesson content 01 02 Types of mountains 03 Tasks 04 4 Orogeny<br>
slide5. Orogeny Orogeny (mountains formation) = series of processes in the crust that result in formation of mountains
Long-term process (may be even tens of millions of years)
Related to plate tectonics 5<br>
slide6. Types of mountains According the type of formation:
Fold mountains
Block mountains
Volcanic mountains 6<br>
slide7. Fold mountains Are formed on convergent plate margins
When plates collide, they tend to buckle and form fold mountains in the process called orogeny (thrusting and folding of rock) e. g. the Appalachian mountains
Sometimes a large sheet-like body of rock is moved above a thrust fold from its original position creating a nappe; examples of such mountains the Alps, the Carpathians, the Himalayas
Important orogenies 7<br>
slide8. Alpine orogeny
Cenozoic era Important orogenies Hercynian (Variscan) orogeny
Paleozoic era 8<br>
slide9. 9 Orogeny - video<br>
slide10. Block mountains the crust can be broken into block by friction faults
the blocks can be raised or tilted along the faults
block mountains is a series of horsts and grabens (the Krušné hory, the Hrubý Jeseník, the Harz) 10<br>
slide11. Volcanic mountains Are formed by volcanic activity
e. g. the Doupovské hory, the České středohoří, the Massive Central 11 Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC<br>
slide12. Tasks https://wordwall.net/play/25558/107/641
https://wordwall.net/play/25558/344/193 12 Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC Tato fotka od autora Neznámý autor s licencí CC BY-SA-NC<br>
slide13. Resources: 13 2020-1-SK01-KA226-SCH-094350 MS Office gallery<br>
slide14. 2020-1-SK01-KA226-SCH-094350 DIGI SCHOOL 14 2020-1-SK01-KA226-SCH-094350 Délka projektu: 01. 03. 2021 – 28. 02. 2023
Rozpočet partnerství: 101.092,-€
Rozpočet GJŠ Zlín: 20.829,- €
Intelektuální výstupy všech partnerů: ANJ, NEJ, FRJ,SPJ, DEJ, OBN, CHE, GEO, MAT, BIO, EKN, ITK,
HUV, ETV
Intelektuální výstupy GJŠ Zlín v předmětech MAT, GEO, CHE, SPJ<br>
slide15. EN The European Commission's support for the production of this publication does not constitute an endorsement of the contents, which reflect the views only of the authors, and the Commission cannot be held responsible for any use which may be made of the information contained therein. 15 2020-1-SK01-KA226-SCH-094350 ČR Podpora Evropské komise na zhotovení této práce nevyjadřuje názor Komise, obsah je názorem autora a Komise není zodpovědná za informace v práci obsažené.<br>