�ݺ�ߣshows by User: armstrong

�ݺ�ߣshows by User: armstrong / http://www.slideshare.net/images/logo.gif �ݺ�ߣshows by User: armstrong / Mon, 14 May 2012 16:49:13 GMT �ݺ�ߣShare feed for �ݺ�ߣshows by User: armstrong Buku geologi sulawesi armstrong sompotan /slideshow/buku-geologi-sulawesi-armstrong-sompotan/12931398 bukugeologisulawesiarmstrongsompotan-120514164914-phpapp01
Sulawesi terletak pada pertemuan 3 Lempeng besar, yang menyebabkan kondisi tektoniknya sangat kompleks, dimana kumpulan batuan dari busur kepulauan, batuan bancuh, ofiolit, dan bongkah dari mikrokontinen terbawa bersama proses penunjaman, tubrukan, serta proses tektonik lainnya. Adapun struktur geologi yang berkembang didominasi sesar-sesar mendatar, dimana mekanisme pembentukan struktur geologi Sulawesi bisa dijelaskan dengan model simple shear.]]>
Sulawesi terletak pada pertemuan 3 Lempeng besar, yang menyebabkan kondisi tektoniknya sangat kompleks, dimana kumpulan batuan dari busur kepulauan, batuan bancuh, ofiolit, dan bongkah dari mikrokontinen terbawa bersama proses penunjaman, tubrukan, serta proses tektonik lainnya. Adapun struktur geologi yang berkembang didominasi sesar-sesar mendatar, dimana mekanisme pembentukan struktur geologi Sulawesi bisa dijelaskan dengan model simple shear.]]> Mon, 14 May 2012 16:49:13 GMT /slideshow/buku-geologi-sulawesi-armstrong-sompotan/12931398 armstrong@slideshare.net(armstrong) Buku geologi sulawesi armstrong sompotan armstrong Sulawesi terletak pada pertemuan 3 Lempeng besar, yang menyebabkan kondisi tektoniknya sangat kompleks, dimana kumpulan batuan dari busur kepulauan, batuan bancuh, ofiolit, dan bongkah dari mikrokontinen terbawa bersama proses penunjaman, tubrukan, serta proses tektonik lainnya. Adapun struktur geologi yang berkembang didominasi sesar-sesar mendatar, dimana mekanisme pembentukan struktur geologi Sulawesi bisa dijelaskan dengan model simple shear. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/bukugeologisulawesiarmstrongsompotan-120514164914-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds" /> Sulawesi terletak pada pertemuan 3 Lempeng besar, yang menyebabkan kondisi tektoniknya sangat kompleks, dimana kumpulan batuan dari busur kepulauan, batuan bancuh, ofiolit, dan bongkah dari mikrokontinen terbawa bersama proses penunjaman, tubrukan, serta proses tektonik lainnya. Adapun struktur geologi yang berkembang didominasi sesar-sesar mendatar, dimana mekanisme pembentukan struktur geologi Sulawesi bisa dijelaskan dengan model simple shear.

Buku geologi sulawesi armstrong sompotan from Armstrong Sompotan

]]> 30892 8 https://cdn.slidesharecdn.com/ss_thumbnails/bukugeologisulawesiarmstrongsompotan-120514164914-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Buku "Logika Penemuan Ilmiah" (armstrong sompotan) /slideshow/buku-logika-penemuan-ilmiah-armstrong-sompotan/6840851 bukupopperlogikapenemuanilmiaharmstrongsompotan-110207113440-phpapp02
Buku Popper Logika Penemuan Ilmiah adalah terjemahan dari buku Popper "Logic of Scientific Discovery" oleh Armstrong Sompotan dkk.]]>
Buku Popper Logika Penemuan Ilmiah adalah terjemahan dari buku Popper "Logic of Scientific Discovery" oleh Armstrong Sompotan dkk.]]> Mon, 07 Feb 2011 11:34:06 GMT /slideshow/buku-logika-penemuan-ilmiah-armstrong-sompotan/6840851 armstrong@slideshare.net(armstrong) Buku "Logika Penemuan Ilmiah" (armstrong sompotan) armstrong Buku Popper Logika Penemuan Ilmiah adalah terjemahan dari buku Popper "Logic of Scientific Discovery" oleh Armstrong Sompotan dkk. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/bukupopperlogikapenemuanilmiaharmstrongsompotan-110207113440-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds" /> Buku Popper Logika Penemuan Ilmiah adalah terjemahan dari buku Popper "Logic of Scientific Discovery" oleh Armstrong Sompotan dkk.

Buku "Logika Penemuan Ilmiah" (armstrong sompotan) from Armstrong Sompotan

]]> 7386 7 https://cdn.slidesharecdn.com/ss_thumbnails/bukupopperlogikapenemuanilmiaharmstrongsompotan-110207113440-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 GEOTHERMAL IN INDONESIA ( Armstrong . UNIMA ) /slideshow/geothermal-indonesia-armstrong-unima/3075540 cfakepathklkamojang-100204200454-phpapp02
Laporan Kuliah Lapangan ENERGI GEOTERMAL DAN PEMANFAATANNYA Di Kamojang - Jawa Barat – Indonesia ]]>
Laporan Kuliah Lapangan ENERGI GEOTERMAL DAN PEMANFAATANNYA Di Kamojang - Jawa Barat – Indonesia ]]> Thu, 04 Feb 2010 20:04:42 GMT /slideshow/geothermal-indonesia-armstrong-unima/3075540 armstrong@slideshare.net(armstrong) GEOTHERMAL IN INDONESIA ( Armstrong . UNIMA ) armstrong Laporan Kuliah Lapangan ENERGI GEOTERMAL DAN PEMANFAATANNYA Di Kamojang - Jawa Barat – Indonesia <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/cfakepathklkamojang-100204200454-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds" /> Laporan Kuliah Lapangan ENERGI GEOTERMAL DAN PEMANFAATANNYA Di Kamojang - Jawa Barat – Indonesia

GEOTHERMAL IN INDONESIA ( Armstrong . UNIMA ) from Armstrong Sompotan

]]> 3765 6 https://cdn.slidesharecdn.com/ss_thumbnails/cfakepathklkamojang-100204200454-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 FLOODING HAZARDS, PREDICTION & MITIGATION /slideshow/flooding-hazards-prediction-mitigation/500471 flooding-hazards-prediction-mitigation-1215295796843870-9
Throughout the last century flooding has been one of the most costly disasters in terms of both property damage and human casualties. Major floods in China, for example, killed about 2 million people in 1887, nearly 4 million in 1931, and about 1 million in 1938. The 2007 flood was a major flood in Jakarta, affected several other areas around the city, such as West Java and Banten. The flood is considered the worst in the last three centuries, including the 1996 and 2002 Jakarta floods, which killed 10 and 25 people respectively. In less developed countries, humans are particularly sensitive to flood casualties because of high population density, absence of zoning regulations, lack of flood control, and lack of emergency response infrastructure and early warning systems. In industrialized countries the loss of life is usually lower because of flood control structures, zoning regulations that prevent the habitation of seriously vulnerable lands, and emergency preparedness. Still, property damage and disruption of life takes a great toll, and despite flood control structures and land use planning, floods still do occur.]]>
Throughout the last century flooding has been one of the most costly disasters in terms of both property damage and human casualties. Major floods in China, for example, killed about 2 million people in 1887, nearly 4 million in 1931, and about 1 million in 1938. The 2007 flood was a major flood in Jakarta, affected several other areas around the city, such as West Java and Banten. The flood is considered the worst in the last three centuries, including the 1996 and 2002 Jakarta floods, which killed 10 and 25 people respectively. In less developed countries, humans are particularly sensitive to flood casualties because of high population density, absence of zoning regulations, lack of flood control, and lack of emergency response infrastructure and early warning systems. In industrialized countries the loss of life is usually lower because of flood control structures, zoning regulations that prevent the habitation of seriously vulnerable lands, and emergency preparedness. Still, property damage and disruption of life takes a great toll, and despite flood control structures and land use planning, floods still do occur.]]> Sat, 05 Jul 2008 15:03:45 GMT /slideshow/flooding-hazards-prediction-mitigation/500471 armstrong@slideshare.net(armstrong) FLOODING HAZARDS, PREDICTION & MITIGATION armstrong Throughout the last century flooding has been one of the most costly disasters in terms of both property damage and human casualties. Major floods in China, for example, killed about 2 million people in 1887, nearly 4 million in 1931, and about 1 million in 1938. The 2007 flood was a major flood in Jakarta, affected several other areas around the city, such as West Java and Banten. The flood is considered the worst in the last three centuries, including the 1996 and 2002 Jakarta floods, which killed 10 and 25 people respectively. In less developed countries, humans are particularly sensitive to flood casualties because of high population density, absence of zoning regulations, lack of flood control, and lack of emergency response infrastructure and early warning systems. In industrialized countries the loss of life is usually lower because of flood control structures, zoning regulations that prevent the habitation of seriously vulnerable lands, and emergency preparedness. Still, property damage and disruption of life takes a great toll, and despite flood control structures and land use planning, floods still do occur. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/flooding-hazards-prediction-mitigation-1215295796843870-9-thumbnail.jpg?width=120&height=120&fit=bounds" /> Throughout the last century flooding has been one of the most costly disasters in terms of both property damage and human casualties. Major floods in China, for example, killed about 2 million people in 1887, nearly 4 million in 1931, and about 1 million in 1938. The 2007 flood was a major flood in Jakarta, affected several other areas around the city, such as West Java and Banten. The flood is considered the worst in the last three centuries, including the 1996 and 2002 Jakarta floods, which killed 10 and 25 people respectively. In less developed countries, humans are particularly sensitive to flood casualties because of high population density, absence of zoning regulations, lack of flood control, and lack of emergency response infrastructure and early warning systems. In industrialized countries the loss of life is usually lower because of flood control structures, zoning regulations that prevent the habitation of seriously vulnerable lands, and emergency preparedness. Still, property damage and disruption of life takes a great toll, and despite flood control structures and land use planning, floods still do occur.

FLOODING HAZARDS, PREDICTION & MITIGATION from Armstrong Sompotan

]]> 1448 3 https://cdn.slidesharecdn.com/ss_thumbnails/flooding-hazards-prediction-mitigation-1215295796843870-9-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Mt. TAMBORA " The Largest Volcanic Eruption in Recorded History " /slideshow/mt-tambora-the-largest-volcanic-eruption-in-recorded-history/498057 mt-tambora-the-largest-volcanic-eruption-in-recorded-history-1215110268406246-9
The 1815 eruption of the Tambora volcano is generally considered as the largest and most violent volcanic event in recorded history. An estimated 150 km3 of volcanic material was released (the approximate equivalent to 16,000 Hiroshima bombs or eight times greater than the 1883 Krakatau eruption). The magnitude was seven on the VEI scale. It was an explosive central vent eruption with pyroclastic flows and a caldera collapse, causing tsunamis, and extensive land and property damage. It had a long-term effect on global climate. The eruption shot 400 million tons of sulfuric gases into the atmosphere, causing global cooling and creating what historians call ... \"The Year Without a Summer” The explosions killed 92,000 people on Sumbawa and Lombok island, now part of Indonesia, and wiped out the kingdom of Tambora (The Pompeii of the East).]]>
The 1815 eruption of the Tambora volcano is generally considered as the largest and most violent volcanic event in recorded history. An estimated 150 km3 of volcanic material was released (the approximate equivalent to 16,000 Hiroshima bombs or eight times greater than the 1883 Krakatau eruption). The magnitude was seven on the VEI scale. It was an explosive central vent eruption with pyroclastic flows and a caldera collapse, causing tsunamis, and extensive land and property damage. It had a long-term effect on global climate. The eruption shot 400 million tons of sulfuric gases into the atmosphere, causing global cooling and creating what historians call ... \"The Year Without a Summer” The explosions killed 92,000 people on Sumbawa and Lombok island, now part of Indonesia, and wiped out the kingdom of Tambora (The Pompeii of the East).]]> Thu, 03 Jul 2008 11:31:47 GMT /slideshow/mt-tambora-the-largest-volcanic-eruption-in-recorded-history/498057 armstrong@slideshare.net(armstrong) Mt. TAMBORA " The Largest Volcanic Eruption in Recorded History " armstrong The 1815 eruption of the Tambora volcano is generally considered as the largest and most violent volcanic event in recorded history. An estimated 150 km3 of volcanic material was released (the approximate equivalent to 16,000 Hiroshima bombs or eight times greater than the 1883 Krakatau eruption). The magnitude was seven on the VEI scale. It was an explosive central vent eruption with pyroclastic flows and a caldera collapse, causing tsunamis, and extensive land and property damage. It had a long-term effect on global climate. The eruption shot 400 million tons of sulfuric gases into the atmosphere, causing global cooling and creating what historians call ... \"The Year Without a Summer” The explosions killed 92,000 people on Sumbawa and Lombok island, now part of Indonesia, and wiped out the kingdom of Tambora (The Pompeii of the East). <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/mt-tambora-the-largest-volcanic-eruption-in-recorded-history-1215110268406246-9-thumbnail.jpg?width=120&height=120&fit=bounds" /> The 1815 eruption of the Tambora volcano is generally considered as the largest and most violent volcanic event in recorded history. An estimated 150 km3 of volcanic material was released (the approximate equivalent to 16,000 Hiroshima bombs or eight times greater than the 1883 Krakatau eruption). The magnitude was seven on the VEI scale. It was an explosive central vent eruption with pyroclastic flows and a caldera collapse, causing tsunamis, and extensive land and property damage. It had a long-term effect on global climate. The eruption shot 400 million tons of sulfuric gases into the atmosphere, causing global cooling and creating what historians call ... \"The Year Without a Summer” The explosions killed 92,000 people on Sumbawa and Lombok island, now part of Indonesia, and wiped out the kingdom of Tambora (The Pompeii of the East).

Mt. TAMBORA " The Largest Volcanic Eruption in Recorded History " from Armstrong Sompotan

]]> 4665 12 https://cdn.slidesharecdn.com/ss_thumbnails/mt-tambora-the-largest-volcanic-eruption-in-recorded-history-1215110268406246-9-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Fenomena Siklon Tropis ( Armstrong . Unima ) /armstrong/fenomena-siklon-tropis-armstrong-unima fenomena-siklon-tropis-armstrong-unima-1198673369556114-3
Siklon tropis atau juga dikenal dengan Hurricane di Samudera Atlantic dan di bagian timur Samudera Pacific, Typhoon di bagian barat Pacific, Cyclone di bagian selatan bumi (Samudera Hindia), dan Willy willies di bagian utara Australia, adalah gejala alam yang berlangsung secara periodik berupa cuaca buruk yang merusak dan sangat mengancam kehidupan manusia. Masih tergiang peristiwa Badai Sidr tanggal 15-16 November 2007 lalu di Bangladesh yang merengut ribuan korban. Siklon tropis sangat berbahaya karena energi merusaknya berupa angin berkecepatan tinggi, hujan deras, badai petir seringkali disertai banjir, tornado, dan tanah longsor. ]]>
Siklon tropis atau juga dikenal dengan Hurricane di Samudera Atlantic dan di bagian timur Samudera Pacific, Typhoon di bagian barat Pacific, Cyclone di bagian selatan bumi (Samudera Hindia), dan Willy willies di bagian utara Australia, adalah gejala alam yang berlangsung secara periodik berupa cuaca buruk yang merusak dan sangat mengancam kehidupan manusia. Masih tergiang peristiwa Badai Sidr tanggal 15-16 November 2007 lalu di Bangladesh yang merengut ribuan korban. Siklon tropis sangat berbahaya karena energi merusaknya berupa angin berkecepatan tinggi, hujan deras, badai petir seringkali disertai banjir, tornado, dan tanah longsor. ]]> Wed, 26 Dec 2007 04:49:30 GMT /armstrong/fenomena-siklon-tropis-armstrong-unima armstrong@slideshare.net(armstrong) Fenomena Siklon Tropis ( Armstrong . Unima ) armstrong Siklon tropis atau juga dikenal dengan Hurricane di Samudera Atlantic dan di bagian timur Samudera Pacific, Typhoon di bagian barat Pacific, Cyclone di bagian selatan bumi (Samudera Hindia), dan Willy willies di bagian utara Australia, adalah gejala alam yang berlangsung secara periodik berupa cuaca buruk yang merusak dan sangat mengancam kehidupan manusia. Masih tergiang peristiwa Badai Sidr tanggal 15-16 November 2007 lalu di Bangladesh yang merengut ribuan korban. Siklon tropis sangat berbahaya karena energi merusaknya berupa angin berkecepatan tinggi, hujan deras, badai petir seringkali disertai banjir, tornado, dan tanah longsor. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/fenomena-siklon-tropis-armstrong-unima-1198673369556114-3-thumbnail.jpg?width=120&height=120&fit=bounds" /> Siklon tropis atau juga dikenal dengan Hurricane di Samudera Atlantic dan di bagian timur Samudera Pacific, Typhoon di bagian barat Pacific, Cyclone di bagian selatan bumi (Samudera Hindia), dan Willy willies di bagian utara Australia, adalah gejala alam yang berlangsung secara periodik berupa cuaca buruk yang merusak dan sangat mengancam kehidupan manusia. Masih tergiang peristiwa Badai Sidr tanggal 15-16 November 2007 lalu di Bangladesh yang merengut ribuan korban. Siklon tropis sangat berbahaya karena energi merusaknya berupa angin berkecepatan tinggi, hujan deras, badai petir seringkali disertai banjir, tornado, dan tanah longsor.

Fenomena Siklon Tropis ( Armstrong . Unima ) from Armstrong Sompotan

]]> 11022 8 https://cdn.slidesharecdn.com/ss_thumbnails/fenomena-siklon-tropis-armstrong-unima-1198673369556114-3-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Formasi Geologi Sulawesi ( Armstrong . Unima ) /armstrong/formasi-geologi-sulawesi-armstrong-unima formasi-geologi-sulawesi-armstrong-unima-1198657071481515-2
Sulawesi terletak pada pertemuan 3 Lempeng besar yaitu Eurasia, Pasifik,dan IndoAustralia serta sejumlah lempeng lebih kecil (Lempeng Filipina) yang menyebabkan kondisi tektoniknya sangat kompleks.]]>
Sulawesi terletak pada pertemuan 3 Lempeng besar yaitu Eurasia, Pasifik,dan IndoAustralia serta sejumlah lempeng lebih kecil (Lempeng Filipina) yang menyebabkan kondisi tektoniknya sangat kompleks.]]> Wed, 26 Dec 2007 00:17:52 GMT /armstrong/formasi-geologi-sulawesi-armstrong-unima armstrong@slideshare.net(armstrong) Formasi Geologi Sulawesi ( Armstrong . Unima ) armstrong Sulawesi terletak pada pertemuan 3 Lempeng besar yaitu Eurasia, Pasifik,dan IndoAustralia serta sejumlah lempeng lebih kecil (Lempeng Filipina) yang menyebabkan kondisi tektoniknya sangat kompleks. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/formasi-geologi-sulawesi-armstrong-unima-1198657071481515-2-thumbnail.jpg?width=120&height=120&fit=bounds" /> Sulawesi terletak pada pertemuan 3 Lempeng besar yaitu Eurasia, Pasifik,dan IndoAustralia serta sejumlah lempeng lebih kecil (Lempeng Filipina) yang menyebabkan kondisi tektoniknya sangat kompleks.

Formasi Geologi Sulawesi ( Armstrong . Unima ) from Armstrong Sompotan

]]> 21972 16 https://cdn.slidesharecdn.com/ss_thumbnails/formasi-geologi-sulawesi-armstrong-unima-1198657071481515-2-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Volcanology And Geothermal Of Lesser Sunda Islands /slideshow/vulcanology-and-geothermal-of-lesser-sunda-islands/212494 vulcanology-and-geothermal-of-lesser-sunda-islands-1198651945110686-4
The Global Volcanism Program database for Lesser Sunda Islands currently contains 29 Holocene volcanoes, sorted below in geographical (volcano number) order.]]>
The Global Volcanism Program database for Lesser Sunda Islands currently contains 29 Holocene volcanoes, sorted below in geographical (volcano number) order.]]> Tue, 25 Dec 2007 22:52:26 GMT /slideshow/vulcanology-and-geothermal-of-lesser-sunda-islands/212494 armstrong@slideshare.net(armstrong) Volcanology And Geothermal Of Lesser Sunda Islands armstrong The Global Volcanism Program database for Lesser Sunda Islands currently contains 29 Holocene volcanoes, sorted below in geographical (volcano number) order. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/vulcanology-and-geothermal-of-lesser-sunda-islands-1198651945110686-4-thumbnail.jpg?width=120&height=120&fit=bounds" /> The Global Volcanism Program database for Lesser Sunda Islands currently contains 29 Holocene volcanoes, sorted below in geographical (volcano number) order.

Volcanology And Geothermal Of Lesser Sunda Islands from Armstrong Sompotan

]]> 1515 5 https://cdn.slidesharecdn.com/ss_thumbnails/vulcanology-and-geothermal-of-lesser-sunda-islands-1198651945110686-4-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 D I S A S T E R L O G ( A R M S T R O N G) /armstrong/d-i-s-a-s-t-e-r-l-o-g-a-r-m-s-t-r-o-n-g d-i-s-a-s-t-e-r-l-o-g-a-r-m-s-t-r-o-n-g-1198648755485336-5
Disaster log (Ag 20- Des 14, 2007)]]>
Disaster log (Ag 20- Des 14, 2007)]]> Tue, 25 Dec 2007 21:59:16 GMT /armstrong/d-i-s-a-s-t-e-r-l-o-g-a-r-m-s-t-r-o-n-g armstrong@slideshare.net(armstrong) D I S A S T E R L O G ( A R M S T R O N G) armstrong Disaster log (Ag 20- Des 14, 2007) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/d-i-s-a-s-t-e-r-l-o-g-a-r-m-s-t-r-o-n-g-1198648755485336-5-thumbnail.jpg?width=120&height=120&fit=bounds" /> Disaster log (Ag 20- Des 14, 2007)

D I S A S T E R L O G ( A R M S T R O N G) from Armstrong Sompotan

]]> 1327 4 https://cdn.slidesharecdn.com/ss_thumbnails/d-i-s-a-s-t-e-r-l-o-g-a-r-m-s-t-r-o-n-g-1198648755485336-5-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 The Phenomenon Of Tropical Cyclone /slideshow/the-phenomenon-of-tropical-cyclone-212474/212474 the-phenomenon-of-tropical-cyclone-1198647876343897-2
Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.]]>
Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.]]> Tue, 25 Dec 2007 21:44:37 GMT /slideshow/the-phenomenon-of-tropical-cyclone-212474/212474 armstrong@slideshare.net(armstrong) The Phenomenon Of Tropical Cyclone armstrong Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/the-phenomenon-of-tropical-cyclone-1198647876343897-2-thumbnail.jpg?width=120&height=120&fit=bounds" /> Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.

The Phenomenon Of Tropical Cyclone from Armstrong Sompotan

]]> 4901 10 https://cdn.slidesharecdn.com/ss_thumbnails/the-phenomenon-of-tropical-cyclone-1198647876343897-2-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 The Phenomenon Of Tropical Cyclone /slideshow/the-phenomenon-of-tropical-cyclone/212471 the-phenomenon-of-tropical-cyclone-1198647620169394-4
Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.]]>
Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.]]> Tue, 25 Dec 2007 21:40:21 GMT /slideshow/the-phenomenon-of-tropical-cyclone/212471 armstrong@slideshare.net(armstrong) The Phenomenon Of Tropical Cyclone armstrong Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/the-phenomenon-of-tropical-cyclone-1198647620169394-4-thumbnail.jpg?width=120&height=120&fit=bounds" /> Tropical cyclones—variously defined as hurricanes, typhoons, and cyclones—regularly impact human populations and periodically produce devastating weather-related natural disasters. The destructive forces of cyclonic winds, inundating rains, and storm surge are frequently accompanied by floods, tornadoes, and landslides.

The Phenomenon Of Tropical Cyclone from Armstrong Sompotan

]]> 4781 16 https://cdn.slidesharecdn.com/ss_thumbnails/the-phenomenon-of-tropical-cyclone-1198647620169394-4-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 Peta Gunung Api Dan Potensi Geothermal Bali Ntb Ntt (ARMSTRONG.UNIMA) /slideshow/peta-gunung-api-dan-potensi-geothermal-bali-ntb-ntt-armstrongunima/207261 peta-gunung-api-dan-potensi-geothermal-bali-ntb-ntt-armstrongunima-1198022611261782-2
]]>
]]> Tue, 18 Dec 2007 16:03:32 GMT /slideshow/peta-gunung-api-dan-potensi-geothermal-bali-ntb-ntt-armstrongunima/207261 armstrong@slideshare.net(armstrong) Peta Gunung Api Dan Potensi Geothermal Bali Ntb Ntt (ARMSTRONG.UNIMA) armstrong <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/peta-gunung-api-dan-potensi-geothermal-bali-ntb-ntt-armstrongunima-1198022611261782-2-thumbnail.jpg?width=120&height=120&fit=bounds" />

Peta Gunung Api Dan Potensi Geothermal Bali Ntb Ntt (ARMSTRONG.UNIMA) from Armstrong Sompotan

]]> 11790 8 https://cdn.slidesharecdn.com/ss_thumbnails/peta-gunung-api-dan-potensi-geothermal-bali-ntb-ntt-armstrongunima-1198022611261782-2-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post

http://activitystrea.ms/schema/1.0/posted

0 https://cdn.slidesharecdn.com/profile-photo-armstrong-48x48.jpg?cb=1522782304 Graduate student at Doctoral Program in Earth Science, Institute of Technology Bandung (ITB) armstrongsompotan.blogspot.com/ https://cdn.slidesharecdn.com/ss_thumbnails/bukugeologisulawesiarmstrongsompotan-120514164914-phpapp01-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/buku-geologi-sulawesi-armstrong-sompotan/12931398 Buku geologi sulawesi ... https://cdn.slidesharecdn.com/ss_thumbnails/bukupopperlogikapenemuanilmiaharmstrongsompotan-110207113440-phpapp02-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/buku-logika-penemuan-ilmiah-armstrong-sompotan/6840851 Buku "Logika Penemuan ... https://cdn.slidesharecdn.com/ss_thumbnails/cfakepathklkamojang-100204200454-phpapp02-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/geothermal-indonesia-armstrong-unima/3075540 GEOTHERMAL IN INDONESI...