O Curso de Geologia de 85/90 da Universidade de Coimbra escolheu o nome de Geopedrados quando participou na Queima das Fitas.
Ficou a designação, ficaram muitas pessoas com e sobre a capa intemporal deste nome, agora com oportunidade de partilhar as suas ideias, informações e materiais sobre Geologia, Paleontologia, Mineralogia, Vulcanologia/Sismologia, Ambiente, Energia, Biologia, Astronomia, Ensino, Fotografia, Humor, Música, Cultura, Coimbra e AAC, para fins de ensino e educação.
The main earthquake struck at 16:58 GMT (04:58 local time) on November
4, 1952. Initially assigned a magnitude of 8.2, the quake was revised
to 9.0 Mw in later years. A large tsunami resulted,
causing destruction and loss of life around the Kamchatka peninsula
and the Kuril Islands. Hawaii was also struck, with estimated damages
of up to US$1 million and livestock losses, but no human casualties
were recorded. Japan reported no casualties or damage. The tsunami
reached as far as Alaska, Chile, and New Zealand.
The hypocentre was located at 52.75°N 159.5°E,
at a depth of 30 km. The length of the subduction zone fracture was
600 km. Aftershocks were recorded in an area of approximately 247,000 km2, at depths of between 40 and 60 km.
A recent analysis of the tsunami runup distribution based on
historical and geological records give some indication as to the slip
distribution of the rupture.
View of the Severo-Kurilsk port. In 1952 a whole settlement was located there. The modern town was rebuilt in another place
1952 Severo-Kurilsk Tsunami was a major tsunami that hit Severo-Kurilsk, Kuril Islands, Sakhalin Oblast, Russian SFSR, USSR, which occurred on 5 November 1952 at about 5 a.m. It led to the destruction of many settlements in Sakhalin Oblast and Kamchatka Oblast, while the main impact struck the town of Severo-Kurilsk. The tsunami was generated by a major earthquake in the Pacific Ocean, 130 km from the shore of Kamchatka,
with an estimated magnitude of 9.0. There were three waves about 15-18
m high. After the earthquake the majority of the Severo-Kurilsk
citizens fled to the surrounding hills, where they escaped the first
wave. However, most of them returned to the town and were killed by the
second wave. The third wave was minor. According to the authorities,
out of a population of 6,000 people, 2,336 died.
The remaining survivors were evacuated to continental Russia. The settlement was then rebuilt in another location.
NOTA: embora provocando poucos mortos, dada a sua magnitude, este sismo é
considerado atualmente o 5º com mais elevada magnitude não inferida de sempre e o 3º mais forte do século XX, segundo a Wikipédia:
The main earthquake struck at 16:58 GMT (04:58 local time) on November
4, 1952. Initially assigned a magnitude of 8.2, the quake was revised
to 9.0 Mw in later years. A large tsunami resulted,
causing destruction and loss of life around the Kamchatka peninsula
and the Kuril Islands. Hawaii was also struck, with estimated damages
of up to US$1 million and livestock losses, but no human casualties
were recorded. Japan reported no casualties or damage. The tsunami
reached as far as Alaska, Chile, and New Zealand.
The hypocentre was located at 52.75°N 159.5°E,
at a depth of 30 km. The length of the subduction zone fracture was
600 km. Aftershocks were recorded in an area of approximately 247,000 km2, at depths of between 40 and 60 km.
A recent analysis of the tsunami runup distribution based on
historical and geological records give some indication as to the slip
distribution of the rupture.
View of the Severo-Kurilsk port. In 1952 a whole settlement was located there. The modern town was rebuilt in another place
1952 Severo-Kurilsk Tsunami was a major tsunami that hit Severo-Kurilsk, Kuril Islands, Sakhalin Oblast, Russian SFSR, USSR, which occurred on 5 November 1952 at about 5 a.m. It led to the destruction of many settlements in Sakhalin Oblast and Kamchatka Oblast, while the main impact struck the town of Severo-Kurilsk. The tsunami was generated by a major earthquake in the Pacific Ocean, 130 km from the shore of Kamchatka,
with an estimated magnitude of 9.0. There were three waves about 15-18
m high. After the earthquake the majority of the Severo-Kurilsk
citizens fled to the surrounding hills, where they escaped the first
wave. However, most of them returned to the town and were killed by the
second wave. The third wave was minor. According to the authorities,
out of a population of 6,000 people, 2,336 died.
The remaining survivors were evacuated to continental Russia. The settlement was then rebuilt in another location.
NOTA: embora provocando poucos mortos, dada a sua magnitude, este sismo é
considerado atualmente o 5º com mais elevada magnitude não inferida de sempre e o 3º mais forte do século XX, segundo a Wikipédia:
The main earthquake struck at 16:58 GMT (04:58 local time) on November
4, 1952. Initially assigned a magnitude of 8.2, the quake was revised
to 9.0 Mw in later years. A large tsunami resulted,
causing destruction and loss of life around the Kamchatka peninsula
and the Kuril Islands. Hawaii was also struck, with estimated damages
of up to US$1 million and livestock losses, but no human casualties
were recorded. Japan reported no casualties or damage. The tsunami
reached as far as Alaska, Chile, and New Zealand.
The hypocentre was located at 52.75°N 159.5°E,
at a depth of 30 km. The length of the subduction zone fracture was
600 km. Aftershocks were recorded in an area of approximately 247,000 km2, at depths of between 40 and 60 km.
A recent analysis of the tsunami runup distribution based on
historical and geological records give some indication as to the slip
distribution of the rupture.
View of the Severo-Kurilsk port. In 1952 a whole settlement was located there. The modern town was rebuilt in another place
1952 Severo-Kurilsk Tsunami was a major tsunami that hit Severo-Kurilsk, Kuril Islands, Sakhalin Oblast, Russian SFSR, USSR, which occurred on 5 November 1952 at about 5 a.m. It led to the destruction of many settlements in Sakhalin Oblast and Kamchatka Oblast, while the main impact struck the town of Severo-Kurilsk. The tsunami was generated by a major earthquake in the Pacific Ocean, 130 km from the shore of Kamchatka,
with an estimated magnitude of 9.0. There were three waves about 15-18
m high. After the earthquake the majority of the Severo-Kurilsk
citizens fled to the surrounding hills, where they escaped the first
wave. However, most of them returned to the town and were killed by the
second wave. The third wave was minor. According to the authorities,
out of a population of 6,000 people, 2,336 died.
The remaining survivors were evacuated to continental Russia. The settlement was then rebuilt in another location.
NOTA: embora provocando poucos mortos, dada a sua magnitude, este sismo é
considerado atualmente o 5º com mais elevada magnitude não inferida, segundo a Wikipédia:
The main earthquake struck at 16:58 GMT (04:58 local time) on November
4, 1952. Initially assigned a magnitude of 8.2, the quake was revised
to 9.0 Mw in later years. A large tsunami resulted,
causing destruction and loss of life around the Kamchatka peninsula
and the Kuril Islands. Hawaii was also struck, with estimated damages
of up to US$1 million and livestock losses, but no human casualties
were recorded. Japan reported no casualties or damage. The tsunami
reached as far as Alaska, Chile, and New Zealand.
The hypocentre was located at 52.75°N 159.5°E,
at a depth of 30 km. The length of the subduction zone fracture was
600 km. Aftershocks were recorded in an area of approximately 247,000 km2, at depths of between 40 and 60 km.
A recent analysis of the tsunami runup distribution based on
historical and geological records give some indication as to the slip
distribution of the rupture.
View of the Severo-Kurilsk port. In 1952 a whole settlement was located there. The modern town was rebuilt in another place
1952 Severo-Kurilsk Tsunami was a major tsunami that hit Severo-Kurilsk, Kuril Islands, Sakhalin Oblast, Russian SFSR, USSR, which occurred on 5 November 1952 at about 5 a.m. It led to the destruction of many settlements in Sakhalin Oblast and Kamchatka Oblast, while the main impact struck the town of Severo-Kurilsk. The tsunami was generated by a major earthquake in the Pacific Ocean, 130 km from the shore of Kamchatka,
with an estimated magnitude of 9.0. There were three waves about 15-18
m high. After the earthquake the majority of the Severo-Kurilsk
citizens fled to the surrounding hills, where they escaped the first
wave. However, most of them returned to the town and were killed by the
second wave. The third wave was minor. According to the authorities,
out of a population of 6,000 people, 2,336 died.
The remaining survivors were evacuated to continental Russia. The settlement was then rebuilt in another location.
NOTA: embora provocando poucos mortos, dada a sua magnitude, este sismo é
considerado atualmente o 12º com mais elevada magnitude, segundo a Wikipédia:
Nove em cada dez terramotos acontece no Anel de Fogo do Pacífico. Porquê?
Anel de Fogo do Pacífico
A maior parte dos terramotos e erupções vulcânica do nosso
planeta dão-se no Anel de Fogo do Pacífico. A culpa é das placas
tectónicas.
A maior parte dos vulcões e terramotos da Terra acontecem em regiões que circundam o Oceano Pacífico.
Vulgarmente designado como Anel de Fogo, esta região do
globo que começa a sul do continente americano e termina na Nova
Zelândia, depois de uma volta circular, onde passa pela América do
Norte, Rússia, Japão, ilhas indonésias…
Todo esse percurso – 40 mil quilómetros de comprimento – é marcado por locais vulcânicos e sismicamente ativos.
De acordo com o EarthSky,
nos últimos 12 mil anos, os geólogos encontraram evidências de quase
1000 vulcões pré-históricos ativos ao longo do Círculo de Fogo.
90% dos sismos ocorrem no Anel de Fogo do Pacífico, e é lá que estão localizados 80% dos vulcões de todo o Mundo.
Há uma explicação…
A maioria dos fenómenos sísmicos e vulcânicos ocorrem, onde há fronteiras de placas tectónicas.
As placas tectónicas são uma parte vital da evolução da Terra, com a crosta e o manto superior a formarem a litosfera: fragmentada numa série de placas.
Estas placas colidem, dispersam-se, sobem e subduzem, criando diversas características geológicas à superfície.
No Anel de Fogo do Pacífico o que acontece é a interação de várias placas tectónicas, em zonas de subducção.
Quando isso ocorre, a placa mais pesada afunda por baixo da placa mais leve e derrete no manto fundido da Terra.
Algumas dessas zonas de subducção encontram-se também nas partes mais profundas do oceano, como explica o EarthSky.
Quando a tensão/energia acumulada de uma placa deformada se liberta subitamente, ocorrem abalos sísmicos.
Consequentemente, nalguns locais, a rocha fundida consegue infiltrar-se através da crosta e geram-se vulcões.
A maior parte das atividades sísmicas acontecem no fundo dos oceanos.
The main earthquake struck at 16:58 GMT (04:58 local time) on November
4, 1952. Initially assigned a magnitude of 8.2, the quake was revised
to 9.0 Mw in later years. A large tsunami resulted,
causing destruction and loss of life around the Kamchatka peninsula
and the Kuril Islands. Hawaii was also struck, with estimated damages
of up to US$1 million and livestock losses, but no human casualties
were recorded. Japan reported no casualties or damage. The tsunami
reached as far as Alaska, Chile, and New Zealand.
The hypocentre was located at 52.75°N 159.5°E,
at a depth of 30 km. The length of the subduction zone fracture was
600 km. Aftershocks were recorded in an area of approximately 247,000 km2, at depths of between 40 and 60 km.
A recent analysis of the tsunami runup distribution based on
historical and geological records give some indication as to the slip
distribution of the rupture.
View of the Severo-Kurilsk port. In 1952 a whole settlement was located there. The modern town was rebuilt in another place.
1952 Severo-Kurilsk Tsunami was a major tsunami that hit Severo-Kurilsk, Kuril Islands, Sakhalin Oblast, Russian SFSR, USSR, which occurred on 5 November 1952 at about 5 a.m. It led to the destruction of many settlements in Sakhalin Oblast and Kamchatka Oblast, while the main impact struck the town of Severo-Kurilsk. The tsunami was generated by a major earthquake in the Pacific Ocean, 130 km from the shore of Kamchatka,
with an estimated magnitude of 9.0. There were three waves about 15-18
m high. After the earthquake the majority of the Severo-Kurilsk
citizens fled to the surrounding hills, where they escaped the first
wave. However, most of them returned to the town and were killed by the
second wave. The third wave was minor. According to the authorities,
out of a population of 6,000 people, 2,336 died.
The remaining survivors were evacuated to continental Russia. The settlement was then rebuilt in another location.
NOTA: embora provocando poucos mortos, dada a sua magnitude, este sismo é
considerado atualmente o 12º com mais elevada magnitude, segundo a Wikipédia:
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