Profundidade dos terremotos na Venezuela amplificou destruição

Profundidade dos terremotos na Venezuela amplificou destruição; entenda

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[{"selector":"#anim-cb861ec9-1108-4bd6-92d1-e475a6e76412","keyframes":{"opacity":[0,1]},"delay":0,"duration":600,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] [{"selector":"#anim-d2d7b60e-2a1f-4e8c-99b6-d84a22215a0f","keyframes":{"opacity":[0,1]},"delay":0,"duration":1000,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] [{"selector":"#anim-d5d9d6a0-83d2-4c92-9c37-ad49f7b81004","keyframes":{"opacity":[0,1]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] [{"selector":"#anim-2915fee2-730a-4af5-a72b-206beb80255e","keyframes":{"transform":["scale(0.3333333333333333)","scale(1)"]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"forwards"}] [{"selector":"#anim-3863914d-51fa-4a39-8834-45137a82c749 [data-leaf-element=\"true\"]","keyframes":{"transform":["translate3d(-55.047320362867055%, 0, 0)","translate3d(0%, 0, 0)"]},"delay":0,"duration":2000,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] REUTERS Esse aspecto é um fator determinante para a extensão dos danos, segundo Allen. Relatos iniciais indicaram que os tremores foram relativamente rasos — entre 10 e 20 km de profundidade —, o que permitiu que mais energia chegasse à superfície e intensificasse o impacto

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[{"selector":"#anim-a42bc254-3d66-47e8-9238-f66242b6b7bf [data-leaf-element=\"true\"]","keyframes":{"transform":["translate3d(43.78196687569129%, 0, 0)","translate3d(0%, 0, 0)"]},"delay":0,"duration":2000,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] [{"selector":"#anim-dc15d391-da37-488a-9cc0-2d0d138a531f","keyframes":{"opacity":[0,1]},"delay":0,"duration":1000,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] [{"selector":"#anim-cf7aa95c-2679-4573-855a-8aeff63b8ff5","keyframes":{"opacity":[0,1]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] [{"selector":"#anim-5208f348-46e5-44c2-b39b-b8e3cacd53d4","keyframes":{"transform":["scale(0.3333333333333333)","scale(1)"]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"forwards"}] [{"selector":"#anim-b4f0dae4-b762-4c39-87c3-e55af46a8052","keyframes":{"opacity":[0,1]},"delay":0,"duration":600,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] O Serviço Geológico dos EUA , utilizando modelos preditivos para estimar o número de vítimas fatais, informou que o total de mortos poderia chegaria à casa dos milhares, com uma probabilidade significativa de ultrapassar 10 mil REUTERS

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Poderíamos ter previsto esses terremotos? A resposta honesta é não. A ciência ainda não chegou a um estágio em que disponhamos de ferramentas robustas que nos permitam prever terremotos

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[{"selector":"#anim-f7a920b3-98c3-4f68-bbb6-060b574a5212 [data-leaf-element=\"true\"]","keyframes":{"transform":["translate3d(0, 13.043478260869568%, 0)","translate3d(0, 0%, 0)"]},"delay":0,"duration":2000,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] [{"selector":"#anim-3e0aa770-dffe-4ea0-9228-0c5f4d6dceca","keyframes":{"opacity":[0,1]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"both"}] [{"selector":"#anim-2827bb15-f490-4774-97fe-ce51f83eab76","keyframes":{"transform":["scale(0.3333333333333333)","scale(1)"]},"delay":0,"duration":500,"easing":"cubic-bezier(.3,0,.55,1)","fill":"forwards"}] [{"selector":"#anim-8fadb8ec-c5fc-4f20-afa4-8d13f62eee9e","keyframes":{"opacity":[0,1]},"delay":0,"duration":600,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] [{"selector":"#anim-3d58c80b-76f2-46c2-beb6-d09672c4fa41","keyframes":{"opacity":[0,1]},"delay":0,"duration":1000,"easing":"cubic-bezier(0.4, 0.4, 0.0, 1)","fill":"both"}] REUTERS O especialista pontuou que apenas é possível identificar as áreas onde os tremores provavelmente ocorrerão, destacando que o norte da Venezuela é propenso a terremotos

[{"selector":"#anim-f1fb8c64-4a6d-49ef-bc0a-ff9ee2d09d85","keyframes":{"opacity":[0,1]},"delay":0,"duration":600,"easing":"cubic-bezier(0.2, 0.6, 0.0, 1)","fill":"both"}] [{"selector":"#anim-169d0ead-e6ae-43ef-991e-b8af8642709b","keyframes":{"transform":["translate3d(0px, 208.8796%, 0)","translate3d(0px, 0px, 0)"]},"delay":0,"duration":600,"easing":"cubic-bezier(0.2, 0.6, 0.0, 1)","fill":"both"}] [{"selector":"#anim-51825ec5-429d-4794-aea2-da19707f9232","keyframes":{"opacity":[0,1]},"delay":0,"duration":600,"easing":"cubic-bezier(0.2, 0.6, 0.0, 1)","fill":"both"}] [{"selector":"#anim-5ac44fa2-e304-4d93-b4f6-392142a38af9","keyframes":{"transform":["translate3d(0px, 274.963%, 0)","translate3d(0px, 0px, 0)"]},"delay":0,"duration":600,"easing":"cubic-bezier(0.2, 0.6, 0.0, 1)","fill":"both"}] Podemos utilizar registros históricos e analisar características das rochas e da paisagem local para fundamentar essas afirmações. No entanto, isso está muito longe de permitir algo realmente útil: prever, com precisão, quando um terremoto ocorrerá, onde acontecerá e qual será a sua magnitude Mark Allen, chefe do Departamento de Ciências da Terra da Universidade de Durham

CNNBRASIL.COM.BR

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