跟读练习: What Is An Earthquake? | The Dr. Binocs Show | Educational Videos For Kids - 通过视频学习英语口语
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You
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You're laughing right watching me tumble like that are you oh?
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No, no go ahead But hey, do you know what just happened?
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Whoa!
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There we go again!
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Well, this is nothing but an earthquake.
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A small one indeed.
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Come, let me tell you about earthquakes today.
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Zoom in!
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The surface of the earth is like a jigsaw puzzle.
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Yes, it's not a single piece of land, but approximately 20 pieces of a puzzle that constantly move.
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But you don't feel it because they move quite slowly.
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Each one of those puzzle pieces are called tectonic plates.
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So, whenever those plates hit, bump or slide past another plate, an earthquake is caused.
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The surface where these plates slip is called the fault or the fault plane.
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So, when do you think it happens?
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Well, it happens all the time.
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But hey, don't be scared.
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Most of the times we don't feel the quakes as they are too small to reach us.
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But sometimes they are so strong that they can be felt over a thousand miles away.
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The place where the earthquake originates is called the Hypo Center.
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And the place where it occurs on the earth's surface is called the Epicenter.
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There are three types of earthquakes.
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Convergent boundary.
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Here, one plate is forced over another during an earthquake, which causes a thrust fault.
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Many hills and mountains have been formed due to the convergent boundary.
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Divergent boundary.
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Here plates are drifted apart from each other, forming a rift zone.
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This kind gives birth to new ocean flows.
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Transform fault.
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Here the plates slip by each other and this is also called strike slip.
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So, earthquakes are nothing but the shaking, rolling or a sudden shock of the earth's surface.
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Now you know that whenever the earth is stressed or angry, it shakes and grumbles.
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Don't be scared, I was just kidding.
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Trivia time!
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The instrument used by scientists to measure the intensity of earthquake is known as a seismograph.
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A tsunami is caused when earthquakes occur under water.
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Woah!
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Woah!
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Yikes!
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I need to rush before I tumble again.
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So this is me zooming out.
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Tune in next time for more fun facts.
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you
关于本课
在这一课中，您将学习与地震相关的词汇和短语，并提高您的英语发音。通过观看视频，您可以了解地震的基本知识，包括其形成的原因和不同类型的地震。此课将帮助您在英语口语练习中掌握更多专业词汇，同时也能提升您在情境对话中的流利度。
关键词汇与短语
- Earthquake（地震）
- Tectonic Plates（板块）
- Hypocentre（震源）
- Epicenter（震中）
- Fault（断层）
- Seismograph（地震仪）
- Tsunami（海啸）
- Convergent Boundary（聚合边界）
练习技巧
为有效地提高您的英语发音，可以采用影子跟读（shadowspeak）的技巧。首先，您需要跟随视频的节奏进行英语影子跟读。视频中的讲解速度适中，非常适合您练习。在跟读时，试着模仿讲解者的语调和语速，这将能帮助您提升英语口语练习的效果。
建议您尝试以下步骤：
- 观看视频时，先理解内容，听清楚每个词的发音。
- 暂停视频，逐句跟读，并注意发音的准确性和流利度。
- 反复练习，直到您能够无障碍地顺畅地跟读整段内容。
- 利用这个过程来提高您的英语口语能力，特别是在与地震相关的专业术语上。
通过这些方法，您将能够更好地掌握英语发音，加深对地震相关词汇的理解，并在实际对话中游刃有余。您可以利用看YouTube学英语的机会，在家中随时随地进行有效的英语学习和练习。
什么是跟读法？
跟读法 (Shadowing) 是一种有科学依据的语言学习技巧，最初开发用于专业口译员的培训，并由多语言者Alexander Arguelles博士普及。这个方法简单而强大：您在听英语母语原声的同时立即大声重复——就像是一个延迟1-2秒紧跟说话者的影子。与被动听力或语法练习不同，跟读法强迫您的大脑和口腔肌肉同时处理并模仿真实的讲话模式。研究表明它能显着提高发音准确性，语调，节奏，连读，听力理解和口语流利度——使其成为雅思口语备考和真实英语交流最有效的方法之一。