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Migmatitic Gneiss in Youngwol, South Korea Analytics Table
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Metamorphic rocks in Youngwol, South Korea (0:00) * νκΈ μλ¬Έ: μ¬λ¬λΆ, λ°κ°μ΅λλ€. μ€λ μ΄ν΄λ³Ό μ΄ μλ£μμ μμ£Ό μ€λλ λ°μλ€μ΄ κ²ͺμ λλΌμ΄ μ°κΈμ μ νν€μ³λ³Ό κ²λλ€. μμ΄ λ²μ: Hello, everyone. In today's material, we are going to uncover the incredible alchemy experienced by ancient rocks. (0:08) * νκΈ μλ¬Έ: μ°λ¦¬κ° λ§€μΌ λ°κ³ λ€λλ νν λλ©©μ΄λ€, κ³Όμ° 20μ΅ λ μ μ μ΄λ€ λͺ¨μ΅μ΄μμκΉμ? μμν΄ λ³΄μ μ μλμ? μμ΄ λ²μ: The common stones we step on every dayβhave you ever imagined what they looked like 2.0 billion years ago? (0:16) * νκΈ μλ¬Έ: μ΄κ±Έ μ΄ν΄νλ €λ©΄ λ³μ±μμ©μ μμμΌ ν΄μ. μ½κ² λ§ν΄, μ§κ΅¬ κΉμ κ³³μ μλ μμ²λ μλ ₯μ κ±°λν μ€λΈμ΄μ£ . μμ΄ λ²μ: To understand this, we need to know about metamorphism. Simply put, it's like a massive oven under immense pressure deep within the Earth. (0:23) * νκΈ μλ¬Έ: μ΄ λ¨κ±°μ΄ μ€λΈμμ νΉ κ΅¬μμ Έλμ¨ κ²°κ³Όλ¬Όμ΄ λ°λ‘ μ λλ ·ν μ€λ¬΄λ¬, νΈλ§μμ λλ€. μ λ§ λ©μ§μ£ ? μμ΄ λ²μ: The result of being thoroughly baked in this hot oven is that distinct striped rock right there: gneiss. Isn't it wonderful? (0:31) * νκΈ μλ¬Έ: μ¬λ£μ λ°λΌ μ’ λ₯λ λλλλ°μ. μ§ν κ°μ ν΄μ μμ΄ κ΅¬μμ§λ©΄ μ€νΈλ§μ, λ§κ·Έλ§κ° κ΅³μ νμ±μμ΄ κ΅¬μμ§λ©΄ μ νΈλ§μμ΄ λ©λλ€. μμ΄ λ²μ: It is classified into different types depending on the raw materials. When sedimentary rocks like mud are baked, they become paragneiss; when igneous rocks solidified from magma are baked, they become orthogneiss. (0:41) * νκΈ μλ¬Έ: λ μ κΉμ΄ 묻νκ³ μμ²λ μ΄κ³Ό μλ ₯μ λ°κ³ μ¬μ§μ΄ μ΄μ§ λ ΉκΈ°κΉμ§ νλ μ΄ λ§λ² κ°μ μΈ λ¨κ³. μμ΄ λ²μ: These three magical stages: being buried deep underground, enduring extreme heat and pressure, and even slightly melting. (0:47) * νκΈ μλ¬Έ: 보μΈμ, μ§νμ μμ²λ μλ ₯μ΄ λ¨λ¨ν λ°μλ₯Ό μ°°νμ²λΌ λ§κ΅¬ ꡬλΆλ €μ μ λ° κΈ°λ§ν λ¬Όκ²° 무λ¬λ₯Ό λ§λ κ²λλ€. μμ΄ λ²μ: Look at this. The immense pressure underground bent the hard rock like clay, creating those amazing wavy patterns. (0:56) * νκΈ μλ¬Έ: μ¨λκ° νκ³μΉλ₯Ό λμΌλ©΄ λ°μκ° μ΄μ§ λ Ήλ λ―Έκ·Έλ§νμ΄νΈνκ° μΌμ΄λμ. μ΄λ λ°κ³ μ΄λμ΄ κ΄λ¬Όλ€μ΄ μ« λΆλ¦¬λμ£ . μμ΄ λ²μ: When the temperature exceeds the limit, migmatization occurs, where the rock melts slightly. At this point, the light and dark minerals separate completely. (1:05) * νκΈ μλ¬Έ: μ, κ·ΈλΌ μ΄ μ§μμ λ°νμΌλ‘ μμ μλΆμ§μ νΈλ§μλ€μ μ§μ§ κ³ ν₯μ νλ² μΆμ ν΄λ³ΌκΉμ? μμ΄ λ²μ: Now, based on this knowledge, shall we trace the true hometown of the gneisses in the western area of Yeongwol? (1:11) * νκΈ μλ¬Έ: λλκ²λ μ΄ μ μ₯ν λ°μλ€μ μ§μ§ μ 체λ μμ£Ό λ¨Ό μλ λ°λ€ λ°μ μμΈ νλ²ν λͺ¨λμ μ§νμ΄μμ΅λλ€. μμ΄ λ²μ: Surprisingly, the true identity of these grand rocks was just ordinary sand and mud deposited under the sea a very long time ago. (1:20) * νκΈ μλ¬Έ: νν λͺ¨λμλ μ¬μ§μμ λ¨κ±°μ΄ μ΄μ λ°μ λ°μ§λ°μ§ λΉλλ λ°±μ΄λͺ¨ νΈλ§μμΌλ‘ μλ²½νκ² ν골νννμ΅λλ€. λλ¨νμ£ ? μμ΄ λ²μ: The psammitic rock, which used to be common sand, was exposed to intense heat and completely transformed into sparkling muscovite gneiss. Amazing, isn't it? (1:31) * νκΈ μλ¬Έ: λ°λ©΄ μ§νμ΄μλ μ΄μ§μμ μ§κ΅¬μ μ€λΈ μμμ ν¨μ¬ λ μ€νν°ν΄ν λ³μ κ³Όμ μ κ±°μΉκ² λ©λλ€. μμ΄ λ²μ: On the other hand, pelitic rock, which used to be mud, undergoes a much more spectacular transformation process inside the Earth's oven. (1:36) * νκΈ μλ¬Έ: μ§νμ΄ κ°νκ² κ½ λ리면 μ°μ μ΄λ κ² μ§κ³ μ λͺ ν μ€λ¬΄λ¬λ₯Ό λ½λ΄λ νμ΄λͺ¨ νΈλ§μμΌλ‘ 1μ°¨ λ³μ μ νκ³ μ. μμ΄ λ²μ: When mud is compressed tightly, it first undergoes a primary transformation into biotite gneiss, boasting these dark and vivid stripes. (1:44) * νκΈ μλ¬Έ: κ±°κΈ°μ μ¨λκ° ν λ μ¬λΌκ° μ΄μ§ λ Ήμλ²λ¦¬λ©΄ λ§μΉ¨λ΄ μ 볡μ‘ν 무λ¬μ λ―Έκ·Έλ§νμ΄νΈμ§ νΈλ§μμ΄ λλ κ²λλ€. μμ΄ λ²μ: When the temperature rises even further and it melts slightly, it finally becomes that intricately patterned migmatitic gneiss. (1:52) * νκΈ μλ¬Έ: μ κΈ° νμ λ λ€ λ³΄μ΄μμ£ ? μ κ±Έ λ₯μ½μμ΄λΌκ³ λΆλ₯΄λλ° μμ λ΄λΆμμ μ§μ§ νν λ Ήμλ νκ°μμ§ μ±λΆμ΄μμ. μμ΄ λ²μ: See those white bands over there? They are called leucosomes, and they are granitic components that actually melted completely inside the rock. (2:00) * νκΈ μλ¬Έ: κ·ΈλΌ λͺ¨λμ μ§νμ΄ μ΄λ° κ²½μ΄λ‘μ΄ μμ μνμΌλ‘ λ°λλλ° λλ체 μΌλ§λ κ±Έλ ΈμκΉμ? νλ² λ§μΆ°λ³΄μΈμ. μμ΄ λ²μ: So, how long on earth did it take for sand and mud to turn into such wondrous works of art? Take a guess. (2:07) * νκΈ μλ¬Έ: μ λ΅μ λ¬΄λ € 18μ΅ 6μ²λ§ λ μ λλ€. μ μ λ§ μ μ΄ λ‘ λ²μ΄μ§λ μλμ μΈ μκ° μλλκΉ? μμ΄ λ²μ: The answer is a whopping 1.86 billion years. Wow, isn't that a jaw-dropping, overwhelming amount of time? (2:15) * νκΈ μλ¬Έ: 20μ΅ λ μ λ°λ€μ μ§νμ΄ μμ΄κ³ 18μ΅ 6μ²λ§ λ μ μ΅κ³ μ‘°λ‘ κ΅¬μμ§κΈ°κΉμ§ κ·ΈμΌλ§λ‘ μ§κ΅¬μ λμμ¬μμ£ . μμ΄ λ²μ: From mud accumulating in the ocean 2.0 billion years ago to being baked at its peak 1.86 billion years ago, it is truly an epic story of the Earth. (2:22) * νκΈ μλ¬Έ: κ·Έλμ λ°μλ κ·Έλ₯ λλ©μ΄κ° μλλλ€. μμ²λ μ΄κ³Ό μλ ₯μ 견λλΈ μ§κ΅¬μ μμν μΌκΈ°μ₯μ΄κ±°λ μ. μμ΄ λ²μ: That's why rocks are not just lumps of stone. They are the Earth's vivid diaries that have endured immense heat and pressure. (2:30) * νκΈ μλ¬Έ: μ¬λ¬λΆ κΈΈμ κ±·λ€ λ¬΄μ¬μ½ λ°λ λλ©©μ΄ μμ μ΄λ€ 10μ΅ λ μ λΉλ°μ΄ μ¨μ΄ μμμ§ μ΄μ μμμ΄ κ°μλμ? μμ΄ λ²μ: Now, can you imagine what kind of billion-year secrets might be hidden inside the pebble you casually step on while walking down the street?
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