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Migmatitic Gneiss in Youngwol, South Korea

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Metamorphic rocks in Youngwol, South Korea (0:00) * ν•œκΈ€ 원문: μ—¬λŸ¬λΆ„, λ°˜κ°‘μŠ΅λ‹ˆλ‹€. 였늘 μ‚΄νŽ΄λ³Ό 이 μžλ£Œμ—μ„  μ•„μ£Ό 였래된 λ°”μœ„λ“€μ΄ κ²ͺ은 λ†€λΌμš΄ μ—°κΈˆμˆ μ„ νŒŒν—€μ³λ³Ό κ²λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: Hello, everyone. In today's material, we are going to uncover the incredible alchemy experienced by ancient rocks. (0:08) * ν•œκΈ€ 원문: μš°λ¦¬κ°€ 맀일 밟고 λ‹€λ‹ˆλŠ” ν”ν•œ λŒλ©©μ΄λ“€, κ³Όμ—° 20μ–΅ λ…„ μ „μ—” μ–΄λ–€ λͺ¨μŠ΅μ΄μ—ˆμ„κΉŒμš”? 상상해 보신 적 μžˆλ‚˜μš”? μ˜μ–΄ λ²ˆμ—­: The common stones we step on every dayβ€”have you ever imagined what they looked like 2.0 billion years ago? (0:16) * ν•œκΈ€ 원문: 이걸 μ΄ν•΄ν•˜λ €λ©΄ λ³€μ„±μž‘μš©μ„ μ•Œμ•„μ•Ό ν•΄μš”. μ‰½κ²Œ 말해, 지ꡬ κΉŠμ€ 곳에 μžˆλŠ” μ—„μ²­λ‚œ μ••λ ₯의 κ±°λŒ€ν•œ 였븐이죠. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 이 뜨거운 μ˜€λΈμ—μ„œ ν‘Ή κ΅¬μ›Œμ Έλ‚˜μ˜¨ 결과물이 λ°”λ‘œ μ € λšœλ ·ν•œ μ€„λ¬΄λŠ¬, νŽΈλ§ˆμ•”μž…λ‹ˆλ‹€. 정말 λ©‹μ§€μ£ ? μ˜μ–΄ λ²ˆμ—­: The result of being thoroughly baked in this hot oven is that distinct striped rock right there: gneiss. Isn't it wonderful? (0:31) * ν•œκΈ€ 원문: μž¬λ£Œμ— 따라 μ’…λ₯˜λ„ λ‚˜λ‰˜λŠ”λ°μš”. 진흙 같은 퇴적암이 κ΅¬μ›Œμ§€λ©΄ μ€€νŽΈλ§ˆμ•”, λ§ˆκ·Έλ§ˆκ°€ ꡳ은 화성암이 κ΅¬μ›Œμ§€λ©΄ μ •νŽΈλ§ˆμ•”μ΄ λ©λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 땅속 깊이 묻히고 μ—„μ²­λ‚œ μ—΄κ³Ό μ••λ ₯을 λ°›κ³  심지어 살짝 λ…ΉκΈ°κΉŒμ§€ ν•˜λŠ” 이 λ§ˆλ²• 같은 μ„Έ 단계. μ˜μ–΄ λ²ˆμ—­: These three magical stages: being buried deep underground, enduring extreme heat and pressure, and even slightly melting. (0:47) * ν•œκΈ€ 원문: λ³΄μ„Έμš”, μ§€ν•˜μ— μ—„μ²­λ‚œ μ••λ ₯이 λ‹¨λ‹¨ν•œ λ°”μœ„λ₯Ό μ°°ν™μ²˜λŸΌ 마ꡬ κ΅¬λΆ€λ €μ„œ μ €λŸ° κΈ°λ§‰νžŒ λ¬Όκ²° 무늬λ₯Ό λ§Œλ“  κ²λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: Look at this. The immense pressure underground bent the hard rock like clay, creating those amazing wavy patterns. (0:56) * ν•œκΈ€ 원문: μ˜¨λ„κ°€ ν•œκ³„μΉ˜λ₯Ό λ„˜μœΌλ©΄ λ°”μœ„κ°€ 살짝 λ…ΉλŠ” λ―Έκ·Έλ§ˆνƒ€μ΄νŠΈν™”κ°€ μΌμ–΄λ‚˜μš”. μ΄λ•Œ 밝고 μ–΄λ‘μš΄ 광물듀이 μ«™ λΆ„λ¦¬λ˜μ£ . μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 자, 그럼 이 지식을 λ°”νƒ•μœΌλ‘œ μ˜μ›” μ„œλΆ€μ§€μ—­ νŽΈλ§ˆμ•”λ“€μ˜ μ§„μ§œ κ³ ν–₯을 ν•œλ²ˆ μΆ”μ ν•΄λ³ΌκΉŒμš”? μ˜μ–΄ λ²ˆμ—­: Now, based on this knowledge, shall we trace the true hometown of the gneisses in the western area of Yeongwol? (1:11) * ν•œκΈ€ 원문: λ†€λžκ²Œλ„ 이 μ›…μž₯ν•œ λ°”μœ„λ“€μ˜ μ§„μ§œ μ •μ²΄λŠ” μ•„μ£Ό λ¨Ό μ˜›λ‚  λ°”λ‹€ 밑에 μŒ“μΈ ν‰λ²”ν•œ λͺ¨λž˜μ™€ μ§„ν™μ΄μ—ˆμŠ΅λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: ν”ν•œ λͺ¨λž˜μ˜€λ˜ μ‚¬μ§ˆμ•”μ€ 뜨거운 열을 λ°›μ•„ 반짝반짝 λΉ›λ‚˜λŠ” 백운λͺ¨ νŽΈλ§ˆμ•”μœΌλ‘œ μ™„λ²½ν•˜κ²Œ ν™˜κ³¨νƒˆνƒœν–ˆμŠ΅λ‹ˆλ‹€. λŒ€λ‹¨ν•˜μ£ ? μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 반면 μ§„ν™μ΄μ—ˆλ˜ μ΄μ§ˆμ•”μ€ μ§€κ΅¬μ˜ 였븐 μ†μ—μ„œ 훨씬 더 μŠ€νŽ™ν„°ν΄ν•œ 변신과정을 거치게 λ©λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 진흙이 κ°•ν•˜κ²Œ 꽉 눌리면 μš°μ„  μ΄λ ‡κ²Œ μ§™κ³  μ„ λͺ…ν•œ μ€„λ¬΄λŠ¬λ₯Ό λ½λ‚΄λŠ” ν‘μš΄λͺ¨ νŽΈλ§ˆμ•”μœΌλ‘œ 1μ°¨ 변신을 ν•˜κ³ μš”. μ˜μ–΄ λ²ˆμ—­: When mud is compressed tightly, it first undergoes a primary transformation into biotite gneiss, boasting these dark and vivid stripes. (1:44) * ν•œκΈ€ 원문: κ±°κΈ°μ„œ μ˜¨λ„κ°€ ν™• 더 μ˜¬λΌκ°€ 살짝 녹아버리면 λ§ˆμΉ¨λ‚΄ μ € λ³΅μž‘ν•œ 무늬의 λ―Έκ·Έλ§ˆνƒ€μ΄νŠΈμ§ˆ νŽΈλ§ˆμ•”μ΄ λ˜λŠ” κ²λ‹ˆλ‹€. μ˜μ–΄ λ²ˆμ—­: When the temperature rises even further and it melts slightly, it finally becomes that intricately patterned migmatitic gneiss. (1:52) * ν•œκΈ€ 원문: μ €κΈ° ν•˜μ–€ 띠듀 λ³΄μ΄μ‹œμ£ ? μ €κ±Έ λ₯˜μ½”μ†œμ΄λΌκ³  λΆ€λ₯΄λŠ”λ° 암석 λ‚΄λΆ€μ—μ„œ μ§„μ§œ νŽ„νŽ„ λ…Ήμ•˜λ˜ ν™”κ°•μ•”μ§ˆ μ„±λΆ„μ΄μ—μš”. μ˜μ–΄ λ²ˆμ—­: See those white bands over there? They are called leucosomes, and they are granitic components that actually melted completely inside the rock. (2:00) * ν•œκΈ€ 원문: 그럼 λͺ¨λž˜μ™€ 진흙이 이런 경이둜운 μ˜ˆμˆ μž‘ν’ˆμœΌλ‘œ λ°”λ€ŒλŠ”λ° λ„λŒ€μ²΄ μ–Όλ§ˆλ‚˜ κ±Έλ Έμ„κΉŒμš”? ν•œλ²ˆ λ§žμΆ°λ³΄μ„Έμš”. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: 정닡은 무렀 18μ–΅ 6천만 λ…„μž…λ‹ˆλ‹€. 와 정말 μž…μ΄ λ–‘ λ²Œμ–΄μ§€λŠ” 압도적인 μ‹œκ°„ μ•„λ‹™λ‹ˆκΉŒ? μ˜μ–΄ λ²ˆμ—­: The answer is a whopping 1.86 billion years. Wow, isn't that a jaw-dropping, overwhelming amount of time? (2:15) * ν•œκΈ€ 원문: 20μ–΅ λ…„ μ „ 바닀에 진흙이 μŒ“μ΄κ³  18μ–΅ 6천만 λ…„ μ „ 졜고쑰둜 κ΅¬μ›Œμ§€κΈ°κΉŒμ§€ κ·Έμ•Όλ§λ‘œ μ§€κ΅¬μ˜ λŒ€μ„œμ‚¬μ‹œμ£ . μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: κ·Έλž˜μ„œ λ°”μœ„λŠ” κ·Έλƒ₯ λŒλ©μ΄κ°€ μ•„λ‹™λ‹ˆλ‹€. μ—„μ²­λ‚œ μ—΄κ³Ό μ••λ ₯을 κ²¬λŽŒλ‚Έ μ§€κ΅¬μ˜ μƒμƒν•œ 일기μž₯μ΄κ±°λ“ μš”. μ˜μ–΄ λ²ˆμ—­: 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) * ν•œκΈ€ 원문: μ—¬λŸ¬λΆ„ 길을 κ±·λ‹€ 무심코 λ°ŸλŠ” 돌멩이 μ•ˆμ— μ–΄λ–€ 10μ–΅ λ…„μ˜ 비밀이 μˆ¨μ–΄ μžˆμ„μ§€ 이젠 상상이 κ°€μ‹œλ‚˜μš”? μ˜μ–΄ λ²ˆμ—­: 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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