Luyện nói tiếng Anh bằng Shadowing qua video: Rock Cycle | Igneous | Metamorphic | Sedimentary Rock
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115 câu
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Rocks are all around us, and every rock you see used to be different.
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Over time rocks change.
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They break down, wear away, or even mount, but never disappear.
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How do rocks transform from this to this?
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Let's find out together in this episode all about the rock cycle.
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There are three types of rock found on Earth.
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Metamorphic, sedimentary, and igneous rock.
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We can classify each type of rock by how it was formed.
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Sometimes rocks form quickly, like when an erupting volcano spews molten rock into the air.
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And sometimes they change slowly, like when a rock is heated and compressed below
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Earth's surface for thousands or even millions of years.
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When you're looking at a rock, you're looking at history.
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Rocks may all seem the same at first, but they're all different and complex.
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The rock cycle shows how each type is formed in a different way, or how Earth's materials, driven by energy flow, change over time through melting,
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crystallization, weathering, erosion, and deformation.
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Within the Earth's crust and beneath the surface is molten rock
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or magma that can cool and solidify and turn into igneous rock.
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Let's take a look at Earth's layers to help us understand how this is possible.
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The Earth is made up of several layers that go all the way down to its core.
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The top layer of the Earth is slowly moving and shifting and is called the lithosphere.
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This layer consists of the Earth's crust and part of the upper mantle and makes up the tectonic plates, sometimes called lithospheric plates.
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These tectonic plates are being pushed together, pulled apart, or sliding past each other along surface faults.
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These movements are what create mountain ranges, seafloor trenches, and volcanoes.
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On the west coast of the United States, two plates are converging.
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The Pacific Plate is going underneath the North American Plate and begins to melt as it moves farther and farther down,
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eventually forming Mount Rainier and Mount St. Helens, which are active volcanoes.
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Old Oceanic Crust is constantly being recycled in the subduction zones.
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This is where Oceanic Crust, being more dense, is subducted or sinks below the continental crust where it melts and is recycled into the mantle.
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Volcanoes like this are a great place to find molten rock and igneous rock.
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You can see this action modeled here.
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At the bottom of this beaker, I have wax to represent magma under the crust.
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A layer of sand is resting on top to represent a thin layer of oceanic crust.
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As the magma rises, it cools and solidifies.
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When magma comes to the surface, it makes brand new rocks.
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Any new rock that has changed from molten to solid is an igneous rock.
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Igneous rocks make up about 90 % of Earth's crust, though you may not notice because they are covered up by other rocks, soil, or ocean.
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One common kind of igneous rock is granite.
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Behind me is enchanted rock.
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A massive 425 5 foot high, 1 .1 billion year old pink granite dome.
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Here is an exfoliated piece for us to get a closer look.
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Another type of igneous rock is this obsidian, which is smooth and glassy.
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Both of these rocks were made of molten rock, so why do they look so different?
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Depending on whether magma cools above or below
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Earth's surface will determine the type of igneous rock that is formed.
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When magma cools and solidifies beneath
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Earth's surface, it forms intrusive igneous rock.
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This granite is intrusive igneous rock.
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It has only been exposed by erosion or the removal of the surrounding rock.
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Intrusive rocks like this cool slowly so they have more time for larger mineral crystals to form,
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which is why granite looks coarse -grained and we can see the crystals even without a microscope.
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When magma erupts to the surface, we call it lava.
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After lava cools and solidifies, it becomes extrusive igneous rock.
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This obsidian is volcanic glass formed when lava cools rapidly with minimal crystal growth.
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If you're still here liking this video, let us know
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And hit that subscribe button so you never miss an episode.
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Once an igneous rock like granite is created, its journey isn't over.
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The rock begins to change through a process called weathering.
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Weathering wears away at exposed surfaces over time.
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It's the breakdown of rocks and minerals into smaller pieces or sediments.
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Brushing water in rivers can wear down sharp edges on rocks over time.
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High temperatures cause rock to expand, and falling temperatures cause rock to contract.
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As this cycle happens over and over again, the structure of the rock weakens.
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Eventually, the outer layers flake off in thin sheets, a process called exfoliation.
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That's what is happening here.
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You can see the curved cracks in peeling sheets.
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Looks a bit like a giant rock onion.
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All this sediment can be moved around or eroded by wind and water.
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Eventually, it will be deposited somewhere, joining sediment from other rocks at the bottom of a riverbed, lake, or ocean.
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Under the right circumstances, sediments can form into sedimentary rock.
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All the material in this sandstone once belonged to other rocks.
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These sedimentary rocks behind me were formed over 250 million years through the deposition of sediments in ancient seas and rivers,
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creating layers of red shale, sandstone, and gypsum.
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Rocks like these are formed when sediments undergo lithification.
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Before lithification can occur, we need sediments.
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So I'm going to create some candy sediments.
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This is taking a long time, so let's speed it up.
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That's better.
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The first step to lithification is called deposition.
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This is when sediment is deposited in a new location and it spreads out to form a layer.
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As more and more layers are created, the layers underneath them become pressed together.
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This is called compaction.
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Minerals settle between the sediment particles which makes everything stick together.
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This is called cementation, like cement.
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This is now our candy sedimentary rock.
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You can see the layers we started with the white and ended with the green.
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With enough heat or pressure, a metamorphic rock can be formed from any other type of rock,
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igneous, sedimentary, or even other metamorphic rocks.
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All of the minerals in the original rock recrystallize without having to melt down back into molten rock.
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The new metamorphic rocks are typically harder, more compact, and more resistant to weathering.
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Metamorphic means it's changed.
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We can create metamorphic rock with our sedimentary candy rock by adding heat and pressure.
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First, I'm going to use an old hairdryer to heat things up.
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Now, squishing action.
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Pressure!
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Squish!
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Pressure!
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Our sedimentary rock is now a metamorphic rock.
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These pink rock islands jutting up through the limestone are metamorphic rocks called valley spring gneiss.
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Intense heat and pressure applied to the original rocks over millions of years formed gneiss.
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The original rocks were sedimentary and igneous, likely granite.
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Rocks really never go away.
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They're changed and reused over time.
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This metamorphic rock can be heated up until it becomes like liquid lava.
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Once it cools, it's now an igneous rock.
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Back to the beginning.
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There are many pathways through the rock cycle.
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Metamorphic rocks and sedimentary rocks can become igneous rocks when they're melted and then cooled.
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Igneous rocks and sedimentary rocks can become metamorphic rocks when they're exposed to high heat and pressure.
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Igneous and metamorphic rocks can become sedimentary rocks if they're broken apart into sediments and go through lithification.
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So the next time you spot an interesting rock, see if you can tell.
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Is it sedimentary, igneous, or metamorphic?
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And if you want to learn more science you can check out this video next.
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Pressure!
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Squish!
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Pressure!
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Từ vựng và ghi chú luyện nói cho bài học này
Những từ được nhắc lại nhiều nhất trong bài: rock, igneous, metamorphic, sedimentary, layer. Video này có 115 câu và 1278 từ để luyện shadowing. Phần lời nói dài 9:01. Người nói giữ tốc độ đều, khoảng 142 từ mỗi phút, vừa sức để nói đuổi theo. Chỉ 74% số từ nằm trong 3.000 từ tiếng Anh thông dụng nhất, nên từ vựng khá khó.
Từ vựng quan trọng trong video
15 từ đáng học trong video, kèm phiên âm và nghĩa:
| Từ | Phiên âm | Nghĩa |
|---|---|---|
| layer danh từ | /ˈleɪ̯ɚ/ | lớp |
| melt động từ | /mɛlt/ | tan, tan chảy |
| granite danh từ | /ˈɡɹæn.ɪt/ | đá hoa cương |
| mineral danh từ | /ˈmɪn.ə.ɹəl/ | khoáng sản, khoáng vật |
| volcano danh từ | /vɑlˈkeɪ.noʊ/ | núi lửa, hoả diệm sơn |
| lava danh từ | /ˈlɑvə/ | dung nham |
| crystal danh từ | /ˈkɹɪstəl/ | tinh thể, pha lê |
| candy danh từ | /ˈkæn.di/ | kẹo |
| thin tính từ | /ˈθɪn/ | mỏng, mảnh |
| sheet danh từ | /ʃit/ | tờ |
| erosion danh từ | /ɪˈɹəʊʒən/ | xói mòn |
| sandstone danh từ | /ˈsændˌstoʊn/ | sa thạch |
| sharp tính từ | /ʃɑɹp/ | sắc, bén |
| occur động từ | /əˈkɜː/ | xảy ra |
| sand danh từ | /sænd/ | cát |
Cụm động từ bạn sẽ nghe
| Từ | Nghĩa |
|---|---|
| break down động từ | hỏng, hỏng hóc |
| check out động từ | tính tiền, trả phòng |
Ngữ pháp trong video
Những cấu trúc người nói dùng nhiều nhất, kèm đúng cụm từ trong video:
| Cấu trúc | Trong video |
|---|---|
| Câu bị động be + quá khứ phân từ — nhấn vào việc xảy ra, không phải người làm | was formed · is heated · is formed |
| Mệnh đề quan hệ who / which + mệnh đề — thêm thông tin về người hoặc vật | Helens, which are · obsidian, which is · particles which makes |
| Thì hiện tại hoàn thành have/has + quá khứ phân từ — việc đã xảy ra nhưng còn liên quan đến hiện tại | has changed · has only been exposed |
Phát âm cần chú ý
Người nói dùng 11 dạng rút gọn, ví dụ they're, you're, I'm. Hãy nói theo dạng ngắn đúng như bạn nghe.
- Âm “th”: thin /ˈθɪn/, beneath /bɪˈniːθ/, underneath /ˌʌndɚˈniθ/, smooth /smuːð/, pathway /ˈpæθˌweɪ/
- Âm “sh” và “zh”: sheet /ʃit/, erosion /ɪˈɹəʊʒən/, deposition /ˌdɛp.əˈzɪʃ.ən/, sharp /ʃɑɹp/, brush /bɹʌʃ/
- Từ dài — đặt trọng âm cho đúng: deposition /ˌdɛp.əˈzɪʃ.ən/, metamorphic /ˌmɛt.əˈmɔɹ.fɪk/, sedimentary /ˌsɛd.əˈmɛn.tə.ɹi/, lithification /ˌlɪθɪfɪˈkeɪʃən/, solidify /səˈlɪdɪˌfaɪ/
Những âm người Việt thường gặp khó:
- Cụm phụ âm cuối — đọc đủ từng âm, đừng nuốt âm cuối: melt /mɛlt/, crust /kɹʌst/, mount /maʊnt/, sharp /ʃɑɹp/, sand /sænd/
- Âm /tʃ/, /dʒ/ và /ʒ/ — tiếng Việt không có, đừng đọc thành “ch” hay “gi”: erosion /ɪˈɹəʊʒən/, trench /ˈtɹɛnt͡ʃ/, converge /kənˈvɜːd͡ʒ/, enchant /ɪnˈt͡ʃænt/, gypsum /ˈd͡ʒɪp.səm/
- Âm /æ/ — mở miệng rộng hơn âm “e”: granite /ˈɡɹæn.ɪt/, candy /ˈkæn.di/, mantle /ˈmæn.təl/, sandstone /ˈsændˌstoʊn/, sand /sænd/
Cách luyện với video này
- Nghe hết video một lần, chưa cần nói, và ghi lại những từ bạn chưa biết.
- Nói đuổi từng câu ở tốc độ bình thường, lặp lại mỗi câu đến khi nhịp của bạn khớp với người nói.
- Ghi âm giọng mình rồi so với bản gốc, chú ý các từ như layer, melt, granite.
Phương Pháp Shadowing Là Gì?
Shadowing là kỹ thuật học ngôn ngữ có cơ sở khoa học, ban đầu được phát triển cho chương trình đào tạo phiên dịch viên chuyên nghiệp và được phổ biến rộng rãi bởi nhà đa ngôn ngữ học Dr. Alexander Arguelles. Nguyên lý cốt lõi đơn giản nhưng cực kỳ hiệu quả: bạn nghe tiếng Anh của người bản xứ và lặp lại to ngay lập tức — như một "cái bóng" (shadow) đuổi theo người nói với độ trễ chỉ 1–2 giây. Khác với luyện ngữ pháp hay học từ vựng bị động, Shadowing buộc não bộ và cơ miệng phải đồng thời xử lý và tái tạo ngôn ngữ thực tế. Các nghiên cứu khoa học xác nhận phương pháp này cải thiện đáng kể phát âm, ngữ điệu, nhịp điệu, nối âm, kỹ năng nghe và độ lưu loát khi nói — đặc biệt hiệu quả cho người luyện IELTS Speaking và muốn giao tiếp tiếng Anh tự nhiên như người bản ngữ.