Практика Shadowing: The Deepest Point in the World: Crash Course Geology #12 - Изучайте разговорный английский по видео
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135 предложений
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It's about to get freaky.
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Gargantuan tube worms, foot-long clams, shrimp with eyes that can detect radiation, and I'm not talking about the special at Red Lobster.
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These are just a few of the stranger-than-fiction creatures you can find in the deep, dark depths of the ocean.
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The ocean is teeming with life, even its most hostile parts.
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It fosters the most spectacular and diverse life forms imaginable, including us.
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Just because we live on land doesn't mean we're not homies with their salty neighbors, okay?
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So how does she do it?
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What makes the ocean so lifey?
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Hi, I'm Sage, and this is Crash Course Geology.
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The ocean!
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More than 70% of our planet is covered in this enormous salty plankton-filled wonderland.
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Seriously, there's a lot of plankton in there.
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We've been fascinated by this massive body of water for centuries.
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One of the earliest studies of the ocean started in 1872
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when the British HMS Challenger hit the seas for a 1,250-day journey that covered over 68,000 nautical miles.
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You could consider it an early feat of oceanography, the study of physics, chemistry, biology, and geology of the oceans.
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Later, tools like sonar, submarine satellites, and submersibles let us gather data from above and send stuff below.
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Everything from cameras to robots to Titanic director James Cameron.
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Voluntarily, of course, he was really vibing down there.
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So today we know quite a bit about the ocean.
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And it isn't just one uniform mass of salt water.
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Some parts are way saltier than others, or way hotter or way colder.
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Some parts are home to thousands of species, while others support almost none at all.
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And when it comes to the seafloor, it's not just flat and sandy.
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There's a lot going on with the ocean's bathymetry, or the topography of the ocean floor.
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Now I can't take you on a tour of it.
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The crash course budget is a little too tight for a full-on submersible, but I bet I know someone who would make the trip.
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Duane, you want to go on a little adventure?
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Duane starts his journey on the coast, where the land meets the sea.
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As he strikes out onto the sea floor, he'll roll along the continental shelf, a part of the ocean floor that's still continental crust.
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stretched out and topped with a thick layer of sediment accumulated over thousands of years.
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Continental crust is thicker and more buoyant than oceanic crust, so it floats higher on top of the mantle.
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Combined with the thick layer of sediments, the ocean is shallower on the shelf, usually less than 200 meters deep.
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Here you'll find algae, seaweed, and tons of different kinds of fish and sea creatures.
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From here, things go downhill fast.
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That's the continental slope, the transition zone between the continental shelf and the deeper basin of the ocean.
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It's made of thinner, denser oceanic crust.
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A few kilometers under the surface, it starts to smooth out again, in an area called the Continental Rise, a zone of sediments accumulated at the base of the slope.
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And when Duane hits the end, he'll find himself in.. the abyss.
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Or at least, the abyssal plain.
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No, don't worry, pal.
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You have location sharing on.
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We won't lose you out there.
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The abyssal plain is the flat-ish bottom of the ocean basin.
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It's mostly made of volcanic rock called basalt and covered in a layer of sediment.
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It tends to hover around 4.5 kilometers deep.
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Here, it's hard for much of anything to survive.
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It's cold, it's dark, and the pressure is up to 600 times what it is on the surface.
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It's okay, Dwayne can handle it.
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Regardless of where you dive in, there are plenty of cool landforms to explore under the sea.
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Like submarine canyons.
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When the sea level is low, they're carved by rivers cutting through the continental shelf and slope.
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Then they're deepened by submarine avalanches called turbidity currents.
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And there are underwater volcanoes called seamounts where violent submarine volcanic eruptions built up mountains on the sea floor.
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You'll find lots of unique sea life here, from bubblegum coral and squat lobsters to loggerhead sea turtles and rare psi whales.
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Alright buddy, time to come to the surface.
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Come on out of the water!
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Now, Duane just took a trip along a passive margin, which is where the continental crust meets an oceanic crust on the same tectonic plate.
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Pretty chill.
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But if he had toured, say, South America's western coast, he would have found a much narrower continental shelf at an active margin.
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That's the edge of a tectonic plate where lots of earthquakes rattle the sea floor.
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Yeah, I'm not gonna put you through that, bud.
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And there are other things I'd worry about if Duane had kept wandering the bottom of the ocean, like hydrothermal vents.
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They're underwater chimneys as high as 55 meters
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that send up blackened plumes of particles and water hot enough to melt solid metal.
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Can you imagine if that's what happened when they picked a new pope?
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Hydrothermal vents are created by plate tectonics, the theory that Earth's outermost layer is broken up into chunks, called tectonic plates, that move across the mantle.
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We got way more into plate tectonics in an earlier episode, but the important thing to note today is that it plays a big role in marine geology.
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One place hydrothermal vents form is where oceanic plates pull apart.
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Here's Here's how that happens.
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At these divergent boundaries, lava erupts in the gaps and then cools and hardens into new oceanic crust, or seafloor.
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All that tectonic movement can crack deep fissures in the crust, where water and magma mix.
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The liquid heats up, dissolving minerals from the surrounding rocks.
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And when that superheated fluid comes back up and meets the frigid temperatures at the seafloor, the minerals form stubby spires and towering chimneys. And voila!
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A hydrothermal vent!
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You'll find a lot of them along underwater mountain ranges called mid-ocean ridges.
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Hydrothermal vents pump heat from deep in the Earth into the oceans, creating hot, mineral-rich zones for super weird creatures to call home.
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That and the fact that these vents are often so deep in the ocean that there's no light for photosynthesis.
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Instead, bacteria are chemosynthetic, meaning they feed on the chemicals from the vents, and they serve as the base for the food chain there.
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Two-meter-long tube worms, orange-shelled mussels, and fuzzy crabs all happily thrive around hydrothermal vents.
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Marine geologists study these ecosystems to try to figure out how life began on Earth, and how it might exist on other planets.
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Like, some research has found primitive microorganisms living by hydrothermal vents, a sign that life could have started in those environments.
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And if chemical-eating organisms can exist in hostile Earth environments, maybe they can survive elsewhere in the solar system, too.
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Hydrothermal vents can also form convergent boundaries, where a continental plate and an oceanic plate collide, plunging one into the mantle beneath the other.
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That process creates a trench, which forms as one plate dives beneath the other, bending the seafloor to create a deep V-shaped depression.
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And if that happens with two oceanic plates, the trench is massive.
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That's how we got the Challenger Deep, the deepest point in the world, located in the Pacific's Mariana Trench.
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It reaches nearly 11,000 meters below sea level,
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so deep that Mount Everest could fit inside with room to spare.
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Well, at least that's how deep we think it is, because it turns out measuring it is surprisingly difficult.
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Since the HMS Challenger, we've been trying to measure it, starting with a weighted rope and then graduating to sonar technology in the 50s.
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The most accurate estimates as of filming in 2026 came from a series of submersible dives in 2020, which clocked it at 10,935 meters deep.
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But it's hard to know for sure.
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We can't exactly drop a yardstick down there to get an exact answer.
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What we do know is that just like at hydrothermal vents, life exists in deep sea trenches.
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And that life is weird with a capital W.
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We're talking transparent sea cucumbers, saucer-sized single-celled organisms, and shrimp-like critters that eat sunken wood.
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But the ocean's geology doesn't just create hot spots for life on the sea floor.
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It affects life everywhere on Earth, especially through currents.
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Currents are continuous, directed oceanic movements that carry water across the globe.
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They're driven by wind, water density, tides, and Earth's rotation, and they're affected by bathymetry, which can change their speed and direction.
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For example, about three million years ago, tectonic shifts formed the Isthmus of Panama, which connected North and South America.
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This stretch of land deflected the warm, salty ocean current that once flowed through the gap.
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It redirected that water northward, which warmed up Europe.
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And currents can have a cooling effect, too, like when Antarctica broke off from South America.
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This allowed frigid waters to circle the continent, creating a barricade for warmer waters and chilling Antarctica into the frozen landscape we know today.
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One of the most important contributions of ocean currents is the distribution of nutrients.
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Upwelling currents bring nutrient-rich waters from deep in the ocean upward to feed microorganisms at the base of marine food webs.
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Currents can even move animals themselves, like a watery superhighway, distributing populations of everything from plankton to fish eggs to sea turtle hatchlings,
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influencing how these creatures evolve.
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Oceans pump tons of water around the globe in a so-called global conveyor belt of currents, mostly driven by changes in temperature and saltiness.
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Basically, water that's saltier and colder is more dense and sinks, traveling along the deep ocean bottom,
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while water that's less salty and warmer is less dense and upwells.
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But as we unleash greenhouse gases into the atmosphere,
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arctic temperatures are warming, which means ocean waters are cooling slower and glaciers are melting faster, flushing fresh water into the mix.
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All of that slows down the conveyor belt.
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The ocean also acts as a huge carbon sink, storing carbon dioxide so that it doesn't warm the atmosphere.
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That's a massive deal for a lot of reasons.
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Like, the temperature of the Earth determines what kind of creatures can live here, including us.
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But as surface water warms and currents slow, the surface waters saturate with carbon dioxide and can't absorb anymore.
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Many scientists recommend cutting carbon emissions to prevent large-scale disruption of currents and ocean environments.
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You can learn more about that in Crash Course Climate and Energy.
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Earth's oceans are still full of mysteries.
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As of June 2024, we've only mapped about a quarter of the world's seafloor in high resolution.
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That means there's a whole three quarters that could still be hiding even more creepy little Earth aliens.
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Dwayne wants to see more of those fuzzy crabs.
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The ocean is much more than a big pool of salt water, and the seafloor isn't just an underwater sandy beach either.
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The bottom of the ocean is a maze of slopes, trenches, and formations that show us plate tectonics in action.
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It creates habitats for creepy creatures and affects the currents that are essential to Earth's climate and life.
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Our planet wouldn't be the same without it.
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In our next episode, we'll tackle volcanoes.
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See you then.
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Thanks for watching this episode of Crash Course Geology, which was filmed in our studio in Indianapolis, Indiana and was made with the help of all these nice people.
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If you want to help keep Crash Course free for everyone, forever.
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You can join our community on Patreon.
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Что вы узнаете
Этот видеоролик поможет вам улучшить разговорный английский, тренируя восприятие быстрой речи и умение выражать сложные идеи простым языком. Вы научитесь различать интонационные паттерны при объяснении географических концепций (например, "continental shelf" или "abyssal plain") и практикуете разговорные формулы для привлечения внимания (например, "It's about to get freaky"). Также это отличная возможность для тренировки shadowing английский — повторения речи за спикером, чтобы улучшить произношение и ритм.
Слушайте, как соединяются звуки
В диалоге часто встречаются связки и редукции, которые делают речь естественной. Например, "it's not just" превращается в /ɪts nɑːt dʒʌst/, а "what makes" sounds like /wɑːt meɪks/. Обратите внимание на сокращения: "I'm not" → /aɪm nɑːt/, "don't worry" → /doʊnt ˈwɜːri/. Эти детали помогут вам лучше понимать быструю речь и говорить так, как это делают носители.
Говорите, как.native
Чтобы подражать ритму спикера, обратите внимание на ударения. В фразах типа "the ocean is teeming with life" основной удар падает на "teeming" и "life". Используйте подъем интонации в вопросах: "So how does she do it?" — здесь интонация поднимается на "do". Для тренировки используйте метод shadowspeak: повторяйте фразы сразу после спикера, стараясь совпадать по темпу и силе голоса. Это эффективно улучшить произношение английского и научиться говорить естественно. Практикуйте каждый день, и вы заметите прогресс в разговорном английском — учить английский с YouTube никогда не было так удобно!
Грамматика в этом видео
Конструкции, которые говорящий использует чаще всего, с точными словами из видео:
| Конструкция | В видео |
|---|---|
| Придаточные определительные who / which + предложение — уточнение о человеке или предмете | someone who would · margin, which is · bathymetry, which can |
| Пассивный залог be + причастие прошедшего времени — важно, что происходит, а не кто это делает | is covered · We've been fascinated · are created |
| Present Perfect have/has + причастие прошедшего времени — прошлое действие, важное сейчас | We've been fascinated · has found · we've only mapped |
Что такое техника Shadowing?
Shadowing — это научно обоснованная техника изучения языка, изначально разработанная для подготовки профессиональных переводчиков и популяризированная полиглотом доктором Александром Аргуэльесом. Метод прост, но эффективен: вы слушаете аудио на английском от носителей языка и немедленно повторяете вслух — как тень, следующая за говорящим с задержкой в 1–2 секунды. В отличие от пассивного прослушивания или грамматических упражнений, Shadowing заставляет мозг и мышцы рта одновременно обрабатывать и воспроизводить реальные речевые паттерны. Исследования показывают, что это значительно улучшает точность произношения, интонацию, ритм, связную речь, понимание на слух и беглость речи — что делает его одним из самых эффективных методов для подготовки к IELTS Speaking и реального общения на английском.