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Ocean Topology
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Eighth segment of the Ocean Odyssey describes Ocean Topography and where oil seepage comes from.
I'm here at VIMS with Ms. Masellus.
00:00:00
She's showing me the vessels they use to map and take core samples.
00:00:03
We learned that there are mountains and valleys on the ocean floor
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and that there's natural oil seepage.
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We need to know more about the topography of the ocean.
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Can you tell me exactly what the floor looks like?
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It's magnificent.
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Under the ocean, you can find the tallest mountains,
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the deepest valleys, and the flattest plains on Earth.
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Sounds fascinating, but I don't see any mountains or valleys when I swim.
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That's because where you swim is actually the continental shelf.
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This area is located along the edge of the continent
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and can extend 10 to 200 kilometers offshore.
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So are mountains the next area?
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No. Next comes the continental slope.
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It starts at the edge of the shelf and dips steeply until you reach the abyssal plain,
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which is one of the flattest areas on Earth.
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And the next area is where the tallest mountains are, right?
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Right. In the middle of the ocean, there are mountain ridges called mid-ocean ridges.
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This is where the seafloor is spreading apart, making new seafloor and building mountains.
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I learned about the seafloor spreading apart in the case of the shaky quake
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when we learned about plate tectonics.
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Very good. You'll also find volcanoes over those ridges and over hot spots in the Earth's crust.
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If a volcano grows tall enough to rise above sea level, they form islands.
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Just like the Hawaiian Islands. Didn't they form over a hot spot?
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That's right. And if a volcano doesn't break the surface of the water, then it's called a seamount.
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There are also deep ocean trenches.
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I always thought of the ocean as sandy.
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Under the ocean is a whole world just waiting to be discovered.
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And that's where the core samples come in.
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Why do you take core samples of the ocean floor?
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Seismic reflection images show buried ancient river channels located near here during the last ice age.
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Coring helps us to verify that they exist.
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It seems like we have another mystery, and we need your help.
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Sure thing. What can I do?
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Right now, we're trying to find out where the oil globs on our beach came from.
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Mr. Wells said that oil sometimes seeps out naturally from the ocean,
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so we need to learn more about oil seeps.
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Oil and gas can seep directly onto the surface of the earth or into the oceans.
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Are seeps very common?
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Yes, they're quite common.
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Did you know in California, every oil and gas field discovered between 1860 and the early 1900s
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was actually found by people seeing it seep up from the earth?
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So how does oil and gas seep out?
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Seeps can come from a single point or from as many as 30,000 individual little holes.
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Divers describe high seepage areas as looking like a whole bunch of gopher holes.
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How much oil and gas seeps out?
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It varies from place to place and can range from nearly impossible to detect
00:02:17
to thick oil films with globular deposits called tar balls.
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That sounds like what's on our beach.
00:02:24
We learned that most of the oil seepage occurs along the Gulf of Mexico,
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so we thought that a current could be carrying the oil globs to our beach.
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But we learned that there aren't any currents that carry things to Virginia from the Gulf of Mexico.
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What about the Gulf Stream?
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We know that the Gulf Stream flows northward from the central part of the Atlantic Ocean
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and turns back towards Europe up around Canada.
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So I don't think that's the answer.
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You might want to learn more about the Gulf Stream.
00:02:48
You're right. Maybe it is the Gulf Stream.
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Thanks, Ms. Vassalos.
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You're welcome. It's my pleasure to help out the treehouse detectives.
00:02:54
Let me show you something else.
00:02:56
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- Idioma/s:
- Niveles educativos:
- ▼ Mostrar / ocultar niveles
- Nivel Intermedio
- Autor/es:
- NASA LaRC Office of Education
- Subido por:
- EducaMadrid
- Licencia:
- Reconocimiento - No comercial - Sin obra derivada
- Visualizaciones:
- 585
- Fecha:
- 28 de mayo de 2007 - 15:34
- Visibilidad:
- Público
- Enlace Relacionado:
- NASAs center for distance learning
- Duración:
- 03′ 01″
- Relación de aspecto:
- 4:3 Hasta 2009 fue el estándar utilizado en la televisión PAL; muchas pantallas de ordenador y televisores usan este estándar, erróneamente llamado cuadrado, cuando en la realidad es rectangular o wide.
- Resolución:
- 480x360 píxeles
- Tamaño:
- 18.27 MBytes