<p>The subduction zones are more easily spotted by the phenomena they cause in the subsurface than their features on the surface. I found this schematic image which shows almost all the features, from <a href="https://www.researchgate.net/publication/318684905_The_Nahuel_Niyeu_basin_A_Cambrian_forearc_basin_in_the_eastern_North_Patagonian_Massif" rel="nofollow noreferrer">https://www.researchgate.net/publication/318684905_The_Nahuel_Niyeu_basin_A_Cambrian_forearc_basin_in_the_eastern_North_Patagonian_Massif</a> :
<a href="https://i.sstatic.net/Rggn5.png" rel="nofollow noreferrer"><img src="https://i.sstatic.net/Rggn5.png" alt="subduction zone"></a></p>

<p>So what you see is the thin black plate subducting under the grey continental rocks. There are two features that it causes in an indirect way.</p>

<ol>
<li><p>The first of those is the <a href="https://en.wikipedia.org/wiki/Forearc" rel="nofollow noreferrer">forearc basin</a>, which is a sometimes present region with thrust faults in the direction of the subduction point. Thus, there is a local basin with a lot of space for sedimentation.</p></li>
<li><p>The volcanism, then, is the most obvious and always-present feature. All the chemicals that the ocean floor brings into the Earth at relatively low temperature create a 'melt' that can eventually reach the Earth's surface.</p></li>
</ol>

<p>The reason why we don't see the actual subduction happening with our own eyes is because of the formation of the 'accretionary prism'. This is the triangle-shaped feature on the figure. It consists of sediment that is held on the interface between the moving oceanic plate and the stationary continental plate. It's a bit like a bulldozer. Hence, the real subduction action is covered by kilometers of piled up sediment! The deepest natural trench in the world, the Mariana Trench, is only about 11 km deep, while the continental plate is probably at least ~40 km deep. Hence, we don't really see the actual subduction in action...</p>

<p>If you have a shripwreck hulk and place it in the Mariana trench, it will get covered with sediment with a speed of <a href="https://scripps.ucsd.edu/biblio/provenances-distribution-and-accumulation-organic-matter-southern-mariana-trench-rim-and" rel="nofollow noreferrer">~0.02cm/year</a>, so assuming your ship is about 30 meters high it will take 150 000 years before it is covered and can become part of the accretionary prism. Then it has to be dragged into the Earth somehow. The Nazca plate moves at <a href="https://en.wikipedia.org/wiki/Nazca_Plate" rel="nofollow noreferrer">~5 cm/year</a>, so it'll be moved by 7.5 kilometers forward. As I wrote, it'll have to subduct at least 30 more kilometers before it's below any continental plate, which would take at least 600 000 years at the speed of the plate motion, and assuming that it somehow moves at the same speed as the crust rather than getting bulldozered into the accretionary prism. In other words, it would probably take much much longer in practice before it reached far enough down. As said, that means that in the meantime your space ship will have been chemically weathered and mechanically deformed (by the enormous mass of sediments), and won't really be recognizable as a space ship anymore!</p>

CC BY-SA 4.0
2019-05-23T06:42:12.313Z
2019-05-23T06:42:12.313Z
Erik
<p>Subduction zones are only observable indirectly through the typical volcanos in these regions (stratovulcanos like Krakatau or Pinatubo on the surface of the continental plate). Another form of typical subduction volcanos are the "Petit Spots" only described for the first time in 2001 by geologists from Japan. These litle volcanos appear under the water surface on top of the oceanic plate at the outer bulge of the oceanic plate.
This is because the real subduction area  lies normally about 3000-4000 metres below the surrounding ocean surface and is covered with sediments.
In most cases subduction is not a smooth and steady process but it proceeds with bigger or smaller earthquakes, depending on the material of the plates. </p>

<p>That means if you drop your spaceship in that zone it will be covered with a huge amount of sediments through the centuries, while at the same time these sediments in the deep sea trench compress the spaceship to a nice geological singularity. By the time it reaches the contact zone between oceanic plate and the continental plate it will be destroyed and with every little tug of the next earthquake it will be more pulverized and transported some centimetres further under the continental plate...</p>

CC BY-SA 4.0
2019-05-23T06:21:27.583Z
2019-05-23T06:21:27.583Z
Martina
<p>My understanding of plate tectonics is that in the middle of the oceans magma rises from the mantle of the earth, cools and then spreads out, building up the sea floor. These places are pretty obvious because they have lava coming out of them.</p>

<p>On the other hand, there are places that sink into the earth, <em>subduction zones</em>, where the reverse happens; the existing crust slides into the mantle. Is there any place where this is visible, like the lava, or does it only take place invisibly far below the surface?</p>

<p>For example, let's say I have an object, like a shipwreck hulk. If I put the hulk on the sea floor in a subduction zone will it get sucked into the earth and vanish? If so, how long would it take for it to disappear?</p>

CC BY-SA 4.0
2019-05-21T16:50:37.287Z
This was a plot point for David Brin's second Uplift trilogy: space refugees trying to protect future generations from discovery drop their starships into a subduction zone. But given that that the "conveyor belt" mechanism only moves a few centimeters per year and you'd be dropping your hulk onto a thick layer of sediment, seems likely the hulk would corrode long before it's dragged under.
jeffronicus
<plate-tectonics>
Is there a place where the sea floor descends into the mantle of the earth?
Tyler Durden
# Is there a place where the sea floor descends into the mantle of the earth?

(Asked by: username_0 on 2019-05-21)

My understanding of plate tectonics is that in the middle of the oceans magma rises from the mantle of the earth, cools and then spreads out, building up the sea floor. These places are pretty obvious because they have lava coming out of them.

On the other hand, there are places that sink into the earth, *subduction zones*, where the reverse happens; the existing crust slides into the mantle. Is there any place where this is visible, like the lava, or does it only take place invisibly far below the surface?

For example, let's say I have an object, like a shipwreck hulk. If I put the hulk on the sea floor in a subduction zone will it get sucked into the earth and vanish? If so, how long would it take for it to disappear?

**Tags:** plate-tectonics

> **Comments:**
> **username_1**: This was a plot point for David Brin's second Uplift trilogy: space refugees trying to protect future generations from discovery drop their starships into a subduction zone. But given that that the "conveyor belt" mechanism only moves a few centimeters per year and you'd be dropping your hulk onto a thick layer of sediment, seems likely the hulk would corrode long before it's dragged under.  

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## 2 answers

### Answer by username_2 on 2019-05-23. Score: 3

The subduction zones are more easily spotted by the phenomena they cause in the subsurface than their features on the surface. I found this schematic image which shows almost all the features, from <https://www.researchgate.net/publication/318684905_The_Nahuel_Niyeu_basin_A_Cambrian_forearc_basin_in_the_eastern_North_Patagonian_Massif> :
[![subduction zone](https://i.sstatic.net/Rggn5.png)](https://i.sstatic.net/Rggn5.png)

So what you see is the thin black plate subducting under the grey continental rocks. There are two features that it causes in an indirect way.

1. The first of those is the [forearc basin](https://en.wikipedia.org/wiki/Forearc), which is a sometimes present region with thrust faults in the direction of the subduction point. Thus, there is a local basin with a lot of space for sedimentation.
2. The volcanism, then, is the most obvious and always-present feature. All the chemicals that the ocean floor brings into the Earth at relatively low temperature create a 'melt' that can eventually reach the Earth's surface.

The reason why we don't see the actual subduction happening with our own eyes is because of the formation of the 'accretionary prism'. This is the triangle-shaped feature on the figure. It consists of sediment that is held on the interface between the moving oceanic plate and the stationary continental plate. It's a bit like a bulldozer. Hence, the real subduction action is covered by kilometers of piled up sediment! The deepest natural trench in the world, the Mariana Trench, is only about 11 km deep, while the continental plate is probably at least ~40 km deep. Hence, we don't really see the actual subduction in action...

If you have a shripwreck hulk and place it in the Mariana trench, it will get covered with sediment with a speed of [~0.02cm/year](https://scripps.ucsd.edu/biblio/provenances-distribution-and-accumulation-organic-matter-southern-mariana-trench-rim-and), so assuming your ship is about 30 meters high it will take 150 000 years before it is covered and can become part of the accretionary prism. Then it has to be dragged into the Earth somehow. The Nazca plate moves at [~5 cm/year](https://en.wikipedia.org/wiki/Nazca_Plate), so it'll be moved by 7.5 kilometers forward. As I wrote, it'll have to subduct at least 30 more kilometers before it's below any continental plate, which would take at least 600 000 years at the speed of the plate motion, and assuming that it somehow moves at the same speed as the crust rather than getting bulldozered into the accretionary prism. In other words, it would probably take much much longer in practice before it reached far enough down. As said, that means that in the meantime your space ship will have been chemically weathered and mechanically deformed (by the enormous mass of sediments), and won't really be recognizable as a space ship anymore!


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### Answer by username_3 on 2019-05-23. Score: 2

Subduction zones are only observable indirectly through the typical volcanos in these regions (stratovulcanos like Krakatau or Pinatubo on the surface of the continental plate). Another form of typical subduction volcanos are the "Petit Spots" only described for the first time in 2001 by geologists from Japan. These litle volcanos appear under the water surface on top of the oceanic plate at the outer bulge of the oceanic plate.
This is because the real subduction area lies normally about 3000-4000 metres below the surrounding ocean surface and is covered with sediments.
In most cases subduction is not a smooth and steady process but it proceeds with bigger or smaller earthquakes, depending on the material of the plates.

That means if you drop your spaceship in that zone it will be covered with a huge amount of sediments through the centuries, while at the same time these sediments in the deep sea trench compress the spaceship to a nice geological singularity. By the time it reaches the contact zone between oceanic plate and the continental plate it will be destroyed and with every little tug of the next earthquake it will be more pulverized and transported some centimetres further under the continental plate...


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