<p>No, we can't. This is because of several reasons, mostly stemming from the fact that the plates are not diverging fast enough to keep the lava hot enough before it cools down.</p>

<p>If we go and look on diverging plate boundaries on land, such as on Iceland or East Africa, you don't have a "line" of lava. Instead, you have individual volcanoes located along a linear trend:</p>

<p><a href="https://i.sstatic.net/MJph4.jpg" rel="noreferrer"><img src="https://i.sstatic.net/MJph4.jpg" alt="enter image description here"></a></p>

<p><sup>source: <a href="http://volcano.oregonstate.edu/vwdocs/volc_images/africa/africa.html" rel="noreferrer">http://volcano.oregonstate.edu/vwdocs/volc_images/africa/africa.html</a></sup></p>

<p>You see all the volcanoes along a line in the Ethiopia and Kenya region? It's not one "line of lava", but single volcanoes along a line.</p>

<p>If we think about divergent boundaries underwater, where the lava comes from a much shallower depth, we may think it might be possible to see this kind of feature. The problem is that water is extremely effective in cooling down lava. Here's an example video of what happens when there is lava underwater:</p>

<p><a href="https://www.youtube.com/watch?v=hmMlspNoZMs" rel="noreferrer">https://www.youtube.com/watch?v=hmMlspNoZMs</a></p>

<p>As you can see, the lava cools in seconds. It doesn't erupt fast enough to sustain a constant liquid lava "line" under water.</p>

<p>This is not something that happens on Earth. But on other planets, maybe. If we think of a planet where the surface temperatures are on the hundreds of degrees Celsius (such as Venus), the cooling of the lava may be slow enough for plate tectonics (if they exist on said planet) to catch up and provide enough magma to sustain a long-lived magma lake-river on the boundary.</p>

CC BY-SA 3.0
2016-03-24T08:59:20.307Z
2016-03-24T08:59:20.307Z
Gimelist
<p>What happens at a divergent boundary is that indeed the two sides are diverging along the entire length. However, this does not mean that there needs to be a crack (and indeed there isn't). Rather, lava pushes into the area from below but most of the time doesn't actually make it to the surface before it cools. This process is called <a href="https://en.wikipedia.org/wiki/Dike_(geology)" rel="nofollow">dyke intrusion</a>, and the wikipedia page just linked to has some very good pictures. Because the spreading rate is pretty slow, it's also not necessary that dykes intrude the entire length of the boundary at the same time. Rather, they could introduce a part of the boundary this year, and some other part a couple of years later. If this just keeps happening, the intruding dykes will still push the two plates apart <em>on average</em> over many years.</p>

CC BY-SA 3.0
2016-03-25T03:35:27.877Z
2016-03-25T03:35:27.877Z
Wolfgang Bangerth
<p>Can we actually see an orange line of lava if we look down to the crack of the divergent boundary of tectonic plates?</p>

<geology><volcanology><plate-tectonics><petrology>
Can we see lava in a divergent tectonic boundary?
Gstestso
# Can we see lava in a divergent tectonic boundary?

(Asked by: username_0 on 2016-03-22)

Can we actually see an orange line of lava if we look down to the crack of the divergent boundary of tectonic plates?

**Tags:** geology, volcanology, plate-tectonics, petrology


---

## 2 answers

### Answer by username_1 on 2016-03-24. Score: 4

No, we can't. This is because of several reasons, mostly stemming from the fact that the plates are not diverging fast enough to keep the lava hot enough before it cools down.

If we go and look on diverging plate boundaries on land, such as on Iceland or East Africa, you don't have a "line" of lava. Instead, you have individual volcanoes located along a linear trend:

[![enter image description here](https://i.sstatic.net/MJph4.jpg)](https://i.sstatic.net/MJph4.jpg)

source: <http://volcano.oregonstate.edu/vwdocs/volc_images/africa/africa.html>

You see all the volcanoes along a line in the Ethiopia and Kenya region? It's not one "line of lava", but single volcanoes along a line.

If we think about divergent boundaries underwater, where the lava comes from a much shallower depth, we may think it might be possible to see this kind of feature. The problem is that water is extremely effective in cooling down lava. Here's an example video of what happens when there is lava underwater:

<https://www.youtube.com/watch?v=hmMlspNoZMs>

As you can see, the lava cools in seconds. It doesn't erupt fast enough to sustain a constant liquid lava "line" under water.

This is not something that happens on Earth. But on other planets, maybe. If we think of a planet where the surface temperatures are on the hundreds of degrees Celsius (such as Venus), the cooling of the lava may be slow enough for plate tectonics (if they exist on said planet) to catch up and provide enough magma to sustain a long-lived magma lake-river on the boundary.


---

### Answer by username_2 on 2016-03-25. Score: 2

What happens at a divergent boundary is that indeed the two sides are diverging along the entire length. However, this does not mean that there needs to be a crack (and indeed there isn't). Rather, lava pushes into the area from below but most of the time doesn't actually make it to the surface before it cools. This process is called [dyke intrusion](https://en.wikipedia.org/wiki/Dike_(geology)), and the wikipedia page just linked to has some very good pictures. Because the spreading rate is pretty slow, it's also not necessary that dykes intrude the entire length of the boundary at the same time. Rather, they could introduce a part of the boundary this year, and some other part a couple of years later. If this just keeps happening, the intruding dykes will still push the two plates apart *on average* over many years.


---

