I Won't Be Missed
Rare Elements Lyrics


We have lyrics for these tracks by Rare Elements:


All Those Things We Ever Dreamt This is the way it's going down All we know is…
At This Time of Year At this time of year The wind can blow cold At this…
Bad Medicine Days go by in haze In the summer heat And the winter…
Choices You sit alone at the corner table And wonder how this…
Dusty Deities Whatever comes to living It's not about giving up Whatever w…
Good Almost Waters fall from the sky But the sky does not fall In…
Great Unknown We are going into The great unknown You can't see the destin…
Radio Silence Today Is the day It's goin' to Take place Until that it's r…
Something Special I don't know How long I've been Sitting here waiting Specia…



Storm in the Making There is a storm in the making That we will all…
Uphill I put on my tattered boots To get some fresh air Didn't…
Where the Beast Sleeps You know Where the beast sleeps But you don't know When it …


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Most interesting comment from YouTube:

Tom P

Hi Atlas Pro!

This is a really well put together video, I loved the pacing, the production and the narrative tone. The research on the abundance of elements in the crust was spot on as far as I could tell, and I thought it was a nice way to introduce the concept of radioactive decay in Earth materials. I'm actually making this post because there were a few glaring errors early on however, which I just couldn't get past as a geologist! Specifically:

"Anything below the crust is completely inaccessible to us, both in terms of mining and research"

Not in terms of research. We use indirect geophysical methods to 'access' and image the mantle/core, but we also have actual rock samples from the mantle in the form of xenoliths - chunks of rock which have survived a journey from the mantle into a crustal magma chamber and eventually spat out by a volcano for us to examine.

The Kola Superdeep borehole was not stopped due to "heat from the mantle", but due to the heat from the higher than expected geothermal gradient of the crust that was being drilled into. Although heat from the mantle would have contributed to total overall heat, geothermal gradients in continental crust are much higher than in the mantle and quite variable - it wasn't foreseen how high the gradient would be at the Kola Superdeep Borehole site.

"Earths's crust can reach up to 40,000 metres deep". In fact, Earth's crust can be even thicker than this at sites of plate convergence and mountain building. Here we can get a crustal thickness of up to 80,000 metres, which is seen in parts of the Himalaya today.

"We don't actually have any precise measurements of what's beyond the crust". In truth, we have loads of physical measurements from seismology and magnetic detection, we also have loads of geochemical measurements from mantle xenoliths.

"The molten lava that comes from the mantle mostly consists of material from the crust which just melted from contact with the mantle." This is the biggest error in the video. Crustal material which gets assimilated into magma chambers does play an important role in the chemical evolution of many magmas, but the vast majority of magmas on Earth represent partial melting of the mantle. All magmas produced everywhere originate from this partial melting of mantle material (with a literal handful of extremely rare cases from the Himalaya where melting can originate in the crust). This is why lavas can be so useful as a window into mantle processes - that's where they come from. Magma chambers are filled with material melted from the mantle, and provided it doesn't sit around too long in there, it may not ever receive any crustal component. The ocean floors are made from basalt which was melted from the mantle alone, mid-ocean ridges are home to magma chambers which are constantly erupting and being replenished.

"Therefore in reality, lava offers little insight into what's beyond the crust". An entire field of geoscience has been long established which deals with classifying lavas, their origin and what they can tell us about the Earth's interior, in particular the mantle. This is known as igneous petrology.



All comments from YouTube:

Evank

Conspiracy theory: Astatine was created by the government in between Polonium (Po) and Radon (Rn) to keep the periodic table from saying Po Rn

~Rin's Empire~

AHHAHAH

cjack56

Thanks
Pp

brazil87ful

Need to pay more attention..

linkbirds

Real Real Real

Andrew Todaro

😂

91 More Replies...

Grebulocities

When I saw helium and neon, I went and got my pressurized ampule of xenon (encased in acrylic) out of the fridge. It's easily the rarest stable element in the Earth's crust. I got it for an amazing property: it turns from a liquid to a state of matter we don't usually get to see - a supercritical fluid - between fridge and room temp. Its critical point falls at 16.6 C or 61.9 F, at a pressure of about 58 atmospheres. As I tilt it back and forth, the interface between the vapor and liquid eventually becomes blurry and then vanishes altogether. Also, it's beautiful in an electric field. It set me back $103 but it's worth every penny.

...but then you bypassed it and went on to trace radioactive elements. That's fine, no hard feelings. Astatine is cool but I had worse luck ordering it. Amazon got it to me in 2 days but only 1/64 of what I ordered was there. So I sent it back but they claimed they only got 1/4096 of what they sent me. Goddamn Jeff Bezos!

VexGotBloxxed

@Human I care a lot

Spacewarp Photography

Astatine is one of my two favorite elements, along with Fluorine. Astatine desperately wants to not exist, and Fluorine desperately wants everything else to not exist! Who knows what would happen if they ever met!

Mihail Milev

@kingdom of Bird nice pfp

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