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WatsisnameDate: Sunday, 30.10.2016, 21:38 | Message # 1051
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I found the edge of the world.



What's beyond that? Nobody knows.

Slowly I drift, into the void.



Swallowed by the endless mist.





 
powermoneywomenDate: Saturday, 05.11.2016, 14:52 | Message # 1052
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http://www.powermoneywomen.com/sitephotos.html

See the second photo of the link i provided.....it was so weird that i had to share.....mars....is that another crab?
 
WatsisnameDate: Sunday, 06.11.2016, 05:19 | Message # 1053
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Exploring the beauty and complete counter-intuitiveness of diffraction. smile All shots taken using a green (532nm) laser passing through various apertures.

A tiny hole just barely punched through a note card with a push-pin:



Through less symmetrical holes. Still makes a symmetrical pattern!





What happens when the laser is passed through three small holes in a tight triangle formation? Something crazy:



And finally, a 'single slit' experiment, with the slit becoming narrower.



The laser is being passed through the gap in a toenail clipper. In the first frame, the gap is about the width of a human hair (~0.1mm). In the last (visible) frame, the gap is down to about 5 micrometers (about the length of a typical bacterium). And how's this for counter-intuitive? The gap is horizontal! surprised





 
AlekDate: Sunday, 06.11.2016, 08:08 | Message # 1054
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Quote Watsisname ()
And how's this for counter-intuitive? The gap is horizontal!


Wait what? That is really weird...it shouldn't be possible for the light to re-arrange itself like that...





Living among the stars, I find my way. I grow in strength through knowledge of the space I occupy, until I become the ruler of my own interstellar empire of sorts. Though The world was made for the day, I was made for the night, and thus, the universe itself is within my destiny.
 
WatsisnameDate: Sunday, 06.11.2016, 13:00 | Message # 1055
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It is probably the least intuitive thing I know in all of physics. smile It's like that because we're so used to light behaving like rays, going in straight lines, not canceling out with itself...

But here we are seeing the wave-like properties of light. Water waves actually provide a very good visual analogue for it:



Notice that with water waves as with light, the waves spread out more when the aperture is similar in size to the wavelength. It's useful to think of each point on the wave front as a source for a new spherical wave. Then the question is how do those new waves interfere with each other as they travel? Peaks meeting with with peaks make brightness. Peaks with troughs make darkness. Once we work through the geometry of it, it begins to make a bit more sense how the diffraction pattern forms. And yet, even with that understanding, to actually see it still strikes me as totally odd. Water waves are one thing, but it's hard to imagine light being like that.

We can also find the diffraction pattern produced by an aperture by taking the Fourier Transform of the aperture. The Fourier Transform is well known in signal analysis, but it also applies in 2D and even higher dimensions, and it has use in optics. Here's the transform of three rough-edged circles in a triangle pattern:



Pretty close to the diffraction pattern photographed.

And the transform for a horizontal slit:



Crudely drawn smiley face? smile






 
WatsisnameDate: Friday, 11.11.2016, 12:44 | Message # 1056
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Snow geese from Siberia. happy












 
spacerDate: Friday, 11.11.2016, 12:49 | Message # 1057
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Watsisname, beautiful images. i like the mountains in the back too!




"we began as wanderers, and we are wanderers still"
-carl sagan

-space engine photographer
 
LookAtDatDakkaDate: Sunday, 13.11.2016, 00:13 | Message # 1058
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Here what I would imagine Space Engine in the future:



Rendered in Blender 2.78 with noise addition

In other words, Watsisname, nice flocks of birds.





NVIDIA 960 GTX 2048MB

Edited by LookAtDatDakka - Sunday, 13.11.2016, 03:57
 
HornblowerDate: Sunday, 13.11.2016, 00:40 | Message # 1059
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LookAtDatDakka, That's what it looks like now! (actually looks better than it does in your picture, but nice render)

Edited by Hornblower - Sunday, 13.11.2016, 00:49
 
AlekDate: Sunday, 13.11.2016, 03:29 | Message # 1060
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Quote LookAtDatDakka ()
Rendered in Blender 2.78


Hm...could've mistaken it for a Grand Designer image with some after editing





Living among the stars, I find my way. I grow in strength through knowledge of the space I occupy, until I become the ruler of my own interstellar empire of sorts. Though The world was made for the day, I was made for the night, and thus, the universe itself is within my destiny.
 
midtskogenDate: Sunday, 13.11.2016, 14:41 | Message # 1061
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Today's NZ earthquake as recorded by my seismometer in Oslo 160 degrees (nearly 18000 km) away:

Attachments: 5210098.png (13.8 Kb)





NIL DIFFICILE VOLENTI
 
WatsisnameDate: Sunday, 13.11.2016, 23:10 | Message # 1062
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Wow. surprised

For being 160° away from epicenter, I was curious what information about the Earth's inner structure are apparent in the recording. Here's an interesting graphic which lays it all out.

Your recording looks very consistent with it, showing a ~20 minute delay between the quake and the wave arrival. The first to arrive are pressure waves that passed through both the outer and inner core. Then there are waves that were refracted through the outer core, and then the pressure wave which was reflected once off the surface. I think that may be the spike you see at around 11:28. The rest are surface waves and further reflections. And there are no direct shear waves, since they can't pass through the liquid outer core.





 
midtskogenDate: Sunday, 13.11.2016, 23:47 | Message # 1063
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Yes, the striking feature of this plot is the lack of an S wave arrival. It would be interesting to convert this data to audio. Usually one hears two crashes followed by a rumble: P wave arrival, S wave arrival and surface waves. But this should be different. I'm in Korea right now, and accessing my usual tools for doing these kind of things is a bit trickier.




NIL DIFFICILE VOLENTI


Edited by midtskogen - Monday, 14.11.2016, 00:21
 
midtskogenDate: Monday, 14.11.2016, 00:05 | Message # 1064
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An attempt to convert to audio. One hour compressed to 5 seconds. The sound appears very soft to me, and no doubt the distance causes that. But I can barely hear the sound, which may be because my $200 laptop has lousy speakers.

Edit: My phone's speaker is better. There are two crashing sounds right in the beginning. The second could be an echo of some kind, since there will be no S wave (and the delay between them is two small for an S wave anyway). It's not one of the aftershocks either, as the first one large enough for clear detection occurred half an hour later. I can't really hear the surface waves, but the frequencies might be too low for my speakers, even when one hour is compressed to 5 seconds. My seismometer peak sensitivity is around 0.06 Hz, which gets turned to audio around 43 Hz and that is way too low for most speakers.

Attachments: 4265737.wav (422.0 Kb)





NIL DIFFICILE VOLENTI


Edited by midtskogen - Monday, 14.11.2016, 00:21
 
WatsisnameDate: Monday, 14.11.2016, 04:48 | Message # 1065
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That second crash seems to be the spike I was mentioning at about 11:28, which based on the graphic is probably the part of the P wave which moved through the mantle and reflected once off the surface before reaching you. At first I thought it surprising that it arrives so soon after the direct wave despite following a longer path, but after going through the math it does make sense.

If we consider a point antipodal to the quake, then the straight line through the Earth is about 12740km. 100km through the crust (both sides), 3900km through mantle, 6200 through the outer core, and 2540 through the inner core. The P-wave velocity changes through all of these, averaging about 7km/s through crust, 10.5km/s through mantle, 9km/s through outer core, and 11km/s through inner core. Then the time it takes to pass through the whole Earth is about 22 minutes.

For the singly-reflected P wave through the mantle, we can imagine (not quite accurately but close enough) that it goes on a straight line to a point 90° away and reflects from there to the antipodal point. This path length is sqrt(2) times the radius of the Earth, times 2, or about 18000km. Then assuming 10.5km/s average speed, it takes about 28 minutes to make that trip. This roughly agrees with the observed waves.

The first surface waves should have arrived somewhere around 40 minutes after the quake. There does seem to be an increase in intensity there, but a lot of other complicated reflections are also reaching you by that point as well.





 
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