WEBVTT - What Does It Take to Freeze a Waterfall?

0:00:01.920 --> 0:00:06.440
<v Speaker 1>Welcome to brain Stuff, a production of iHeart Radio, Hey

0:00:06.519 --> 0:00:11.200
<v Speaker 1>brain Stuff, Lauren Bogobam. Here. Should Hell ever freeze over,

0:00:11.440 --> 0:00:15.960
<v Speaker 1>it'll probably happen right after Niagara Falls does. The Roaring

0:00:16.079 --> 0:00:19.720
<v Speaker 1>Landmarks sits on the border of Upstate New York and Ontario, Canada.

0:00:20.160 --> 0:00:23.480
<v Speaker 1>It consists of three separate waterfalls, with the tallest being

0:00:23.520 --> 0:00:27.320
<v Speaker 1>a hundred and sixty seven feet that's fifty one high.

0:00:27.640 --> 0:00:31.080
<v Speaker 1>These cascading waters have attracted the odd There devil over

0:00:31.120 --> 0:00:33.760
<v Speaker 1>the years. We've all heard the stories about thrill seekers

0:00:33.760 --> 0:00:37.280
<v Speaker 1>and barrels, but most visitors simply come to admire the

0:00:37.320 --> 0:00:41.280
<v Speaker 1>falls natural beauty. In the wintertime, the falls get extra

0:00:41.320 --> 0:00:47.080
<v Speaker 1>gorgeous because I see formations often appear on or around them. Yet,

0:00:47.320 --> 0:00:51.960
<v Speaker 1>despite claims to the contrary, Niagara Falls doesn't ever fully freeze.

0:00:52.479 --> 0:00:56.120
<v Speaker 1>And it turns out that freezing Niagara Falls solid would

0:00:56.120 --> 0:00:59.960
<v Speaker 1>be quite a feat. During the winter, a whopping twenty

0:01:00.120 --> 0:01:03.880
<v Speaker 1>two million gallons or five million liters of water tumble

0:01:03.920 --> 0:01:07.280
<v Speaker 1>over the falls per minute, and scientists say it would

0:01:07.280 --> 0:01:10.720
<v Speaker 1>be extremely difficult to freeze that much fast flowing water.

0:01:11.000 --> 0:01:15.720
<v Speaker 1>Even in sub zero temperatures, the falls can appear frozen

0:01:15.920 --> 0:01:18.880
<v Speaker 1>when the thick mist that they produced freezes as it

0:01:18.880 --> 0:01:23.959
<v Speaker 1>accumulates on the trees, boulders, and railings that surround the falls. Also,

0:01:24.120 --> 0:01:27.000
<v Speaker 1>there are days when a thin layer of frozen spray

0:01:27.040 --> 0:01:31.319
<v Speaker 1>and miss hardens over the falls themselves, right beneath this

0:01:31.520 --> 0:01:34.759
<v Speaker 1>icy blanket, though you'll still find plenty of liquid water

0:01:34.880 --> 0:01:39.720
<v Speaker 1>flowing on its usual downward path. A bottom line, Niagara

0:01:39.720 --> 0:01:42.920
<v Speaker 1>Falls isn't going to freeze all the way through anytime soon.

0:01:43.600 --> 0:01:47.840
<v Speaker 1>But that's just one landmark. Let's talk about some other waterfalls.

0:01:49.360 --> 0:01:54.160
<v Speaker 1>On a cold morning in January, physics professor Michael J.

0:01:54.320 --> 0:01:58.720
<v Speaker 1>Ruise and independent researcher Charles Cranford filmed a sixty five

0:01:58.720 --> 0:02:02.760
<v Speaker 1>foot that's twenty waterfall in North Carolina that had mostly

0:02:02.880 --> 0:02:06.440
<v Speaker 1>frozen Trickling over. Some of the ice was a stream

0:02:06.600 --> 0:02:10.799
<v Speaker 1>of super cooled water. Super Cooled water is water that's

0:02:10.840 --> 0:02:14.840
<v Speaker 1>managed to remain liquid below its normal freezing temperature, that

0:02:14.960 --> 0:02:19.000
<v Speaker 1>being thirty two degrees fahrenheit or zero degrees celsius. It

0:02:19.080 --> 0:02:23.320
<v Speaker 1>was significantly colder outside when Louise and Cranford recorded their video.

0:02:23.680 --> 0:02:26.840
<v Speaker 1>The local temperature was just five degrees fahrenheit or negative

0:02:26.880 --> 0:02:30.960
<v Speaker 1>fifteen celsius. Under those conditions, even the super cooled water

0:02:31.080 --> 0:02:35.440
<v Speaker 1>couldn't stay liquefied for long. The duo captured the Carolina

0:02:35.440 --> 0:02:39.600
<v Speaker 1>waterfall freezing into ice in real time, and not just

0:02:39.760 --> 0:02:43.640
<v Speaker 1>any ice. The water was hardening into a clumping collection

0:02:43.760 --> 0:02:49.360
<v Speaker 1>of tiny needle shaped crystals. Meteorologists call that frazzle ice,

0:02:50.520 --> 0:02:54.639
<v Speaker 1>often associated with turbulent and super cooled water. Frazzle ice

0:02:54.680 --> 0:02:58.560
<v Speaker 1>can also develop when mist droplets freeze. This ice is

0:02:58.600 --> 0:03:01.720
<v Speaker 1>a common site around and waterfalls, like the ones at

0:03:01.720 --> 0:03:06.000
<v Speaker 1>California's you Semity National Park during below freezing weather, When

0:03:06.080 --> 0:03:08.880
<v Speaker 1>frazzle ice clings to a rocky surface, it can become

0:03:08.960 --> 0:03:13.480
<v Speaker 1>a platform for even more ice to build upon. Waterfall

0:03:13.720 --> 0:03:17.720
<v Speaker 1>icicles can also build up or down, found in many

0:03:17.840 --> 0:03:20.359
<v Speaker 1>regions of the globe, from France to Utah, they can

0:03:20.400 --> 0:03:24.560
<v Speaker 1>take many forms. You can find ice stalactites dangling off

0:03:24.560 --> 0:03:28.239
<v Speaker 1>of cliffs or ice stalagmites ascending from the ground below,

0:03:28.960 --> 0:03:32.640
<v Speaker 1>and if a lowering stalactite touches a rising stalagmite, you

0:03:32.720 --> 0:03:36.360
<v Speaker 1>get a column like ice pillar. A note that these

0:03:36.480 --> 0:03:40.680
<v Speaker 1>icicles and columns can be dangerous as they can suddenly collapse.

0:03:41.920 --> 0:03:44.920
<v Speaker 1>But if you do see I see stalactites, stalacmites, or

0:03:45.000 --> 0:03:48.560
<v Speaker 1>pillars gathered around your favorite waterfall. It doesn't mean the

0:03:48.560 --> 0:03:52.200
<v Speaker 1>whole waterfall has frozen solid. That only happens when the

0:03:52.240 --> 0:03:55.560
<v Speaker 1>source of the waterfall freezes through. Whether that's a creek,

0:03:55.680 --> 0:03:59.200
<v Speaker 1>a stream, or a river, the larger and faster flowing

0:03:59.280 --> 0:04:03.000
<v Speaker 1>a given source is, the smaller its chances of becoming frozen.

0:04:08.280 --> 0:04:10.840
<v Speaker 1>Today's episode was written by Mark Mancini and produced by

0:04:10.840 --> 0:04:13.160
<v Speaker 1>Tyler Clang. For more on this and lots of other

0:04:13.200 --> 0:04:16.360
<v Speaker 1>fast flowing topics, visit how stuff works dot com. Brain

0:04:16.360 --> 0:04:19.039
<v Speaker 1>Stuff is production of I heart Radio. For more podcasts

0:04:19.080 --> 0:04:22.040
<v Speaker 1>my heart Radio, visit the i heart Radio app, Apple Podcasts,

0:04:22.120 --> 0:04:23.880
<v Speaker 1>or wherever you listen to your favorite shows.