Continental Drift [Updated, 2018] — Transcript
Full transcript
- 0:02[Music]
- 0:07[Laughter]
- 0:14take a look at this satellite image of
- 0:16Earth's surface if you look carefully at
- 0:19the continents you might notice
- 0:21something which many have noticed in the
- 0:23past and that is that the continents
- 0:25almost look like they fit together kind
- 0:28of like the pieces of some sort of giant
- 0:31massive puzzle of course you probably
- 0:34notice this the very first time you saw
- 0:37a map of the earth or a globe while a
- 0:39child in school the place on the earth
- 0:42where this is most obvious is along the
- 0:45eastern coast of South America and the
- 0:48western coast of Africa here it really
- 0:51appears like the continents fit together
- 0:55now of course people have known this for
- 0:57hundreds of years ever since the first
- 1:00accurate maps were created but most
- 1:03people just chalked it up to mere
- 1:05coincidence one person who had trouble
- 1:08with that though was German
- 1:10meteorologist Alfred Wegener you see
- 1:13Vagner couldn't just accept that this
- 1:16was a coincidence and that these land
- 1:18masses had such similar shaped
- 1:20coastlines and so he began to think
- 1:24about this and try and come up with some
- 1:26sort of explanation and what he
- 1:29concluded was something radical that the
- 1:32continents are moving an inventor's head
- 1:36if the continents are in fact moving and
- 1:39you run time backwards there must have
- 1:42been a time when all of those continents
- 1:44work together in some sort of
- 1:46supercontinent something he named
- 1:49Pangaea coming from the greek term for
- 1:53all earth this became known as vague
- 1:58neurs theory of continental drift
- 2:02now vague nur being a man of science
- 2:04knew that if his theory was going to
- 2:06gain any traction he needed to provide
- 2:09evidence and so he set to his life's
- 2:12work of researching every corner of the
- 2:15planet to better understand this strange
- 2:18observation and to explain it to the
- 2:21scientific community
- 2:23by the end of his life he had collected
- 2:26four main pieces of evidence and we're
- 2:30going to look at those today we'll begin
- 2:34where we've already begun and that is
- 2:37with this shape of the continents if we
- 2:40look carefully all over the earth
- 2:42coastlines appear to fit together like
- 2:44this part of South America and this part
- 2:48of Africa and so that becomes evidence
- 2:51number one the apparent fit of the
- 2:54continents that the coastlines appear to
- 2:57fit together like the pieces of some
- 2:59sort of giant puzzle but of course this
- 3:02was just a starting point and so Vagner
- 3:05continued his research the next thing he
- 3:08dove into involved life fagner began to
- 3:13study fossils of ancient creatures and
- 3:15more importantly where those fossils
- 3:18were located take for instance this
- 3:21creature an ancient freshwater reptile
- 3:24called a mezzo Saurus interestingly if
- 3:28you look on all of the continents and
- 3:31land masses of Earth fossils of the meso
- 3:34source are only found in two places
- 3:37these include the very southern tip of
- 3:41South America and the southern tip of
- 3:44Africa now let's think about this how
- 3:47could this be possible
- 3:49we know the meso source could not have
- 3:52evolved in one location and then
- 3:54traveled to the other it was a
- 3:57freshwater reptile and therefore could
- 3:59never make the journey through the salty
- 4:01atlantic ocean and so that idea is out
- 4:04the window another idea is that perhaps
- 4:08the same exact creature evolved in the
- 4:11same exact way at the same exact time in
- 4:13two locations that are separated by
- 4:17thousands of miles but too vague no that
- 4:21was unlikely if not impossible and so
- 4:24what he concluded was that during the
- 4:27days when the Meza source thrived Africa
- 4:31and South America were not separated by
- 4:33an ocean but rather they were connected
- 4:35as one land
- 4:37where the Mesozoic and roam free and
- 4:39then at some point later on those land
- 4:42masses with the remains of the Mesozoic
- 4:45were ripped apart and separated by the
- 4:48ocean as we see today
- 4:51now this seemed like a radical idea to
- 4:53Vagner until he began to look at other
- 4:56species of living organisms from the
- 4:59time and what he found was much the same
- 5:02there were all sorts of creatures beyond
- 5:05the meso source like the sign onethis
- 5:08and glassy Terrace and Lystra Soros who
- 5:10all showed very similar unique fossil
- 5:14distributions as seen here and strangely
- 5:19enough if you reassemble the continents
- 5:21according to their shapes the
- 5:24distribution of the fossils makes
- 5:26perfect sense and so this becomes piece
- 5:28of evidence number two fossil
- 5:31correlation or the matching up of
- 5:34similar fossils found in distant
- 5:36locations at this point vague nor is
- 5:39excited because his theory is coming
- 5:42together and his ideas seem to have a
- 5:44lot of support and so he's set off to
- 5:47find even more evidence and he did so by
- 5:50studying geology or rock structures very
- 5:55similar to what he saw with fossil
- 5:58distribution he saw with rock
- 6:00distribution in fact if you look at the
- 6:02mountains of the modern day northeastern
- 6:05United States they are the exact type
- 6:08and age of rock found in the mountains
- 6:11of the UK and northern Scandinavia and
- 6:15so Vagner said to himself could it be
- 6:18that the same exact rocks formed at the
- 6:20same exact time but in very different
- 6:23locations well it is possible but it
- 6:26seems unlikely
- 6:27and so what Vagner concluded was that
- 6:29those rocks formed at the same time in
- 6:32the same location and then that area was
- 6:35torn apart by the motion of the
- 6:37continents carrying those rocks
- 6:40to the distant locations they are in
- 6:42today and so this becomes evidence
- 6:45number three Rock and mountain
- 6:48correlation or the matching
- 6:50of similar rocks from distant locations
- 6:53proving that they were once together and
- 6:56finally his fourth piece of evidence is
- 6:59probably the most compelling of all and
- 7:01this involves a look at the past climate
- 7:04of the earth so vague nurse studied
- 7:07things like glaciers and what he knew
- 7:11was that when glaciers move over the
- 7:14surface of the earth they leave behind
- 7:16evidence in the form of these glacial
- 7:19striations or deep scratches in the rock
- 7:21that show the direction the ice moved as
- 7:24it dragged over the surface now
- 7:27interestingly if you look at where on
- 7:30earth we find glacial striations today
- 7:32they're located in areas like the Amazon
- 7:35rainforest on the equatorial South
- 7:39American continent and the hot sticky
- 7:42jungles of Central Africa now of course
- 7:45these are places where you could not
- 7:47find glaciers today simply because
- 7:50they're too close to the equator and
- 7:52getting sunlight that is too intense and
- 7:55hot preventing glaciers from forming and
- 7:58so what Vagner concluded was that these
- 8:00areas were not always near the equator
- 8:03but rather in the past they were located
- 8:06closer to the poles where a colder
- 8:09climate could exist and support glaciers
- 8:13similarly Wagner looked at rocks like
- 8:17bituminous coal which is a sedimentary
- 8:20rock that can be found on the new york
- 8:22state earth science reference tables you
- 8:25can find this table at this link
- 8:30bituminous coal is a sedimentary rock
- 8:34that is made from compacted and cemented
- 8:36plant remains but not just any plant
- 8:39remains tropical plant remains from hot
- 8:42sticky humid jungles interestingly if
- 8:47you look at the major coal deposits on
- 8:49earth today they don't fall in hot humid
- 8:52areas but rather they fall in frigid
- 8:55areas like northern Asia and Antarctica
- 8:59so Vagner knew that if this was the
- 9:02observation he was
- 9:04making this tropical cold being found in
- 9:07frigid places that those places must not
- 9:10always have been frigid and maybe in
- 9:13fact they were once located closer to
- 9:16the equator and so this becomes piece of
- 9:19evidence number four Paleo climate data
- 9:22or past climate data like finding
- 9:25evidence of coal in currently cold areas
- 9:29and evidence of glaciers and currently
- 9:31warm areas and so these four pieces of
- 9:35evidence put together became the theory
- 9:37of continental drift as published by
- 9:39Vecna in his book the origin of
- 9:42continents and oceans unfortunately
- 9:48there was one thing that Vagner could
- 9:50never wrap his mind around and that was
- 9:52what force could be driving the motion
- 9:55of the continents he couldn't understand
- 9:58how it would be possible for huge land
- 10:01masses to actually move considering the
- 10:04amount of force and energy required to
- 10:07do so and without this explanation his
- 10:10theory of continental drift remains
- 10:13largely rejected in the scientific
- 10:16community
- 10:18in November of 1930 while on a research
- 10:23expedition on the ice sheets of
- 10:24Greenland Vagner froze to death his body
- 10:29was found in the ice months later you
- 10:34can still visit a cross that marks the
- 10:38site of his death frozen on the ice
- 10:41sheets of Greenland the story of Alfred
- 10:47Wegener is a tragic one it's the story
- 10:49of a great scientific mind who was ahead
- 10:52of his time but died before he reached
- 10:55his true potential modern geologists owe
- 10:59to him their understanding of how the
- 11:02earth actually works
- 11:10you
- 11:11[Music]
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