Neil DeGrasse Tyson Answers Angry Tweets on Pluto's Demotion

Many moons ago, Pluto – the outermost planet in our solar system – was demoted. For those of us who grew up with the nine-planet solar system model, this came as somewhat of an affront to everything we knew about anything, ever. I mean, what is the meaning of life if the planetary status of Pluto can so easily be revised and revoked? Why, Neil, why??

In this hilarious video, Neil DeGrasse Tyson answers to the angry rants and raves (and insults) of those really strange people who were truly and deeply wounded by Pluto’s demotion from planetary status to mere space-wandering rock. Why people give such a damn is beyond me. After all, Pluto is only a quarter the size of our moon and even then, most of its mass is ice.

Video Source: Uploaded by National Geographic on YouTube channel

Neil DeGrasse Tyson is a megamind and, not coincidentally, also curator of the Hayden Planetarium, as well as the presenter of Carl Sagan’s revised TV-series, “Cosmos” He is awesome and anyone who has watched any of his videos, lectures or presentations will appreciate just how erudite and smart this man is.

But by far one of Neil’s greatest talents is the perfect balance between a sophisticated understanding of science and the ability to communicate with those who don’t. This makes him one of today’s most powerful and persuasive public figures in science and technology.


If The Planets Took The Place of Our Moon…

Ever wonder what the view of Mars would be if it were as close to us as our moon? Would it glow a belligerent red in our night sky and confuse moths the world over? How about Neptune: would it cast a seductive blue glow over the body of your lover as she lies recovering from a delicious round of rodgering? Now imagine Jupiter, our solar system’s largest planet with moons that are twice/thrice the size of ours… what would they all look like if they had to take the place of our moon, without cataclysmically affecting life on our planet? This video answers that question…

Video Source: Uploaded by yeti dynamics to YouTube channel



Fire and Brimstone – the Story of Volcanoes

eruzione Etna volcano
Mount Etna eruption, Nicolosi Catania, Italy

There’s something beautiful about a woman’s rage (not counting the tarts from Geordie Shore) and in no better way is this sentiment illustrated than by Mother Nature’s ire. As terrifying as it is to be at ground zero, from a safe distance, natural disasters are incredibly awe-inspiring and angry volcanoes deserve a top spot for making people go “ooooh” and “aaaaah” and “oh shit…”

Volcanoes are literal pathways from the Earth’s fiery guts to its crusty exterior. But the channels available for the molten rock and gas that spew forth are far too narrow to satisfy the sheer volume of indigestion within and the result is an immense build-up of pressure. The release of this pressure includes, but is not limited to, violent sprays of lava, devastating pyroclastic flows, stratospheric columns of volcanic ash, electrical storms, scalding gas and dust and Hiroshima-type explosions that not only dislocate millions of tonnes of solid rock, but have been reported to be audible many thousands of kilometres away from the point of origin.

Vesuivio_Eruzione eruption volcano
Source: “Vesuivio Eruzione April 26th, 1872” by Giorgio Sommer – Own work. Licensed under Public Domain via Wikimedia Commons

Volcanoes have the potential to send species to extinction, yet at the very same time, they nourish the biosphere in an appreciable radius around them (volcanic ash is highly fertile). Volcanoes are magnificent and a wonderful example of how the surface of our planet is in a constant state of dynamism.

Where Not To Go On Summer Vacation

Planet tectonics plate diagram

Volcanoes typically form at the convergent and divergent boundaries between the enormous shifting tectonic plates that comprise the Earth’s crust (see gorgeous image above). It is here that the seams of the Earth permit plumes of its molten interior to travel towards the surface. But as it was mentioned, the surface-bound transport of this material is anything but a six-lane highway. It’s more like a gravelly, pothole-ridden country road. The gas and molten rock that are trying to get from A to B encounter rigid rock and the cracks they exploit along their journey are incredibly narrow. A build-up of pressure results in a potentially explosive situation, so that when something finally gives, the results are disastrous for the local biology: human habitation included.

Volcanoes also form over features called “hot spots”, which don’t necessarily occur near plate tectonic boundaries (see diagram below). The Hawaiian Islands – all of them formed by volcanic activity in the middle of the Pacific Plate – are a prime example of this.


There are several scientific theories that seek to explain what hot spots are and a popular one is that they are upwelling intrusions of molten material (mantle plumes) that originate at the boundary between the Earth’s core and mantle. The exact depth of this varies, but the Hawaiian hot spot is estimated to be 3,000 km deep. That’s 9,842,520 ft. for those of you in ‘Merica.

Volcano Classification

There’s more to volcanology than your stock standard angry Earth pimple. Volcanoes come in many shapes, sizes and compositions. What happens at the surface – what we see and experience when volcanoes awake from their slumber – is dependent on a suite of factors and an especially important one is the composition of the magma that is trying to escape the lithified constraints of the crust.

Lava Composition

Lava flow in Hawaii

Rock that is rich in silicates tends to form chunky, viscous slow-moving magma. This subset of liquid rock is in no hurry to go anywhere and tends to contribute to terrible congestion. It also has the particularly nasty habit of trapping gas, which is why things can get explosive. Since Hawaii is no stranger to seismic activity, its inhabitants have coined a word for this particular magma and it’s pāhoehoe.

At the other end of the spectrum, you get magma that doesn’t contain a lot of silicates, but is rather rich in ferrous (iron) compounds. This magma – ʻAʻa, pronounced “ah ah” – get’s extremely hot and tends to flow hard and fast. If you’ll excuse the crass analogy, the difference between pāhoehoe and ʻAʻa is much like the difference between constipation and Delhi belly.

Both, however, are extremely uncomfortable.

Magma isn’t, of course, one or the other. There is a vast spectrum of mineral compositions between, but by understanding the difference between one extreme and the other, we can begin to understand how different kinds of volcanoes are formed.

Cone, Shield and Stratovolcanoes

If there’s one thing to be said for geologists, it’s that they don’t mess around with terminology. The name bestowed upon a volcano is as transparent as a wet T-shirt.

Cone (Cinder) Volcanoes

Bromo volcano in Indonesia
Mount Gunung Bromo (Indonesian island of Java): A classic cinder or cone volcano

Cone volcanoes, also known as cinder cones, generally consist of a hill that can be anywhere from 30 meters (98 ft.) to 400 (1,312 ft.) meters in height. Formed from the eruption of materials that are riddled with gas, crystals and a hodgepodge of fragmented rock. To see an example of this kind of volcano, put on your sombrero, crack open the tequila and get on a plane to New Mexico. There, you will find a spectacular volcanic field called Caja Del Rio, which comprises more than 60 cone volcanoes. If the prospect of New Mexico doesn’t appeal, you can always bum a lift on the next scientific mission to Mars or the moon, both of which are believed to feature this type of volcano.

Shield Volcanoes

Kohala-Landsat Hawaii shield volcano
Kohala Mountain, the oldest of Hawaii’s five volcanoes. The entire island is a massive shield volcano. Source: By USGS (source usage) via Wikimedia Commons

Shield volcanoes have a much broader profile than cone volcanoes and, as the name suggests, are shaped like shields. Bet you didn’t see that one coming. These beasts are formed from the eruption of very runny lava that tends to escape the Earth’s crust before causing too much mayhem as a result of a build-up of pressure. Shield volcanoes are, by comparison, the placid elderly aunt of volcanoes and are most commonly found at oceanic tectonic boundaries. Oceanic plates aren’t usually rich in silicates, which explains why the magma produced here is more felsic in composition, hence its lower viscosity. Skjaldbreiður in Iceland (say that three times fast) is an example of a shield volcano. The Hawaiian Islands, which have formed almost smack bang in the middle of the Pacific Plate over a “hot spot,” are also shield volcanoes.

In June of 2013, the Mayon stratovolcano in Albay, Philippines, reached Level 1 alert level due to what the Philippine Institute of Volcanology and Seismology refers to as “abnormal behavior”.


Stratovolcanoes, or composite volcanoes, are the tri-polar member of the volcanic family. They look like your typical volcano but actually consist of alternating layers of different kinds of erupted material as the above diagram depicts. Stratovolcanoes produce a range of eruptions depending upon their mood and these include chunky cinders, choking ash and molten rock (lava). One of the best known (and least loved) of these volcanoes is Mount Vesuvius, which is located in Stromboli, Italy. This one was responsible for the notorious levelling of the cities of Pompeii and Herculaneum in AD 79, killing 16,000 people. It is estimated that Mount Vesuvius released 100,000 times the energy liberated by the Hiroshima bomb.

Volcanic Hazards

Mount Pinatubo Explodes
Run? Source: “Point of View Photos” Huffington Post

When volcanoes become active, a number of things can happen, none of them good if you’re fond of life. One of the most devastating of these consequences is ash. You wouldn’t think so… ash is soft and white. How on Earth could it possibly inconvenience you the way a searing hot lake of lava might? Stratovolcanoes are especially fond of explosive eruptions, which send voluminous clouds of ash into the atmosphere and cascading down their slopes.

This ash, however, isn’t the kind you find in your barbeque pit after a night of camping, beer and sing-a-longs. It’s mixed with gas that is hot enough to disassociate your atoms. These eruptions send roiling clouds of gas, dust, ash and other debris down the mountain, which devastate anything organic in their path, leaving behind a scene that looks like a bomb went off in a cocaine factory.

Extinct, Dormant and Active Volcanoes: The Good, the Bad and the Ugly

Stromboli volcanic eruption3

Volcanoes are dangerous creatures. So an apt analogy for the popular classifications of these geological features would be your mother. When she has a gin and tonic in her hand (dormant), you may want to make plans for the evening. When she’s 10 G&T’s down (active), it’s time to execute those plans and get the hell out of the house. When she’s passed out on the couch (extinct), it’s safe to come home, although my recommendation to you would be to move out your childhood home and get yourself an education.

Extinct volcanoes, such as the Netherland’s Zuidwal and Shiprock volcanoes, are no longer considered to be active at all because they don’t have a supply of magma. They also have no documented history of indigestion. Dormant volcanoes, on the other hand, are known to have erupted at some stage in recent history. They may be quiet, but that doesn’t mean they can’t suddenly awaken. Mount Vesuvius (Gulf of Naples) was a purring kitten before it went psycho in AD 79, as was Mount Pinatubo (Philippines) prior to its epic tantrum in 1991. The latter is now considered an active volcano, which is one that has exhibited recent activity and is therefore a potential hazard to all within its vicinity.



If you’ve ever had a fight with Mexican food and lost (who hasn’t?) then integrating “Krakatoa” into your vocabulary is a wonderful idea if you need help explaining exactly what just happened to you to the flat mate who is next in line for the bathroom. You may not be absolved for your sins, but it’ll get you a laugh or two.

Krakatoa is a first class example of what happens when Mother Nature gets really cross and decides to let off a bomb that makes Hiroshima look like a fart. In 1883, the build-up of pressure under the Earth’s crust between the islands of Sumatra and Java in the Sunda Strait was so immense that it caused an apocalyptic-sized explosion, sending a once much bigger island into the stratosphere.

The Krakatoa eruption was reported to have been heard almost 5,000 km away (the loudest sound ever made in recorded history) and the resultant shock waves sent barograph needles oscillating violently off the page. Over 36,000 people were killed by the eruption: if not by the devastating pyroclastic flows and falling debris, then by the tsunamis that followed. The dust catapulted into the atmosphere caused stunning sunsets around the world for months after the eruption.

Too bad colour photography wasn’t in vogue in the 19th Century.

krakatoa - krakatau volcano map
Source: Krakatau Tour Website: A map of ex-Krakatoa and the now much smaller island of Anak Krakatau, which means “son of Krakatoa”. The dotted line represents the size of the island before it went nuclear.

Class Dismissed: Your Take-Home Message

If you ever needed to respect the fact that we are just not in control of our natural environment, then stand next to an active volcano. From lakes of lava and earthquakes that shake the foundations of your stick hut to falling debris and scalding hot pyroclastic flows that choke the biosphere, volcanoes are creatures to be respected, studied and understood. If ever there were an item to put on your bucket list, it would be to stand next to an active volcano and feel the heat of Earth’s exterior lap at your cheeks. Just make sure you’ve ticked off the rest of those bucket list items before you do so…

Mount Redoubt Eruption
“Mount Redoubt Eruption” by R. Clucas – Licensed under Public Domain via Wikimedia Commons. Mount Redoubt is a stratovolcano and is part of the very seismically active Aleutian Range in Alaska.

Life on Mars: Relocation, Relocation, Relocation!

Planet Mars with Rising Sun

Every single morning, when my alarm drops a hydrogen bomb into the middle of my sexy dreams, I lie in bed entertaining fantasies of further sleep. What would I do to be able to sink back into the cotton wool comfiness of my sub-consciousness for another half hour? In my irrational sleep-addled state, a lot! So, sign me up for the first commercial flight to Mars because with days that are not 30 minutes, but 40 minutes longer than on Earth, my desperate desire for extra sleep would be granted!

Curiosity Weighs 899 kg

Luckily There Aren’t Any Cats on Mars

On the 5th August of 2012, the Mars rover ‘Curiosity’ made a successful landing on the powdery, rock-strewn surface of the Red Planet. A part of the Mars Science Laboratory (MSL) mission, Curiosity’s primary objective is to explore the real estate on Mars and the possibility of humans inhabiting it at some time in the not-so-distant future.

Curiosity Mars Rover self-portraitA self-portrait of the Mars rover, Curiosity. #Selfie.

Image Credit: NASA/JPL-Caltech/Malin Space Science Systems. Derivative work including grading, distortion correction, minor local adjustments and rendering from tiff-file: Julian Herzog –

This sophisticated piece of machinery (see above image) cost NASA $2.5 billion to build and is designed to investigate features of Mars’ geology and climate during the course of its two-year long investigation. More specifically, the aptly-named ‘Curiosity’ will be looking for “ancient organic compounds,” according to NASA Ames Research Centre’s planetary scientist, Carol Stoker. This would help us understand the history of Mars, Earth’s sister planet,’ as a previous or even current supporter of life

All of the high tech gadgetry aboard the ‘Curiosity’ is essentially geared to measure the presence, nature and concentration of organic compounds that are possibly locked within the planet’s dry soils. After two years of exploration, ‘Curiosity’ will hopefully have answered our many pressing questions about the habitability of Mars. This could bring us closer, much closer, to planning an alternate future on the Red Planet… just in case we gas ourselves out of our own home in the solar system.

Or, you know, Bruce Willis chickens out of his mission to blow up an Earth-bound asteroid.

Meet The Red Planet! 

Planet Mars

Hey, hi, how are ya?

Astute academics such as Dr. Richard Zurek, Chief Scientist in the Mars Program Office at NASA’s Jet Propulsion Laboratory (JPL), have strong reason to suspect that Mars was once home to living organisms and that the Curiosity mission will indeed yield fruit. The presence of frozen water at the poles, an atmosphere that consists almost entirely of carbon dioxide, geological features that appear to have been carved and shaped by running water and a climate that is not wholly intolerable, indicate that out of all other known planets and moons in our solar system, Mars is or at least was the most accommodating of life.

What we want to know is whether we too could one day inhabit this arid red landscape… and if so, what would life on Mars be like?

Planet Profile: Mars

Mars planet

Etymology: Thanks to its blood-red colour, Mars was named by ancient civilizations after the Roman God of War.

Diameter: 6,787 kilometres

Average distance from Sun: 227,936,640 kilometres.

Rotation period (length of day): 1.026 Earth days

Orbital period (length of year): 686.98 Earth days

Menstrual period: huh?

Tilt of axis: 25° (Earth’s is approximately 23.4°)

Maximum surface temperature (tanning weather): 37°C

Minimum surface temperature (cuddle weather): -123°C

Best view from Mars: Olympus Mons, which is 27 kilometres higher than surrounding lava plains.

Atmospheric constituents: (1) 95% carbon dioxide, (2) 3% nitrogen, (3) 1.6% argon and (4) other trace gases. Methane was recently discovered there, too.

Your Martian Calendar and Climate

Because of Mars’ distance from the sun, 227,936,640 km on average, it takes quite a bit longer for it to bumble its way around the fiery focal point of our solar system. This means that a Martian year is much longer than an Earth year; approximately twice as long, in fact. There are 687 days in a year on Mars. Thanks to the planet’s tilted axis, however, there are still two primary seasons: summer and winter. This doesn’t really matter though. With average year-round temperatures of -60°C (-80°F) you’re still going to need to take a very warm jacket and maybe a pair of mittens, too. There are a few balmy days to look forward to… in summer, the mercury in Mars’ equatorial regions can actually hit 20°C (70°F), punctuated by days of a roasty toasty 37°C (98°F).

In spite of the cold, Mars is a desert planet, much like Tatooine, the one Star Wars’ Anakin Skywalker comes from… wait, hold on… did I just say that out loud? It never rains on Mars’ rust-red landscape and the only break you get in the distant and diluted sunshine is high level, coruscating congregations of ice-crystals; similar in fact to the cirrus clouds we get here on Earth. Bitterly cold winters aside, Mars would seem to be a rather affable place to settle.

Wouldn’t it?

Not always! When the horizon darkens and the wind picks up, it’s time to hit to road, Jack. Mars’ raging dust storms are the most tempestuous in the entire solar system.

Mars 2001 sandstorm NASA

In 2001, the Hubble Space Telescope captured the complete transformation of Mars as an enormous dust storm swept over the entire globe’s surface. These storms are driven by winds of up to 160 km/hr and can last weeks or even months. On the up-side, with nothing else to do other than stay inside, this would hurry along the population of Mars…

Martian Tourist Attractions

Once you get bored of admiring endless vistas of red nothingness and of tripping over the legions of sharp rocks that are ubiquitous to Mar’s dusty, empty landscape, you will need to take in a few of the planet’s more redeeming features. Thankfully, there are plenty of those. Mars offers some spectacular natural attractions that make the Grand Canyon look like a butt crack and Earth’s biggest volcano, Mauna Loa, look like a bug bite. Albeit a bad one.

Olympus Mons is Mars’ largest mountain/volcano/OMG-look-at-THAT!! At a lofty 27 kilometres (17 miles) high and an expansive 600 kilometres (372 miles) across, this megalith is three times as tall as Mount Everest, Earth’s largest mountain. It’s also the largest known volcano in the solar system.

Olympus Mons on Mars

What was once a suppurating abscess of death is now a brooding blackhead on the face of Mars’ blood-red landscape. Olympus Mons sits conspicuously in the top-right hand quadrant of this colorised topographical map of The Red Planet, from the MOLA instrument of Mars Global Surveyor.

Sciencey LOL of the Week

unny_science_test_answerI’m almost certain this kid knew the answer and, at the expense of one mark, decided this joke was too good to pass up on.

For those enquiring minds who really do want to know the answer…

Saturn is one of the largest planets in our solar system, in mass and size. It is known as a gassy giant because of its penchant for Mexican cuisine. I’m kidding. Because it is so massive and its gravity so great, that everything from giant space rocks to gass molecules were drawn in towards its centre at the formation of our solar system, approximately 4.5 billion years ago. If Saturn was just a little bit bigger (“a little bit” being an approximation for a whole lot), the intensity of its gravitational pull would have generated the central pressure and heat necessary to initiate nuclear reactions. And THIS would have made Saturn a star! The same applies to Jupiter, which is also a flatulant giant.

So, in other words, Saturn and Jupiter are failed stars… or that is what my astronomy professor always referred to them as.

Picture of planet Saturn
Saturn in all its real colour glory. This image was taken by the Cassini satellite in 2004. As a matter of interest, Saturn appears a sickly yellow colour due to the great glittering clouds of ammonia crystals held aloft in its atmosphere. I can only imagine what smells one would have to endure on a stroll around Saturn. Similar to your single toilet after you and 15 of your beer-soaked friends have relieved yourselves, I’m guessing.

Saturn’s rings are composed of orbiting particles of rocks and ice, some no bigger than snowballs and others the size of a bus, according to NASA’s fun cosmology website. Each of these particles, gargantuam and minute, are by definition moons, all in gentle orbit around the giant planet. They share this orbit with 63 other more “traditional” moons, the largest of which is the aptly-named Titan.

While it is unclear as to why all of this orbiting debris has accumulated into almost perfect geometric circles around the planet, the answer is suspected to lie in gravity. Over the many millions of years subsequent to the formation of the solar system (or seven days subsequent to creation), each particulate, snowball, moon and hunk of rock has had the time to settle into a position that reflects, in part, the force of attraction between itself and its giant parent planet. One might suspect that the larger, heavier particles will be arranged in belts closest to the planet, while the lighter and less dense particles will be in belts further away.

Saturn's ringsAnd you might suspect this because the force of attraction between two objects is proportionate to their respective masses and disproportionate to the distance between them. In other words, the heavier you are, the more attractive Earth finds you, which is why your bathroom scale groans every morning. You can refer to this spectacular blog entry for elucidation on this point: Gravity And The Laws of Attraction, Somewhat Revised.

This is precisely what I thought, but the picture is more complex than that. Each particle in orbit around its central giant – each particle of dust and each bus-sized space rock – is travelling at a certain speed. And while gravity acts to pull these particles in towards Saturn, they continue along a path that is perpendicular to it, rather than careening inwards. The force that propels these “moons” forward is called the centripetal force and you would have experienced that as a child when you were flung off a merry-go-round, because your douchebag brother seemed to think the word “stop!” meant “faster!”

Saturn’s rings are therefore organised into belts of particles that are travelling at different velocities. I have a very helpful reader to thank for this relevation and you will find his comment below.

And so, this gasy giant finds itself swathed in many beautiful, carefully arranged rings all consisting of particles, rocks, snowballs and moons travelling at varying velocities; trapped in an eternal dance around itself. Here’s something else: so does Jupiter and Neptune! The only difference is that the two latter planets’ bridal trains are thinner and far more translucent and so Saturn, with its ostentatious display, has become the planet in our solar system famed for its rings.

beyonce-put a ring on it