Book Review: The Galactic Supermassive Black Hole

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Combining large scale astronomical observations with the careful reasoning of physics leads to the widely encompassing field of astrophysics. Apparently, the physical laws that rule interactions on Earth also rule the actions across our universe. Fulvio Melia takes this consideration to task in his book The Galactic Supermassive Black Hole. Within the book, the equations bring reason to some very murky observations and sharpen our view of the heavens.

The target of Melia’s book is our own active galactic centre; the region in and about Sagittarius A*. One of today’s postulations is that each galaxy has a supermassive black hole at its centre. Thus, we’d expect to see a black hole in or near Sagittarius A*. But this raises the question, “How does one see a black hole?”. For, of course, a black hole absorbs everything about it, including light, so there is little for satellites to detect. Nevertheless, though we aren’t able to directly see a black hole, there are many other indicators foretelling such an astronomical entity. Thus, by observation, inference and a great deal of reliance upon physical laws, Melia dishes out reason about the contents of our galactic centre.

To make reason, Melia provides the tools and background throughout his book. He begins with a brief review of relevant observational data about Sagittarius A*. In particular, he looks at emission strengths and characteristics for various energy levels. As an example of the difficulties of this subject, much of the observation supports each other, but yet there’s no exact match. Thus, there’s the need to account for the common problems with astronomy, in that targets move, viewing platforms shake and differences arise for no known cause. Nevertheless, with diagrams, graphs and satellite survey results, Melia shows the data that’s important and provides ways and means to interpret it.

After this review, Melia takes the reader through some simple and some esoteric mathematical manipulations. The simple is setting up transformation matrices for four-dimensional space time. He then goes on to utilize these constructs as a substrate for simulations of the magnetohydrodynamic properties at the galactic centre. These equations come after some development, though many are results from other, external works or papers (that are usually referenced). The equations aren’t present for an intimidation factor, however. Rather, Melia uses them to construct comparative figures and graphs. And, with these, he brings together the hard relations of physics with the softer visages from the satellites. In consequence, the reader, if they can follow the mathematical development, will have effective and viable tools for analyzing the expected properties at our, and other, active galactic nuclei. This is as wonderfully complete as a reader could expect for introductory analytical tools.

And the target audience of this book is the people who are thinking of extending their interests into active galactic nuclei. Melia’s stated goal with the book is to help young astronomers come up to speed with mature primary literature on Sagittarius A*. This book is a great resource for doing just this. By providing background references, establishing equations and comparing theory to observation, this book has excellent breadth. With the derivation of equations and presentation of typical hard data, this book has good depth. For those well into the wonders of astronomy and astrophysics, reading this book would be just the treat to help them reach further into this specialized area of astrophysics.

However, for those readers who are more interested in results or enjoying the view, this book may have too much depth. Integrals, distribution functions and relativistic motion are all present and are necessary preparations for many of Melia’s discussions. His expectation, apparently, is that the reader is comfortable with this technical level. Thus, he doesn’t draw out derivations. A reader, unfamiliar with this level, may soon find themselves grasping for understanding.

Yet, for those who want to make a serious commitment in the field of active galactic nuclei, particularly of Sagittarius A*, this is a very thorough and polished book. The chapters and material follow on naturally. There aren’t surprises nor need for guess work. Somewhat unsettling is the ending. Here, Melia skips from a paragraph on needed telescope upgrades to the next paragraph, where he states that his book is at best a work in progress. The reader, therefore, is left hanging. There’s very little on expected future research efforts, centres of research or practitioners in the field. Thus, if a person is contemplating further study, they may know more of what to do from reading this book, but they will need to look elsewhere on how best to contribute to the field.

The light from far away stars, beautiful in its own right, can carry great meaning. As it bounces off of dust or reflects about great masses of matter, we can infer details. Fulvio Melia in his book The Galactic Supermassive Black Hole combines the little information we can detect from our galactic centre together with our accepted laws of physics. This foundation is just waiting for the next contributor to extend our knowledge into the further reaches of space.

Read more reviews or purchase a copy online from Amazon.com

SMART-1 Links Geologic and Volcanic Activity on the Moon

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ESA’s SMART-1 spacecraft was purposely crashed into the Moon on September 3, 2006. But before it died, it analyzed the Moon in incredible detail. One of the key questions it’s attempting to help scientists answer: how were surface features formed? By putting together data from both SMART-1 and NASA’s Clementine spacecraft, scientists have detailed views of some of the fine details that will help answer these questions.

Most of the Moon’s surface features – all those big craters – were created approximately 350-750 million years after the formation of the Moon, during a period called the Lunar Late Heavy Bombardment period. Almost all of the large lunar basins 300 km or larger were created during that period. And then after that, many of these basins were filled in by lava from volcanic activity.

By combining images from SMART-1 and Clementine, scientists can now see many of the fine geological structures, using SMART-1’s AMIE micro-camera. During its orbits, SMART-1 passed very close to the surface of the Moon, and took low-elevation images that revealed very fine scale geological features that had been undetected before now.

One example of this is the Humorum basin; a nice, round compact basin that was created by a simple impact event. The spacecraft data shows a thin crust and mass concentration within a small area.

This is different from the Procellarum basin. This region is a large, extended, complex basin that is moderately thick and has no mass concentration. It might have been formed by faulting associated with an adjacent crater, and not a gigantic impact.

Each lunar crater has a story to tell. The SMART-1 data is helping scientists understand when the Moon was volcanically active, and how and when the lava flowed into ancient impact craters.

Original Source: EPC News Release

Details on Germany’s Lunar Exploration Orbiter

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The Moon is going to be a busy place. NASA is sending the Lunar Reconnaissance Orbiter in 2008, and will be sending humans back as early as 2020. Germany, a member of the European Space Agency, announced they’ll be getting in the lunar game too. Their recently announced Lunar Exploration Orbiter will be heading to the Moon in 2012, giving our satellite another satellite of its own.

The new details on the Lunar Exploration Orbiter were announced at the European Planetary Science Congress, which is being held this week in Potsdam.

The mission will consist of two spacecraft flying in formation, and taking simultaneous measurements of the lunar surface. As with NASA’s Stereo mission, targeted at the Sun, this twin vision will give scientists a true stereoscopic view of the Moon’s surface features. The Moon, in thrilling 3-D!

It will also be able to study the Moon’s magnetic and gravitational fields in 3 dimensions as well, both on the near side, and the far side of the Moon. The main satellite will weigh about 500 kg (1100 pounds), and the secondary satellite will only weigh about 150 kg (330 pounds), carrying duplicate magnetic and gravity instruments.

The main satellite carries a microwave radar that will allow it to peer beneath the lunar surface to a depth of several hundred metres. At maximum depths, it’ll be able to resolve structures two metres across, and within the top few metres, it’ll be able to resolve structures just a few millimetres across. This will help scientists track the distribution of rocks and particles, and help reveal the history of impacts.

LEO will create high resolution maps of the entire lunar surface in stereo and multispectral bands. The whole mission should last 4 years, so it will even be able to watch for new impacts, by looking for new craters and detecting impact events. That should be pretty impressive.

STS-118: Endeavour Touches Down Safely in Florida

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After 13 days in space, the space shuttle Endeavour touched down safely in Florida today. NASA managers actually decided to bring the shuttle home a day early, to beat Hurricane Dean, currently ravaging the East Coast of Mexico. Despite the nearby stormy weather, conditions at Cape Canaveral were perfect for landing.

NASA managers gave the Endeavour crew instructions to begin their de-orbit burn at 11:05 am EDT. 30 minutes later they fired their retro rockets for 3.5 minutes, slowing their orbital speed enough to get caught by the Earth’s atmosphere. The shuttle descended through breezy, blue skies across Costa Rica, Cuba, and then onto the 3-mile (4.8 km) landing strip in Florida. It rolled to a stop at 12:32 pm EDT.

The reason for the early return was Hurricane Dean, which had recently passed through Jamaica, and is now tearing up the coastal resorts in Mexico. The category 5 hurricane ended up turning south, but had it continued north, it could have forced an evacuation of the Kennedy Space Center in Florida.

Engineers were a little concerned about the landing, because of the small chunk taken out of the shuttle’s protective heat tiles on its underside. A small piece of foam fell off the shuttle’s insulated external fuel tank and gouged out a hole across two tiles. NASA analyzed the damage and calculated that it wouldn’t pose a risk to the shuttle or the crew. They were certain that it wouldn’t even damage the shuttle’s aluminum frame, requiring extensive repairs. They landed safely, but what kind of damage the shuttle took still remains to be seen.

During their time in space, the crew of STS-118 installed a new truss element onto the station, transfered cargo, and reorganized some communications equipment.

Original Source: NASA News Release

Closest Neutron Star Discovered

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Canadian and US astronomers have located what is thought to be the closest neutron star ever seen. The exotic object, nicknamed Calvera after the villain in the movie “The Magnificent Seven”, is located in the constellation Ursa Minor, somewhere between 250 and 1,000 light-years away. It’s a member of a rare group of isolated neutron stars – they lack binary companions – and could be just the tip of the iceberg.

The discovering astronomers pored over a gigantic catalog of 18,000 X-ray sources captured by the German-American ROSAT satellite, which was operational between 1990 and 1999. They compared these X-ray sources to objects visible other wavelengths of light, such as infrared, visible light, and radio waves. One object, 1RXS J141256.0+792204, stood out as being visible only in X-rays.

Then they targeted the object with NASA’s Swift satellite, and performed more detailed observations. Swift was able to find the source, and confirmed that it was putting out as much X-ray energy today as had been captured by ROSAT. Then they pointed one of the most powerful telescopes on Earth, the 8.1 Gemini North Telescope in Hawaii, and couldn’t find a single optical light object down to the faintest magnitudes. It was only shining in X-rays.

According to the researchers, there are no widely accepted alternate theories for objects like Calvera, which are bright in X-rays, but faint in visible light. Either it’s an unusual example of a neutron star, or it might be a completely new kind of object. Another mystery: it’s high above the plane of the Milky Way Galaxy. It must have formed in the plane, but then somehow migrated up to its current position.

With the discovery of Calvera, astronomers think there could be many objects like this. It’s close enough that astronomers will be able to perform detailed observations with many instruments. It should yield interesting results for years to come.

Original Source: PSU News Release

Podcast: Venus

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The planet Venus, as imagined by the Magellan 10 mission. Credit: NASA/JPL

Last week we talked about Mercury, so this week our planetary parade proceeds to Venus. It’s the brightest object in the sky, the hottest object in the solar system, and it’s probably one of the most deadly places to go and visit. You might be amazed to know that spacecraft have actually reached the surface of Venus and taken pictures. Find out more about our Earth’s evil twin planet.

Click here to download the episode

Venus – Show notes and transcript

Or subscribe to: astronomycast.com/podcast.xml with your podcatching software.

What’s Up this Week: August 20 – August 26, 2007

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Monday, August 20 – Our first order of business for the evening will be to pick up a lunar club challenge that we haven’t noted yet – Hipparchus.

Located just slightly south of the central point of the Moon and very near the terminator, this is not truly a crater – but a hexagonal mountain-walled plain. Spanning about 150 kilometers in diameter with walls around 3320 meters high, it is bordered just inside its northern wall by crater Horrocks. This deep appearing “well” is 30 kilometers in diameter and its rugged interior drops down an additional 2980 meters below the floor. To the south and just outside the edge of the plain is crater Halley. Slightly larger at 36 kilometers in diameter, this crater named for Sir Edmund is a little shallower at 2510 meters deep – but it has a very smooth floor. To the east you’ll see a series of three small craters, the largest of which is Hind.

Now, relax! Tonight is the peak of the Kappa Cygnid meteor shower. Although the Moon will interfere early in the evening, wait until it has set and watch the area near Deneb. Discovered in the late 1800’s, the Kappa Cygnids are often overlooked because the grander, more prolific Perseids tend to get more attention. Although the stream has been verified, peak dates and fall rates vary from year to year. The average fall rate is usually no more than 5 per hour, but it is not uncommon to see 12 or more per hour with many fireballs. The stream’s duration is around 15 days. Clear skies!

Tuesday, August 21 – When we begin our observations tonight, we’ll start by having a look at another great study crater – Archimedes. You’ll find it located in the Imbrium plain north of the Apennine Mountains and west of Autolycus.

Under this lighting, the bright ring of this class V walled plain extends 83 kilometers in diameter. Even though it looks to be quite shallow, it still has impressive 2150 meter high walls. To its south is a feature not often recognized – the Montes Archimedes. Though this relatively short range is well eroded, it still shows across 140 kilometers of lunar topography. Look for a shallow rima that extends southeast across Palus Putredinus towards the Apennines. Mark your challenge notes!

Now let’s go have a look at a star buried in one of the spiral arms of our own galaxy – W Sagittarii…

Located less than a fingerwidth north of Gamma, the tip of the “teapot spout,” W is a Cepheid variable that’s worth keeping an eye on. While its brightness only varies by less than a magnitude, it does so in less than 8 days! Normally holding close to a magnitude 4, nearby field stars will help you correctly assess when minimum and maximum occur. While it’s difficult for a beginner to see such changes, watch it over a period of time. At maximum, it will be only slightly fainter than Gamma to the south. At minimum, it will be only slightly brighter than the stars to its northeast and southwest.

While you watch W go through its changes – think on this: not only is W a Cepheid variable (a standard for distance measurements), but it is also one that periodically changes its shape. Not enough? Then think twice… Because W is also a Cepheid binary. Still not enough? Then you might like to know that recent research points toward W having a third companion as well!

Wednesday, August 22 – Tonight as the skies darken, look for Antares less than a degree north of moon. For some areas of the world, this could be an occultation event so be sure to check IOTA… And while you’re watching, check out Jupiter about 5 degrees further to the north!

Tonight will be another opportunity to note a lunar challenge feature you may have missed earlier in the year – The Straight Wall. Begin in the lunar south where you can’t miss the outstanding rings of craters Ptolemaeus, Alphonsus, Arzachel, Purbach and Walter descending from north to south. To the west, identify the beginnings of Mare Nubium. Look between Purbach and Walter for the small, bright ring of Thebit and further west and for a long, thin, dark “line” cutting across the mare. It is properly known as Rupes Recta – but more commonly called “The Straight Wall.” It’s one of the steepest slopes on the lunar surface and only visible when the lighting is just right. If you can’t see it tonight, try again in 15 days when the sunlight changes the viewing angle!

Although it will be tough to locate with the unaided eye thanks to the Moon, let’s take a closer look at one of the most unsung stars in this region of sky – Eta Sagittarii. This M-class giant star will show a wonderful color contrast to binoculars or scopes, being slightly more orange than the surrounding field. Located 149 light-years away, this irregular variable star is a source of infrared radiation and is a little larger than our own Sun – yet 585 times brighter. At around 3 billion years old, Eta has either expended its helium core or just begun to use it to fuse carbon and oxygen – creating an unstable star capable of changing its luminosity by about 4%. But have a closer look… For Eta is also a binary system with an 8th magnitude companion!

Thursday, August 23 – Do you remember a few days ago in history when Lunar Orbiter 1 was launched? Well, on this day in history it made headlines as it sent back the very first photo of Earth seen from space!

Tonight let’s do a little lunar orbiting of our own as we head to the western shore of Mare Cognitum and look along the terminator for the Montes Riphaeus – “The Mountains In The Middle of Nowhere.” But are they really mountains? Let’s take a look.

At the widest, this unusual range spans about 38 kilometers and runs for a distance of around 177 kilometers. Less impressive than most lunar mountain ranges, some peaks reach up to 1250 meters high, making these summits about the same height as our volcano Mt. Kilauea. While we are considering volcanic activity, consider that these peaks are all that is left of Mare Cognitum’s walls after lava filled it in. At one time this may have been amongst the tallest of lunar features!

Now let’s have a look at the brightest star in the “Archer” – Epsilon Sagittarii. Known as Kaus Australis, or the “Southern Bow,” Epsilon holds a respectable magnitude 1.8 and is located around 120 light-years from Earth. This sparkling blue/white star is 250 times brighter than our own Sun. While a major challenge would be to spot Epsilon’s 14th magnitude companion star located about 32″ away, even the smallest of telescopes and most binoculars can try for the 7th magnitude visual companion widely spaced to the north-northwest.

Friday, August 24 – Today in 1966 from an Earth-orbiting platform, the Luna 11 mission was launched on a three day trip. After successfully achieving orbit, the mission went on to study many things, including lunar composition and nearby meteoroid streams.

Tonight let’s start our lunar observations with features that can be seen with both binoculars and telescopes. Just slightly north of center along the terminator, look for the bright point of Kepler. Watch as this feature develops a bright ray system in the coming days. To the north you will see equally bright Aristarchus – quite probably one of the youngest of the prominent features at around 50 million years old. It will also develop a ray system.

Now, grab your telescope and look west of Aristarchus for less prominent crater Herodotus. Just to the north you will see a fine white thread known as Vallis Schroteri – or Schroter’s Valley. Winding its way across the Aristarchus plain, this feature is about 160 kilometers long, from 3 to 8 kilometers wide, and about 1 kilometer deep – but what is it?

Schroter’s Valley a prime example of a collapsed lava tube – created when molten rock flowed over the surface. This may have been from a major meteor strike, such as the formation of Aristarchus crater, or early volcanic activity. What is left is a long, narrow cave on the surface which only shows well when the lighting is correct. Like many sinuous rilles covering the surface, collapse has occurred. If intact tubes can be found on the lunar surface they could conceivably provide shelter for future settlers!

Saturday, August 25 – Tonight we’ll start our observations in the lunar southwest as we look along the terminator to identify challenge crater Schickard. Look for an elongated grey oval that’s more than just another cool crater…

Named for Dutch mathematician and astronomer Wilhelm Schickard, this 227 kilometer diameter feature is a ringed plain and very old. At high power you’ll see a variegated floor and dark areas near the walls – yet the center is creased by a lighter coloration. It is believed Schickard was formed by an early impact before Mare Nectaris formed. Its floor may have contained vents which allowed it to fill with lava during the Imbrium period. As it cooled and matured another impact event occurred nearby which formed the Orientale Basin and splashed material its way. But Schickard wasn’t done evolving yet… Lava continued to flow and left even more dark evidence for us to observe. How do we know this is so? If you’re able to resolve Schickard’s tiny interior impacts, you’ll see that far fewer of them occur over newer material. Older formations bear the scars of time and impact while younger features are fresh and unmarked!

Tonight is also the peak of the Northern Iota Aquarid meteor shower. While the Moon will totally interfere, you still might catch a bright streak!

Sunday, August 26 – Tonight we’ll continue our journey of lunar evolution as we have a look at another walled plain just south of Grimaldi.

Named for English naturalist Charles Darwin, this equally old feature bears the scars of the impact the created the Orientale Basin. Look carefully at the slopes in the northeast, for this may very well be material that was thrown there and left to slide back down to the crater floor. Spanning around 130 kilometers in diameter, Darwin’s actual size is only diminished by the fact that we view it on a curve. Its northern and southern shores have almost completely eroded, yet evidence remains of its eastern margin broken by the Rima Darwin which stretches for 280 kilometers. Was there lava here as well? Yes. Evidence still exists in the form of a dome along Darwin’s battered western edge.

On this date in 1981, Voyager 2 made a fly-by of Saturn. Eight years later in 1989, Voyager 2 flew by Neptune on this date. Why don’t we make a “date” tonight to have a look at this distant blue world? You’ll find it on the ecliptic plane east of the Moon. While large binoculars can pick up Neptune’s very tiny blue orb, you’ll need a telescope tonight to spot it through the lunar glare.

Arctic Ice Coverage Will Shrink to 2050 Projections… This Summer

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Sometimes you wish records didn’t get broken. A group of Japanese science agencies announced today that the area of the Arctic Sea covered by ice is at its lowest level ever recorded. It reached this low point on August 15th, and it’s going to get worse. Ice levels should continue to shrink all the way through mid-September. If reality matches predictions, the ice levels will reach IPCC predictions 40 years ahead of schedule.

On August 15th, 2007 the area of Arctic sea ice was 5.31 million square km (2.1 million square miles). This beats the previous record of 5.32 million seen back in September 2005. That might sound like it’s almost the same amount, but just you wait, ice is expected to continue shrinking until mid-September, getting as small as 4.5 million square km.

These results were announced today by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) and the Japan Aerospace Exploration Agency (JAXA), which have been tracking Arctic ice levels by satellite since 1978. By their calculation, an amount of ice equal to the Japanese archipelago has been lost in just the last 3 years.

According to the Japanese agencies, there could be several reasons why the ice levels are so low this year. One explanation is that ice in coastal areas which is more prone to melting could have entered the Arctic Sea. It’s also possible that melting within the Arctic Sea has quickened – thanks to global warming – and is leading to the ocean absorbing more sunlight. Finally, they suggest that more sea ice could have drifted from the Arctic Sea to the warmer Atlantic Ocean and melted.

Here’s the scary part. The United Nations Intergovernmental Panel on Climate Change predicted that this level of ice coverage would be met in 2050. I’ll say that again, Arctic ice will reach levels predicted for 2050 by the end of this summer. I wonder what the levels will be in 2050?

Here’s what one official had to say about the IPCC predictions:

The IPCC forecast cannot adequately explain what is now happening in the Arctic Sea.

Original Source: JAXA News Release

Bigelow Speeds Up Plans for a Human Habitable Space Station

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Where are you planning to go on your next vacation? Hawaii, Mexico, or Europe would be nice. But what about a trip into orbit? Space tourism entrepreneur Robert Bigelow announced this week that he’s going to be fast tracking his plans to a launch an orbital space hotel. With his current prototypes, Genesis 1 and 2 already in orbit, Bigelow has decided to skip another unmanned prototype and go straight for the habitable Sundancer module, launching as early as 2010.

Bigelow posted the news on his company’s website this week.

According to Bigelow, the incentive for the decision came from the rising costs of launching spacecraft into orbit. The company was originally planning to launch its Galaxy prototype next. This was supposed to be a 45% scale prototype module that would bridge the gap between the Genesis modules and the first human test module: Sundancer. After both Genesis modules launched successfully, and have been sending back exactly the kinds of scientific information Bigelow Aerospace required, the company decided another unmanned prototype wasn’t necessary.

The company will still construct and test the Galaxy prototype, in order to gain familiarity and experience with the subsystems, but they won’t actually launch it. This gives time in their schedule, and additional budget to move up the launch of the Sundancer prototype.

When it finally launches, Sundancer will be capable of accommodating three people in orbit. In his website post, Bigelow targeted 2010 as a possible launch date, but speculates that it might happen “much earlier than any of us had previously anticipated.” So, maybe even 2009 isn’t out of the question.

How people are actually going to reach their hotel in space, that’s another question.

Original Source:Bigelow News Release

Did Life on Earth Originate With Comets?

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The traditional thinking is that life on Earth began… on Earth. At some point in our distant past, some mixture of amino acids made the jump from a pool of organic molecules to something more lifelike. But maybe the source of life on Earth came from space, hitching a ride aboard balls of ice and dust: comets.

This is the controversial theory proposed by Chandra Wickramasinghe, an astrobiologist at Cardiff University in the United Kingdom. Wickramasinghe is one of the long time proponents for the theory of panspermia; that life on Earth originated from space or another planet.

Wickramasinghe and his team are claiming that new evidence gathered by space probes reveals how these first organisms could have gotten started.

When NASA’s Deep Impact spacecraft ended its life in 2005, crashing into Comet Tempel 1, it discovered a mixture of organic and clay particles inside the comet. One theory about the origins of life is that clay particles act as a catalyst, allowing simple organic molecules to get arranged into more and more complex structures. The 2004 Stardust mission found a range of complex hydrocarbon molecules when it collected particles from Comet Wild 2.

The Cardiff team think that radioactive elements inside comets could make pockets warm and toasty enough to keep water in its liquid form for millions of years. These iceballs could serve as the perfect incubators for early life. And when one finally crashes into a planet, it delivers this life to its new home.

There are so many comets out there, with potentially so many liquid pockets inside, that Wickramasinghe and team calculated that the likelihood is far greater that life got started in comets, and not here on Earth.

With any controversial theory, there are many scientists who think this is just too speculative. Without actual evidence for one of these oases inside a comet, it’s just an interesting idea. Perhaps ESA’s Rosetta mission, currently on its way to Comet 67P/Churyumov-Gerasimenko, and equipped with a lander will be just to tool to gather this kind of evidence.

Original Source: Cardiff News Release