If you asked the question, you already know the answer.
Maybe I will be pleasantly surprised one day?
If you asked the question, you already know the answer.
India conducted a successful anti-satellite test today.
I thought there might be a discussion about sexist space suits going on in here. Alas, no.
Maybe I will be pleasantly surprised one day?
Okay, how in the hell can we be sure about most of the stuff we think we know if we were off by a factor of 10 about our own sun's magnetic field?
https://phys.org/news/2019-03-million-year-old-deathbed-linked-dinosaur-killing-meteor.html
On a branch of an inland sea in North America - N Dakota to be specific - a rather unique situation gave us the best find to date showing how animals died when a 6-mile wide chunk of rock from space killed off 75% of life on the planet 66 million years ago.
The impact on the northern Yucatan peninsula generated massive quakes that sent shock waves around the world possibly magnifying or resuming eruptions of lava in India's Deccan Traps region and tsunamis even on bodies of water far from the ocean.
In North Dakota a large inland sea began sloshing back and forth dumping fish and marine life up onto the shore at about the same time rock melted by the impact was falling from the sky. These little bullets - tektites, spherules - rained down igniting fires and becoming embedded in animals and trees at speeds of 100-200 mph.
Some of these missiles hit trees and became surrounded by amber, they're the best unaltered samples of material from the impact found so far. Some fish lived long enough for these melted pieces of debris to lodge in their gills and feeding mechanisms only to be buried minutes later by another tsunami's sediments and gravel.
More than 99.9999 per cent of all living organisms on Earth died, and the carbon cycle came to a halt.
Earth itself became toxic.
the new yorker article says the inland sea was actually a seaway linked to the Gulf which I presume means the Yucatan splashdown had a direct line for tsunamis
After the G.S.A. talk, DePalma realized that his theory of what had happened at Tanis had a fundamental problem. The KT tsunami, even moving at more than a hundred miles an hour, would have taken many hours to travel the two thousand miles to the site. The rainfall of glass blobs, however, would have hit the area and stopped within about an hour after the impact. And yet the tektites fell into an active flood. The timing was all wrong.
This was not a paleontological question; it was a problem of geophysics and sedimentology. Smit was a sedimentologist, and another researcher whom DePalma shared his data with, Mark Richards, now of the University of Washington, was a geophysicist. At dinner one evening in Nagpur, India, where they were attending a conference, Smit and Richards talked about the problem, looked up a few papers, and later jotted down some rough calculations. It was immediately apparent to them that the KT tsunami would have arrived too late to capture the falling tektites; the wave would also have been too diminished by its long journey to account for the thirty-five-foot rise of water at Tanis. One of them proposed that the wave might have been created by a curious phenomenon known as a seiche. In large earthquakes, the shaking of the ground sometimes causes water in ponds, swimming pools, and bathtubs to slosh back and forth. Richards recalled that the 2011 Japanese earthquake produced bizarre, five-foot seiche waves in an absolutely calm Norwegian fjord thirty minutes after the quake, in a place unreachable by the tsunami.
Richards had previously estimated that the worldwide earthquake generated by the KT impact could have been a thousand times stronger than the biggest earthquake ever experienced in human history. Using that gauge, he calculated that potent seismic waves would have arrived at Tanis six minutes, ten minutes, and thirteen minutes after the impact. (Different types of seismic waves travel at different speeds.) The brutal shaking would have been enough to trigger a large seiche, and the first blobs of glass would have started to rain down seconds or minutes afterward. They would have continued to fall as the seiche waves rolled in and out, depositing layer upon layer of sediment and each time sealing the tektites in place. The Tanis site, in short, did not span the first day of the impact: it probably recorded the first hour or so. This fact, if true, renders the site even more fabulous than previously thought. It is almost beyond credibility that a precise geological transcript of the most important sixty minutes of Earth’s history could still exist millions of years later—a sort of high-speed, high-resolution video of the event recorded in fine layers of stone. DePalma said, “It’s like finding the Holy Grail clutched in the bony fingers of Jimmy Hoffa, sitting on top of the Lost Ark.” If Tanis had been closer to or farther from the impact point, this beautiful coincidence of timing could not have happened. “There’s nothing in the world that’s ever been seen like this,” Richards told me.
thats true, even at the speed of a jet airliner it would have taken several hours to reach N Dakota but shockwaves would have taken much less time
I missed the 1,000 ppm in the article, do they have a measure for the layer deposited by impact debris? I imagine there's one helluva spike representing the KT boundary.
We lost a good chunk of Florida about 125-115kya during a warm period as seas were several meters higher back then.
"Currently, carbon dioxide levels are just above 400 parts per million (ppm), up approximately 120 ppm in the last 150 years and rising about 2 ppm each year," said Ken MacLeod, a professor of geological sciences at MU. "In our study, we found that during the Late Cretaceous Period, when carbon dioxide levels were around 1,000 ppm, there were no continental ice sheets on earth. So, if carbon dioxide levels continue to rise, the earth will be ice-free once the climate comes into balance with the higher levels."
When the asteroid struck, it vaporized layers of limestone, releasing into the atmosphere a trillion tons of carbon dioxide, ten billion tons of methane, and a billion tons of carbon monoxide; all three are powerful greenhouse gases. The impact also vaporized anhydrite rock, which blasted ten trillion tons of sulfur compounds aloft. The sulfur combined with water to form sulfuric acid, which then fell as an acid rain that may have been potent enough to strip the leaves from any surviving plants and to leach the nutrients from the soil.
Today, the layer of debris, ash, and soot deposited by the asteroid strike is preserved in the Earth’s sediment as a stripe of black about the thickness of a notebook. This is called the KT boundary, because it marks the dividing line between the Cretaceous period and the Tertiary period. (The Tertiary has been redefined as the Paleogene, but the term “KT” persists.) Mysteries abound above and below the KT layer. In the late Cretaceous, widespread volcanoes spewed vast quantities of gas and dust into the atmosphere, and the air contained far higher levels of carbon dioxide than the air that we breathe now. The climate was tropical, and the planet was perhaps entirely free of ice. Yet scientists know very little about the animals and plants that were living at the time, and as a result they have been searching for fossil deposits as close to the KT boundary as possible.
I don't have high confidence that we would spot a planet-killer before it hit. We've had recent high-profile impacts like Chelyabinsk that came out of nowhere. Even though they were smaller rocks, they were still big enough to take down a city had the impact angles been different. There are lots and lots of 6-mile asteroids out there and while I could go along with the notion that we've spotted most of them, we haven't spotted them all.
We are protected in large part by the extremely low odds of any two objects colliding in space but we're playing a numbers game right now that we will lose given enough time. This is one area I believe a Space Force should play a large role in. NASA is awesome but no one gets funded like the military and this is a big enough threat that it is worth devoting serious resources too.