Blog

Archive for the ‘Tunguska’ tag

Jan 27, 2013

AIAA Rocky Mountain — Sentinel Program

Posted by in categories: asteroid/comet impacts, business, defense, education, engineering, events, physics, space

For those in Colorado who are interested in attending a talk by John Troeltzsch, Sentinel Ball Program Manager, Ball Aerospace & Technologies Corp. please R.S.V.P Chris Zeller (czeller@ball.com) by Tuesday, 26 February 2013 for badge access. US citizenship required.

6:00 pm Thursday, February 28th 2013
6:00 pm Social, 6:30 pm Program
Ball Aerospace Boulder Campus RA7 Conference Room
1600 Commerce St
Boulder, CO 80301

It will be good to see you there.

About the Talk:
The inner solar system is populated with a half million asteroids larger than the one that struck Tunguska and yet we’ve identified and mapped only about one percent of these asteroids to date.

Continue reading “AIAA Rocky Mountain — Sentinel Program” »

Jan 4, 2011

Public comments invited: Asteroid Apocalypse (part 2, bigger than Tunguska)

Posted by in categories: asteroid/comet impacts, cosmology, existential risks, futurism, space

(See also part 1, Tunguska below)

Powerful though it was, the Tunguska event was just a fire cracker compared to what can happen. Bigger asteroids can resist complete atmospheric breakup long enough to blow up on contact with the ground. The result is an impact crater, which can blast enough pulverized rock into the atmosphere to change the climate dramatically, perhaps for months, over the entire world. One such impact killed the dinosaurs 65 million years ago, when asteroid Dinolith slammed into the ground near Chicxulub town on the Yucatan peninsula, in Mexico. It has been argued, however, that some dinosaurs survived and live on today. We call them birds (some we call “hummingbirds”).

A much more recent and, thankfully, smaller one landed only 50,000 years old. It is about 3/4 mile in diameter, and is now billed as “the world’s best preserved meteorite impact site just minutes from Interstate 40.” In Arizona, it is owned by the Barringer Crater Co., perhaps the world’s only legitimate crater company. There are some other crater companies that will sell you craters and other land on the moon and other extraterrestrial getaways. However under established international law they do not actually own what they are selling, and so can hardly be considered legitimate. Other companies sell merely certificates of ownership to extraterrestrial craters and such, not the craters themselves, leaving it to the possessors of the certificates to try to enforce their claims of ownership. Those companies may be legitimate, but are really certificate companies, not crater companies. For those who feel that priceless and unique geological treasures should not be privately owned, even the Barringer Crater Co. is not legitimate, leaving the world without even one legitimate crater company. In any event, this crater is also unique in being the world’s most plainly named crater: its legal name is “Meteor Crater.” It is now marketed as a tourist attraction, not having the billion dollars worth of buried iron that old man Barringer hoped for when he acquired it in 1903.

The largest impact crater on Earth known with certainty is the Vredefort crater in South Africa at about 170 miles across. It was crated when asteroid Archaeoaster (“ark-ee-oh-aster”), 3 to 6 miles in diameter, slammed into Earth just over 2 billion years ago, long before the first dinosaur stepped out of its eggshell. The largest in the U.S. is Chesapeake Bay on the coasts of Maryland and Virginia. Impact craters on Earth tend to weather to the point that it is not obvious to the naive observer that they are craters. On the other hand, the moon is pockmarked with numerous and well-preserved impact craters easily visible through telescopes, because erosion from atmospheric winds and surface liquids does not happen there.

Dec 28, 2010

Asteroid Apocalypse (part 1: Tunguska)

Posted by in categories: asteroid/comet impacts, cosmology, defense, existential risks, futurism, space

Back in 1908 — just yesterday, geologically speaking — a huge blast occurred over a swampy area near the Lower Stony Tunguska River. In case you forgot from high school geography class, this is about 40 miles from Vanavara in Siberia. The explosive force of the Tunguska Event has been variously calculated but agreed to be in the ballpark of an H-bomb, perhaps around 10 megatons (a megaton is the energy released by exploding a million tons of TNT). It was not a H-bomb however, but evidently an asteroid tens of meters (perhaps as low as 20) in diameter, that crashed into the atmosphere at high speed and exploded.

I say “crashed” because asteroids that approach Earth most commonly do so at around 20,000 miles/hr. Suppose you have a 10-mile commute that takes 20 minutes when traffic is reasonable. At 20,000 mph it would take just under 2 seconds. Ever stick a hand out of the car window at highway speed to feel the air resistance? It feels significant against your hand (try it again to remind yourself). Physics tells us that drag increases proportionally to the speed squared, and 20,000 mph is a little over 300 times faster than 65 mph. That means the drag experienced at asteroidal velocities is 300×300 or 90,000 times the drag you and your car feel at 65 mph. Just to put 90,000 times into perspective, if your hand experiences 1 lb. of drag when you stick it out the window at 65 mph, it would experience 90,000 lb. of drag were you to try commuting by asteroid. That is why drag destroys most asteroids in the air before they hit the ground, converting their energy of motion mostly into heat — in other words they explode. The Tunguska event could easily have destroyed a city, but luckily it exploded over a remote, forested area and killed mostly trees, several hundred square miles worth.

Part 2 (next time): Tunguska was just a fire cracker compared to what can happen.

References

Continue reading “Asteroid Apocalypse (part 1: Tunguska)” »