A lot of events that produce markers for an impact are explained as asteroid airbursts. Asteroid airbursts are factual events which frequently occur.
One under reported property of airbursts is the inherent limits of their destructive power. An airburst is an asteroid which detonates before reaching the surface. The energy released by an airburst is dependent on the size, velocity, and composition of the object producing it.
An icy asteroid (comet) has low mass density and not much structural strength. Even with these limitations an icy asteroid can still impact if it is large enough or if it is moving fast enough. This would tend to limit the explosive yield of an airburst to (a guess) 5 to 10 megatons before it will always produce a surface crater.
For denser or stronger masses like rock and iron these numbers go down since these masses have a greater chance of reaching the ground and producing a visible crater. Airbursts therefore have upper limits on the energy that they can release before they will produce an impact crater.
If someone puts forth a scenario where a vast area >10,000 km^2 is affected by an airburst then they have blamed the wrong phenomenon.
The flare of energy (thermal energy released by a column of vaporized rock) produced by an interstellar impact is capable of affecting an area > 1,000,000 km^2. These impacts can leave behind flood basalts and impact structures which superficially resemble volcanic structures.
One of the features which can help determine whether an airburst is responsible for the damage in a particular area is the presence of an ash layer. Since the body which produced the airburst never reached the ground it can only produce a limited amount of ash. That ash would be the disintegrated mass of the asteroid along with any ash produced by surface fires such as forests. The chemistry of the ash would look like powdered asteroid mixed with organic ash.
In the case of an interstellar (or high velocity) impact the amount of ash located near the impact point could be much greater than 10 cm. The Impact point itself might be barren of ash since the outflow from the flare might blast it away. At some distance from the impact point a significant ash layer will be deposited. The chemistry of an interstellar impact ash layer is dependent upon the energy of the impact.
One under reported property of airbursts is the inherent limits of their destructive power. An airburst is an asteroid which detonates before reaching the surface. The energy released by an airburst is dependent on the size, velocity, and composition of the object producing it.
An icy asteroid (comet) has low mass density and not much structural strength. Even with these limitations an icy asteroid can still impact if it is large enough or if it is moving fast enough. This would tend to limit the explosive yield of an airburst to (a guess) 5 to 10 megatons before it will always produce a surface crater.
For denser or stronger masses like rock and iron these numbers go down since these masses have a greater chance of reaching the ground and producing a visible crater. Airbursts therefore have upper limits on the energy that they can release before they will produce an impact crater.
If someone puts forth a scenario where a vast area >10,000 km^2 is affected by an airburst then they have blamed the wrong phenomenon.
The flare of energy (thermal energy released by a column of vaporized rock) produced by an interstellar impact is capable of affecting an area > 1,000,000 km^2. These impacts can leave behind flood basalts and impact structures which superficially resemble volcanic structures.
One of the features which can help determine whether an airburst is responsible for the damage in a particular area is the presence of an ash layer. Since the body which produced the airburst never reached the ground it can only produce a limited amount of ash. That ash would be the disintegrated mass of the asteroid along with any ash produced by surface fires such as forests. The chemistry of the ash would look like powdered asteroid mixed with organic ash.
In the case of an interstellar (or high velocity) impact the amount of ash located near the impact point could be much greater than 10 cm. The Impact point itself might be barren of ash since the outflow from the flare might blast it away. At some distance from the impact point a significant ash layer will be deposited. The chemistry of an interstellar impact ash layer is dependent upon the energy of the impact.
(breaking this up into bite size pieces to compensate for my attention span)