Chapter 1: The Context of Extinction

Long before dinosaurs vanished from Earth, the planet faced significant geological upheaval. The Deccan Traps in India, a massive expanse of volcanic flows covering 500,000 square kilometers, were formed several hundred thousand years prior to the extinction event. This serves as a reminder that Earth is an ever-evolving planet.

What if the extinction wasn’t solely the result of a meteor impact? If we consider a correlation between global warming and the demise of the dinosaurs, alternative explanations might emerge.

Could a cosmic lightning strike, rather than a comet, have generated Iridium from terrestrial materials, covering the planet in it? What if this Iridium was not delivered from space, but produced on Earth itself through interstellar lightning, ultimately poisoning the atmosphere and leading to the extinction of many species?

Chapter 2: The Warming Planet

There are numerous potential reasons for the warming of our planet. This article presents an alternative theory regarding the extinction of dinosaurs. If you find this concept implausible, I hope you still find the discussion enjoyable.

The timeline of interest spans from 70 to 65 million years ago, during which the Indian subcontinent was migrating toward the equator as part of tectonic shifts. The arrangement of landmasses was quite different from today.

Applying principles of friction and electromagnetism, we can speculate that the positioning of this continent along the Earth's fastest-spinning section added drag to the system. This drag could translate into heat, contributing to the planet's warming.

Naturally, this added heat might seem trivial, yet over one million years, even a slight increase in temperature could accumulate significantly, resulting in continuous warming without a clear upper limit.

In addition to heat, an electromagnetic charge would have built up during this process. This scenario suggests that the planet became increasingly charged.

The first video titled "Iridium and the Dinosaurs" explores the relationship between Iridium and the extinction of dinosaurs, discussing various theories surrounding this phenomenon.

Chapter 3: The Role of Electromagnetism

While planets orbit the Sun independently, there are still interactions among them. Jupiter, with its strong magnetosphere, protects against solar winds extending nearly 3 million kilometers outward. This immense magnetic field dwarfs Earth's, being about 20,000 times more powerful.

What would happen if Earth had a more potent magnetosphere around 66 million years ago? How far into space could this magnetic field have reached? Could this increase in electromagnetic charge have disrupted a long-standing balance, resulting in an enormous discharge?

The hypothesis proposes that Earth's rising temperatures were influenced by an increase in electromagnetic drag at the equator, with the Indian subcontinent contributing to this effect.

As the electromagnetic balance within the inner solar system became unstable, Earth might have received a significant jolt—perhaps directly from the Sun or, alternatively, from Jupiter.

Given that Jupiter is four times more distant than the Sun, it’s plausible that electromagnetic interactions could have allowed for a more direct connection with Jupiter than with the Sun. The potential for a major discharge could have been facilitated by Mars and the asteroid belt, acting as intermediaries.

The second video, "The Day the Mesozoic Died: The Asteroid That Killed the Dinosaurs," delves into the asteroid impact theory, providing insights into its effects on Earth’s environment.

Chapter 4: The Iridium Mystery

Iridium is found globally at the Cretaceous-Tertiary boundary. This theory suggests that a colossal lightning strike hit Earth in a tropical region, possibly the closest point to Jupiter or the Sun.

During this immense lightning event, especially in metal-rich areas, Iridium would have been released from the crust and potentially created from other metals. Scientifically, Iridium typically forms in neutral conditions, not in charged environments, indicating that only a brief moment of neutrality—perhaps a few days—would allow its creation.

This Iridium-laden atmosphere would have become toxic, leading to the demise of the dinosaurs. Smaller animals might have survived by seeking shelter, but the size and needs of dinosaurs would have made survival impossible in such conditions. The distinctive layer rich in Iridium, suspended in the air, would have suffocated these large creatures.

In conclusion, this presents an alternative theory for the extinction of the dinosaurs. It is likely to be met with skepticism or ignored in the current scientific discourse.

I hope you found this theory entertaining and perhaps even a cautionary tale about the balance of our planet, especially in light of human actions that could disrupt this equilibrium. The heating of our planet, coupled with rising electromagnetic forces, poses significant risks.

This article is part of the "What if..." series, exploring intriguing hypotheses about our world.

Here is another article from the series: