So, if you seek the center of the earth, skip Iceland. Go to the Zagros. Stand at the edge of the steaming crack. Listen to the roar of compressed air. And remember: Do you have a story about geothermal anomalies in your region? Contact the author via the Kurdish Geographical Society. Do not attempt to descend into any active geothermal vent. You will not find dinosaurs. You will find your own cremation.
In August 1972, a British geologist named —obsessed with Verne—convinced a Kurdish guide, Mamo Zirki , to lead him to the "Earth’s Crack" near the Sirwan River (Diyala).
For centuries, Kurdish shepherds avoided a specific valley near the massif (Agirî in Kurdish). They called it "Xetîka Bin erdê" – The Earth’s Crack. During winter blizzards, this valley remained snow-free, steaming like a teakettle. They believed that if you fell into that crack, you would not die from a fall, but would be cooked alive before you hit the bottom. Hence, the "Kurdish Hot" descent. Local Proverb: "The road to the center is cold in Iceland, but in the land of the Medes, the devil stokes the furnace." Part 2: The Geology – A Natural Pressure Cooker Forget the gentle lava tubes of Hawaii. The Kurdish Hot descent is characterized by a rare phenomenon: Geothermal Supercritical Fluids . journey to the center of the earth kurdish hot
By Roj Hadrut, Exploratory Geographer
It tells us that beneath the olive groves and ancient citadels of Kurdistan, the planet is alive, furious, and running a fever of 400°C. The "Kurdish Hot" is not a myth. It is a scientific fact waiting to kill any explorer foolish enough to believe Verne’s fiction. So, if you seek the center of the earth, skip Iceland
This article explores the reality, the mythology, and the terrifying science behind the "Journey to the Center of the Earth" as viewed through Kurdish folklore and modern geothermal surveys. To understand the keyword, we must break it down. Unlike Verne’s temperate descent, the Kurdish version is inherently hot —thermally and politically.
In 2018, a joint team of Turkish and Iranian geologists (working despite border tensions) drilled a test well 3.2 km deep in the Hakkâri region. Their sensors melted. They recorded a —three times the global average. Listen to the roar of compressed air
The Zagros fold-thrust belt is one of the most tectonically active zones on Earth. Here, the Arabian Plate is crashing into the Eurasian Plate at 2.5 cm per year. This collision generates friction so intense that subsurface temperatures reach at depths of just 1,000 meters—shallower than almost anywhere else in the world.