Digging of earth deep inside is a common practice for many applications like, ore & oil extraction from deep inside the earth but scientists and engineers are also interested to dig very deep inside the earth to know about the characteristics of inner earth. During the study on variation of gravity (gravitational force involving Earth) and its one of the important consequence i.e., acceleration due to gravity (g) in school and college, there was always a curiosity to learn more about its variation deep inside the earth to its centre. According to the mathematical formula giving the variation of acceleration due to gravity along the depth of the earth [g/ = g (1-d/R)], where ‘g’ is the value (maximum) at the surface of earth, ‘d’ is the depth and ‘R’ is the radius of earth. From the formula to best of approximation, acceleration due to gravity will reduce to zero at the centre of earth. Sometimes, it comes to mind as a general reader whether it is possible to dig a deep hole into centre of earth and verify and experience the behavior of mass bodies falling through the hole.
A 100-year-old copper mine in the mountains near Salt Lake City, Utah hosts a pit that extends three quarters of a mile deep and spans 2.5 miles. At 215 meters, the Kimberley Diamond Mine in South Africa is one of the largest holes in the world dug by human hands. But extracting resources like fossil fuels and metals are not only the reasons that humans dig deep into the Earth. Human also dig deep holes in earth, of course, for science. Experiments looking for neutrinos, nearly massless subatomic particles that get produced in explosive astronomical events like exploding stars and gamma-ray bursts, have to put their detectors far below the Earth’s surface. These depths are needed to pick out the faint signal of the neutrinos from the stronger background radiation at the Earth’s surface. Drilling the Kola Superdeep Borehole was, for the most part, purely science-driven. Soviet scientists wanted to learn more about our planet’s outermost layer, called the crust, to understand how that crust has formed and how it evolved. Science was the goal, but everyone wanted bragging rights for winning the race to the center of the Earth.
There are a number of portals in the internet giving details of sites and status of various digging projects to the center of the earth.
Although it didn’t reach the planned depth, the Kola Superdeep Borehole was still an impressive feat of engineering. New drill technology had to be developed to make the project possible. That includes a drill bit at the end of the shaft that rotated separately and a custom drill bit that pumped a type of lubricant, known as pressurized drilling mud down, to the drill site. At 4.4 miles down (~7 kilometers), scientists found two-billion-year-old fossils from single-celled marine organisms. Scientists were also surprised by what they found in that hole. They obviously learned that our temperature map of the Earth’s interior had to be updated since they hit hotter temperatures earlier than expected. At 4.4 miles down (~7 kilometers), they found two-billion-year-old fossils from single-celled marine organisms. And as deep as they dug, they found liquid water, which is far deeper than we had previously thought that water could exist. The scientists think that water may have been squeezed out of the rock crystals due to the incredibly high pressures.
We know surprisingly little about the interior of our planet given that it is just below our feet. The Earth’s outermost layer, the crust, is about 25 miles thick below the land. That means the next layer, the mantle, doesn’t even start until nearly 25 miles (40 kilometers) below the surface and continues for another 1800 miles. That means that despite the impressive nature of the Kola Superdeep Borehole, it still only penetrates about a third of the Earth’s crust and 0.2% of the entire distance to the center of the Earth. Being able to probe deeper toward the mantle will help us understand why earthquakes happen, how our planet formed, and how life may have originated on Earth. The next big push for science is to make it to the mantle. There, scientists expect to encounter temperatures of 250 degrees Celsius or about 500 degrees Fahrenheit. The mantle holds the imprint of the geological record of the Earth’s history, much like how we can trace the history of organisms on the Earth’s surface through the layers of rock we see there. Being able to probe deeper toward the mantle will help us understand why earthquakes happen, how our planet formed, and how life may have originated on Earth.