Music drives our cars, buses, and planes, powers our electricity, and allows us to cook our food and heat our water. Most of today's energy needs are met by fossil fuels like coal, oil, and gas. These unique, high-energy fuels are non-renewable resources that took millions of years to form. About two billion years ago, marine organisms such as algae and microscopic animals and plants died and settled on the ocean floor beneath other sediments. In the absence of oxygen, these fossils changed into a substance called kerogen under heat and pressure. Kerogen gradually changes into oil or gas, and this process usually takes at least a million years. At the molecular level, oil and gas are hydrocarbons made up of hydrogen and carbon atoms. The constant pressure and movement of the Earth's crust squeeze oil and gas through the pores or spaces between rocks. Some oil and gas reach the Earth's surface and seep out naturally onto land or water. However, they are often trapped beneath the surface by impermeable layers or rock structures like faults and folds within the crust. Oil or gas deposits build up and form reservoirs, which are like vast sponges filled with oil and gas. These reservoirs can be as large as a city. To find oil and gas deposits, geologists use a number of different survey techniques including seismic surveys, gravitational surveys, and geological mapping. Seismic surveys use reflected sound waves to produce a 3D view of the Earth's interior. New technologies such as four-dimensional projections and sophisticated graphic renderings of rock structures are improving the way we find conventional oil and gas deposits as well as unconventional oil and gas deposits. In a world with limited energy resources, people are looking for more efficient ways of tapping into unconventional oil and gas or alternative and...