A tale set in stone
10 Rock Solid Facts About Geology To Rock Your World
Published on November 5, 2024
Credit: NEOM
Underneath a (mostly) humble appearance, rocks hold within them fascinating stories of our planet's origins. From the depths of the Earth to the surface, each rock has its own tale to tell. Luckily, you don’t need to become a geologist to learn a bit more about the origins of the rocks and minerals that make up our planet. Whether you are an aspiring rock hound or a science enthusiast, you will surely find these 10 intriguing facts about rocks and geology fascinating!
Oldest Rock on Earth
Credit: Daria Volkova
The oldest rock of terrestrial origin was found in Western Australia and dates back a staggering 4.4 billion years. Known as the Jack Hills zircon, this ancient rock offers a glimpse into the Earth's infancy, having endured eons of geological turmoil virtually unchanged. However, it’s far from being the oldest rock found on Earth, as many meteorites can be much older. In fact, the oldest rocks found so far are Murchison meteorite particles, determined to be 7 billion years old —older than our planet, even older than the Sun!
Rock Cycle
Credit: Oliver Paaske
Nothing is permanent on our planet, not even rocks! The rock cycle is a fundamental concept in geology, illustrating how rocks transform from one type to another over time through processes like weathering, erosion, deposition, and lithification. It's a dynamic process that shapes the Earth's surface, and it’s driven by some of its most fundamental forces, like plate tectonics, erosion, and the water cycle.
Fossils in Rocks
Credit: Wes Warren
Rocks aren't just stone; they're time capsules. Fossils embedded within sedimentary rock layers provide invaluable clues about past life forms and environments, helping scientists reconstruct the Earth's ancient ecosystems. Fossils present themselves in many different forms and shapes, and examples include petrified bones, shells, imprints of animals or microbes, organisms preserved in amber, hair, and even DNA remnants.
Petrified Forests
Credit: Caleb Jack
Wood can become a fossil too, given the right conditions —and a boatload of time! As different minerals replace the original materials present in wood, taking their shape, even an entire tree can be transformed into stone over millions of years. Petrified forests, like Arizona's Petrified Forest National Park, offer a glimpse into prehistoric landscapes, providing invaluable insights into ancient climates and ecosystems
Rock Strata
Credit: Nick Fewings
What looks like a rock sandwich —layer upon layer of different colored and textured rocks— you have likely gazed into Earth’s deep past without realizing it. A common sight on heavily eroded rock surfaces (like canyons), rock strata reveal the sequential deposition of sediment over time.
While common sense tells us that older layers are found deeper, while younger layers must be on top, this is not always the case, as many processes can alter the shape of the depositions. By studying these layers, geologists can unravel the Earth's history, identifying different periods of geological activity.
Mineral Formation
Credit: Irina Iacob
Minerals should not be confused with rocks, although they are closely related. In fact, minerals are the building blocks of rocks. These peculiar structures form through various processes such as crystallization from magma, precipitation from solution, or metamorphism under high pressure and temperature. Each mineral has its own unique properties and characteristics. Common examples are quartz, halite (also known as rock salt), and diamonds.
Unexpected Mineral
Credit: Jan Kopřiva
Ice, a substance seemingly ephemeral and transient, holds a surprising geological distinction —it is technically a mineral. According to the International Mineralogical Association, a mineral is defined as a naturally occurring inorganic solid with a definite chemical composition and an ordered atomic arrangement. Remarkably, ice meets all these criteria. Bet you won’t look at the ice on your drink the same after this!
Birth of Mountains
Credit: Pascal Debrunner
Mountains, Earth's sleeping giants, are actually more awake than we realize. Born from the collision of tectonic plates or from explosive and violent processes inside our planet, these massive landforms are created as the layers of rock are pushed upward, becoming towering peaks that shape landscapes and influence climates. Although most mountains take millions of years to form, in some cases volcanic mountains can seem to appear from nowhere over a few years!
Geological Time Scale
Credit: Jamie Hagan
The geological time scale divides Earth's history into distinct periods, epochs, and eras based on significant geological and biological events. Beginning around 4.5 billion years, with the formation of planet Earth, it extends up to current times, providing a comprehensive framework for understanding the evolution of our planet. Currently, we live in the Cenozoic Era, which covers the last 66 million years, and it is characterized by the dominance of mammals, birds, and flowering plants.
Rock Erosion
Credit: Jeremy Gallman
Erosion is a natural process that wears away rock and soil, sculpting landscapes over millennia. Factors such as water, wind, ice, and gravity play a role in shaping the Earth's surface, from towering cliffs to winding canyons. While erosion is always a natural process, human activity can affect the rate at which it occurs. In the Appalachian Mountains, intensive farming practices have caused the rate of local erosion to speed up to 100 times the natural rate, disrupting ecosystems and creating all sorts of problems for the local population.