Posted on May 26, 2023 (Updated on July 9, 2025)
The Role of Assumptions in Isotopic Radiometric Dating: An Earth Science Perspective
Geology & LandformRadiometric dating is a powerful tool used by scientists to determine the age of rocks and other geological materials. It is based on the decay of radioactive isotopes, which allows scientists to calculate the amount of time that has elapsed since the material was formed. However, radiometric dating relies heavily on a number of assumptions,
Posted on May 26, 2023 (Updated on July 9, 2025)
Uncovering the Secrets of Mud Crack Formation: A Stratigraphic Perspective
Geology & LandformIntroduction Mud cracks are a common feature in sedimentary rocks formed by the desiccation or drying of mud. These cracks can provide valuable information about the depositional environment and the history of the sediment. In this article we will explore the formation of mud cracks from a stratigraphic perspective. Formation of mud cracks Mud cracks
Posted on May 25, 2023 (Updated on July 10, 2025)
Exploring Facies and Petrography: A Guide to Processes and Depositional Environments
Geology & LandformIntroduction Facies and petrography are two important concepts in earth science that are often studied together. Facies refers to the physical characteristics of a rock, such as its grain size, texture, color, and mineral composition. Petrography is the study of the composition and structure of rocks and can be used to interpret the depositional environment
Posted on May 25, 2023 (Updated on July 9, 2025)
Exploring the Expansion of Earth’s Atmosphere in the Face of Gravity
Geology & LandformWhat is gravity and how does it affect the atmosphere? Gravity is a force of attraction between two objects that is proportional to the mass of each object. It is the force that holds the Earth and all of its components, including the atmosphere, in place. The atmosphere is made up of a number of
Posted on October 3, 2022 (Updated on July 22, 2025)
Why continents do not subduct
Geology & LandformWhy Continents Refuse to Take a Dive: The Subduction Story Ever wonder what makes our planet tick? Earth’s surface is like a giant jigsaw puzzle, with tectonic plates constantly bumping and grinding against each other. These plates, made of the crust and upper mantle, are the reason we have earthquakes, volcanoes, and those jaw-dropping mountain
Posted on September 27, 2022 (Updated on July 22, 2025)
What are the key elements defining the separation between Jurassic and Cretaceous?
Geology & LandformThe Jurassic-Cretaceous Boundary: When the World Started to Change So, picture this: it’s about 145 million years ago. Dinosaurs roam, the planet’s a bit warmer, and things are… well, shifting. We’re talking about the transition from the Jurassic to the Cretaceous period – a time that, while not as dramatic as the asteroid that wiped