Rocks and Dates Geology Analysis

The Grand Canyon is the perfect place to learn about the real era of the Earth, because you can know the age of the rocks in the canyon. The rocks exposed at the Grand Canyon are really old, from 18.4 million years to 84 billion years (until 27 million years). (Beus and and Morales, 2003). The Grand Canyon is not so big on Earth but it is considered a young planet because it has been overwhelmed for over 6 million years. This makes the rock a fossil of the icy age in the canyon and makes it a new deposit of ambitious plan.

Appalachia geology dates back more than 480 million years ago. Looking at the rocks exposed in the Appalachian mountain range today, you can see the ocean bottom sedimentary rocks folded back and crushed in the opposite direction, volcanic rocks, and ancient seabed fragments of thin bands. The birth of the Appalachian mountains began for the first time with several mountain plate collisions and eventually to the construction centers near the Pangea, the Appalachian mountain range of the supercontinent and the adjacent Little Atlas (now located in Morocco) These mountains May have reached an altitude similar to the Alps or Rocky Mountains before being eroded.

Structural geology is the process leading to the formation of the geological structure and the study of the influence of these structures on the rock. Structural geology is a diverse range of sizes ranging from microscopic (eg early wrinkle traces after multiple deformation events) to large enough to spread to the Earth (eg the mid-ocean ridge) Includes structural features.

Geology describes the structure of the earth below the surface of the earth and the process of shaping it. It also provides tools to determine the relative and absolute ages of rocks found in specific locations and also explains the history of these rocks. By combining these tools geologists can record the geologic history of the entire earth and indicate the age of the earth. Geology provides the main evidence of plate tectonics, the history of life evolution, and the past climate of the Earth

Most geological studies relate to rock research, as rocks provide a majority record of the majority of the earth's geological history. There are three types of igneous rocks, sedimentary rocks and metamorphic rocks. The lock cycle shows the relationship between them (see figure). When rocks crystallize from lava (magma or lava), it is igneous rock. The rocks are weathered and eroded, then re-deposited and become sedimentary rocks. It can then transform into metamorphic rocks by heat and pressure. And we change the mineral content to form a unique fabric. In this way, a new magma is formed and the igneous rocks crystallize again.