Contact Metamorphism:Occurs when rocks are in contact with magma or lava, leading to changes in the surrounding rocks due to the heat from the molten material.
Foliated Rocks: Display a layered or banded appearance due to the alignment of mineralgrains, examples include schist and gneiss.
Non-Foliated Rocks: Lack a layered structure and are composed of minerals that have recrystallized without preferred alignment, examples include marble and quartzite.
Study Guide
To understand metamorphism, it is essential to study the following concepts:
Additionally, it's important to familiarize yourself with the various rock samples, geological maps, and diagrams related to metamorphic processes.
Practice identifying different types of metamorphic rocks and interpreting the geological history and conditions that led to their formation.
Understanding the principles of petrology and mineralogy will also be beneficial for comprehending the intricate changes that occur during metamorphism.
Lastly, stay updated with current research and advancements in the field of metamorphic geology to gain a comprehensive understanding of this dynamic process.
From Molecules to Organisms: Structures and Processes
Students who demonstrate understanding can:
Develop and use a model to illustrate the hierarchical organization of interacting systems that provide specific functions within multicellular organisms.
Plan and conduct an investigation to provide evidence that feedback mechanisms maintain homeostasis.