Plate tectonics is the scientific theory that describes the large-scale movements of Earth'slithosphere. The lithosphere is divided into several large and small tectonic plates that float on the semi-fluid asthenosphere beneath them. These plates are in constant motion, which causes various geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Key Concepts
Tectonic Plates: The Earth'slithosphere is divided into several major and minor tectonic plates, including the Pacific Plate, North American Plate, Eurasian Plate, and many others. These plates are not stationary but instead move in relation to each other.
Plate Boundaries: The edges of tectonic plates, known as plate boundaries, are the primary sites of geological activity. There are three main types of plate boundaries: divergent boundaries (where plates move apart), convergent boundaries (where plates move together), and transform boundaries (where plates slide past each other).
Geological Features: Plate tectonics is responsible for a variety of geological features, including mountain ranges (formed at convergent boundaries), oceanic ridges (formed at divergent boundaries), and deep ocean trenches (formed at convergent boundaries).
Continental Drift: The theory of plate tectonics also explains the concept of continental drift, which suggests that continents have moved and are still moving slowly across Earth's surface due to the movement of tectonic plates.
Study Guide
Here are some key points to focus on when studying plate tectonics:
Identify and describe the major tectonic plates and their locations on Earth's surface.
All organisms have structures and systems with separate functions. Students can:
Develop and communicate an evidence-based scientific explanation of the role of different organs or structures that are important for an organism's survival - in both plants and animals