HS-ESS2-1 | Earth's Surface Processes
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Clarification statement: Emphasis is on how the appearance of land features (such as mountains, valleys, and plateaus) and sea-floor features (such as trenches, ridges, and seamounts) are a result of both constructive processes (such as volcanism, tectonic uplift, and deposition) and destructive processes (such as weathering, subduction, and coastal erosion).
Assessment boundary: Assessment does not include recalling the details of the formation of specific geographic features of Earth’s surface.
Performance Level Descriptions
Every Regents exam question on HS-ESS2-1 is written to match one of the performance level descriptions (PLDs) below.
Resources
Examples and discussion of resources for the learning, teaching, and assessment of HS-ESS2-1.
Regents Exam Questions
Released New York State Regents exam questions that assess HS-ESS2-1 are listed here by exam and question cluster. Each link opens the question with its answer key.
NGSS Dimensions
Performance expectation HS-ESS2-1 was developed using the following elements from the NRC document A Framework for K-12 Science Education:
- Developing and using models: Develop a model based on evidence to illustrate the relationships between systems or between components of a system.
- Earth materials and systems: Earth’s systems, being dynamic and interacting, cause feedback effects that can increase or decrease the original changes.
- Plate tectonics and large-scale system interactions: Plate tectonics is the unifying theory that explains the past and current movements of the rocks at Earth’s surface and provides a framework for understanding its geologic history.
- Plate tectonics and large-scale system interactions: Plate movements are responsible for most continental and ocean-floor features and for the distribution of most rocks and minerals within Earth’s crust.
- Stability and change: Change and rates of change can be quantified and modeled over very short or very long periods of time. Some system changes are irreversible.