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.
Reference Tables
Relevant reference tables:
- Generalized Surface Bedrock Geology of New York State
- Geographic Province and Landscape Regions of New York State
- Generalized Cross Section Model of Earth's Surface and Interior
Assessment
What assessment of HS-ESS2-1 might look like on a NY state exam.
Performance Level Descriptions
PLDs communicate the knowledge and skills expected of students to demonstrate proficiency in each Learning Standard. NYS assessments classify student performance into one of five levels.
Vocabulary
Terms from the Earth & Space Science Glossary that come from this standard or from the released exam questions that assess it.
- coastal erosion
- constructive processes
- continental features
- crust
- deposition
- destructive processes
- Earth
- Earth materials
- Earth’s surface
- Earth’s systems
- erosion
- feedback
- geologic history
- internal and surface processes
- land features
- minerals
- model
- mountain
- ocean
- ocean-floor features
- plate movements
- plate tectonics
- plateaus
- ridges
- sea-floor features
- seamounts
- spatial scales
- subduction
- surface processes
- tectonic uplift
- temporal scales
- trenches
- unifying theory
- valleys
- volcanism
- weathering
- accretion – Sample 2024
- active volcanoes – June 2025
- archipelago – Sample 2024
- asteroids – Sample 2024
- atmosphere – Jan 2026
- banded iron formations – Jan 2026
- barrier sand bar – Sample 2024
- basin – Aug 2026, Aug 2025, Sample 2024
- bedrock – June 2025
- black smokers – Jan 2026
- butte – Sample 2024
- canyon – Sample 2024
- chemical weathering – June 2026
- climate zone – Aug 2025
- collision – Sample 2024
- composition – Sample 2024
- continental crust – Aug 2025, June 2025
- continental drift – Sample 2024
- continental shelf – June 2026
- crystallization – June 2026
- delta – Sample 2024
- Earth’s interior – Sample 2024
- earthquakes – June 2025
- elements – June 2026
- Equator – Aug 2026, Aug 2025
- eurypterid – Aug 2025
- extinct volcanoes – June 2025
- fault – Aug 2025
- felsic – June 2026
- flood basalts – Sample 2024
- flood plain – Sample 2024
- fossil forest – Aug 2025
- fossils – Aug 2025, Sample 2024
- fresh water – Aug 2025
- geologic epoch – Aug 2026
- geologic processes – Aug 2025, Sample 2024
- ghost forest – June 2025
- giant impact hypothesis – Sample 2024
- granitic plutons – Aug 2025
- impact craters – June 2025, Sample 2024
- inlet – Sample 2024
- inner planets – Sample 2024
- intrusive igneous rock – Aug 2025
- iron – June 2026, Jan 2026
- island arc – June 2026
- island chain – Aug 2026, June 2025
- land plants – Aug 2025
- lava – Sample 2024
- lava flows – Sample 2024
- lithification – June 2026
- lunar crust – Sample 2024
- lunar highlands – Sample 2024
- mafic – June 2026
- magma – June 2025
- mantle – June 2025, Sample 2024
- mantle convection – Aug 2026
- mare – Sample 2024
- mechanical weathering – June 2026
- mesa – Sample 2024
- metamorphism – Aug 2025
- meteorites – June 2025
- meteorologist – Sample 2024
- molten rock – June 2025, Sample 2024
- moon – Sample 2024
- moon formation – Sample 2024
- moraine – Sample 2024
- motion – June 2026
- mountain range – Sample 2024
- Northern Hemisphere – Aug 2025
- ocean floor – Aug 2026
- oceanic crust – Aug 2025
- paleomap – Aug 2025
- peninsula – June 2025, Sample 2024
- planetary body – Sample 2024
- plate interaction – June 2026
- plate tectonic movement – June 2025
- precipitate – June 2026
- proto-Earth – Sample 2024
- quarry – Aug 2025
- recrystallization – June 2026
- river – Sample 2024
- river valley – Sample 2024
- sea level – Aug 2026, Jan 2026, June 2025
- sea level rise – June 2025
- sea-floor spreading – June 2025
- sediment – Jan 2026, Aug 2025, Sample 2024
- shoreline – June 2025
- soil – Jan 2026
- stratosphere – June 2026
- subduction zone – Aug 2025
- subsidence – June 2026, June 2025
- surface trench – Sample 2024
- tributary – Sample 2024
- tsunami deposits – Jan 2026
- volcanic activity – June 2025
- volcanic arc – June 2025
- volcanic eruptions – June 2026, June 2025
- volcano – June 2026, June 2025, Sample 2024
- waterfall – Sample 2024
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.