Apply scientific principles regarding thermal convection and gravitational movement of dense materials to predict the outcomes of continued development and movement of lithospheric plates from their growing margins at a divergent boundary (mid-ocean ridge) to their destructive margin at a convergent boundary (subduction zone).
Standard detail
GEO.ESS2.14
Depth 1Parent ID: 2A388DD3985A4906973671900AC15D54Standard set: Geology
Original statement
Quick facts
- Statement code
- GEO.ESS2.14
- List ID
- 14
- Standard ID
- 0080F0B76F0945FDA307696CB2404EB5
- Subject
- Science (2022-)
- Grades
- 09, 10, 11, 12
- Ancestor IDs
- 2A388DD3985A4906973671900AC15D54
- Source document
- Tennessee Academic Standards for Science
- License
- CC BY 4.0 US