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
Standard
Depth 1Parent ID: EE7A2622B5DD4FB8BC678E979A018FFAStandard set: Geology: Grades 9, 10, 11, 12
Original statement
Quick facts
- Statement code
- GEO.ESS2.14
- Standard ID
- 01B8591326154011AC95EE944E6C94F1
- ASN identifier
- S2773016
- Subject
- Science (2016-)
- Grades
- 09, 10, 11, 12
- Ancestor IDs
- EE7A2622B5DD4FB8BC678E979A018FFA
- Source document
- Tennessee Academic Standards: Geology (2016)
- License
- CC BY 3.0 US