5. Do y ou t hink t he c rystals i n t he r ock w ould b e b igger o r s maller i f t his m agma
cooled a t a h igher t emperature? W ould t hey b e b igger o r s maller i f c ooled a t a l ower
temperature?
Create a H ypothesis:
How w ill y ou t est t his H ypothesis? W rite o ut y our e xperimental p lan:
Carry o ut y our e xperiment
1. What d id y ou o bserve t his t ime?
2. How d id y our t est a ffect t he c rystallization o f t he m agma?
3. How d oes t he m agma w e c ooled a t r oom t emperature c ompare t o y our c ooled
magma?
4. Which m agma h as l arger c rystals, o ne t hat c ools q uickly o r o ne t hat c ools s lowly?
Why d o y ou t hink t his i s?
SCWIBLES is an NSF-GK-12 project, #DGE-0947923,
Rock Types and Formation
a partnership between the University of California, Santa Cruz,
Igneous Lab
and the Pájaro Valley Unified School District.
page 2 of 3
For more information, see: