Lab: Formation Of Igneous Rocks Page 2

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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
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