Name: _ __________________________________
Lab: F ormation o f I gneous R ocks!
adapted f rom
a l ab e ntitled “ Igneous R ocks”
by M abry G aboardi o f t he F lorida S tate U niversity G K-‐12 p rogram.
Today w e a re g oing t o b e s tudying i gneous r ocks. W e a re g oing t o m ake t wo i gneous r ocks
and e xplore h ow t hey a re f ormed. T ake a l ook a t r ocks A -‐D i n y our b ox. ( A-‐Granite, B -‐
Rhyolite, C -‐Gabbro, D -‐Basalt) Y ou c an r emove t hese f our r ocks a nd p ut t hem o n y our d esk.
1. What o bservations c an y ou m ake a bout t hese r ocks?
2. What d o y ou t hink m akes t he c olor i n t hese r ocks?
3. Do y ou s ee c rystals i n a ll f our o f t he r ocks? W hat i deas d o y ou h ave a bout w hy y ou
can s ee c rystals w ell i n s ome b ut n ot i n o thers?
We a re g oing t o f ind o ut w hy. I h ave m elted m inerals t o m ake m agma. I a m g oing t o p ut t his
magma o n w ax p aper a nd I w ant y ou t o o bserve w hat h appens.
4. What d id y ou s ee?
This i s h ow i gneous r ocks a re f ormed! R emember w hat f orms i gneous r ocks f rom m agma?
Cooling! T he a mount o f t ime m agma h as t o c ool a ffects t he s ize o f t he c rystals.
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.
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