Last Updated: January, 2019  
Igenous Rocks

Examples

Ultramafic

Mafic

Intermediate

Felsic

Intrisive

Dunite, BH250-41, BH250-80, BH25-112a

Gabbro, BH250-50, BH250-113, BH250-189

Diorite, BH250-90, BH250-164, BH250-176

Granite, BH250-49, BH250-92, BH250-96, BH250-152

 

Extrusive

Komatiitie, BH250-87, BH250-161

Basalt, BH250-60, BH250-82, BH250-124

Andsite, BH250-130, BH250-165

Rhyolite, BH250-72, BH250-89, BH250-95

 

Pyroclastic

--

Scoria

Pumice, Welded Tuffs ( BH250-130)

Obsidian , Tuff, BH250-108, BH250-169

 

Metamoprhic rocks

Examples
Foliated

Slate, BH250-123

Phyllite, BH250-88, BH250-126, BH250-157

Schist, BH250-52, BH250-110, BH250-159

Gneiss, BH250-111, BH250-115, BH250-118

                               From Mudd to Gneiss

Mudstone -->Shale --> [ Slate -->Phyllite -->Schist -->Gneiss]

 

Non-foliated

Quartzite, BH250-27, BH250-160, BH250-166

Marble, BH250-138

   
Sedimentary Rocks

Examples
Clastic

Mudstone

Shale, BH250-180

Sandstone, BH250-61, BH250-69, BH250-70

Conglomerate, BH250-141, BH250-153

Clastic sedimenary rocks are classfied in terms of grain size

Name of Particle

Size range

Loose sediment

Consolidated rocks

Boulder

>256 mm

Gravel

Conglomerate

Cobble

64-256mm

Gravel

Conglomerate

Pebble

2-64mm

Gravel

Conglomerate

Sand

1/16-2mm

Sand

Sandstone

Silt

1/256-1/16mm

Silt

Siltstone

Clay

<256mm

clay

Mudstone

 

To learn more about variation within the sand size (see attachements 1, 2)

 

 

Conglomerates and Breccias

A clastic rock made of particles larger than 2 mm in diameter is either a conglomerate or breccia. A conglomerate has rounded clasts while a breccia has angular clasts.

Chemical

Limestone, BH250-109, BH250-122

Dolostone, BH250-155, BH250-156

Oolite, BH250-179

   

 

 

Chemical Composition of Common Igneous Rocks

 

Plate Tectonics and Rock Types