74 ^-1 XATURALIST IX THE GREAT LAKES REGIOX 



crystals while the others are minutely crystallized or more or 

 less glassv. the rock is called a porphyry. Plutonic rocks are 

 dense, since formed below the surface under great pressure. 

 Naturally there will be all intergrades between the plutonic and 

 the volcanic rocks, since the cooling lava may be in any one of 

 many situations from the deep-seated reservoir to the surface 

 flow. 



The molten material differs greatly in chemical composition 

 in different resiions of the earth and even two successive lava 

 flows from the same volcanic crater ma}' be quite unlike. If the 

 lava contains much silica it is an acid lava and gives rise to rocks 

 with many silicates and much free sihca or quartz. If, on the 

 other hand, it contains strong bases Hke calcium, magnesium, 

 and iron, it is a basic lava and the resulting rocks will contain 

 little free silica or quartz, though they will contain silicates of 

 the basic elements mentioned in the form of such minerals as 

 plagioclase, hornblende, augite, etc. The following scheme with 

 the brief characterizations that follow will aid in the determina- 

 tion of the igneous rocks of the Chicago area. Nothing hke a 

 complete key or complete descriptions can be given here, and 

 the interested student will secure some good hthology and 

 studv it in connection with the specimens of typical rocks found 

 in the museums. This scheme will help the observer to make a 

 start on interpreting the past history of a rock from its present 

 structure. Five rock groups are given in the order of their 

 increasing basidity so that, from left to right in the series, quartz 

 is becoming less abundant, the rocks are darkening in color and 

 increasing ill weight as the plagioclases replace the orthoclase, 

 and the augite, hornblende, and ohvine at the end largelv 

 replace even the plagioclase. 



Vertically in each column the members of any group are 

 named from distinctly volcanic rocks down to those that are 

 whollv plutonic. Going down the column, the members of the 

 famihes are less porous, less glassy, the component crystals are 

 constantlv larger, and the rocks increase in speciflc gravity. 



