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\par \hich\af5\dbch\af4\loch\f5 ** v=veins, am=amydules, p=pebbles, ab=altered basalt
\par \hich\af5\dbch\af4\loch\f5 ***Quartz occurs in many distinct forms: agate (banded or mossy amydaloidal fillings), carnelian (clear, red chalcedony) , jasper (opaque red yellow, gr\hich\af5\dbch\af4\loch\f5 
een or brown), amethyst (purple crystals) or rock crystal (colorless crystals) are all found on Isle Royale.  Smoky quartz is also present in many beach pebbles.
\par 
\par \hich\af5\dbch\af4\loch\f5 Isle Royale Minerals
\par 
\par \hich\af5\dbch\af4\loch\f5 The rocks of Isle Royale are mainly massive, dark colored basalt lavas \hich\af5\dbch\af4\loch\f5 which are made up primarily of feldspar and pyroxene with lesser amounts of other minerals.  The sandstone of SW Isle Royale 
\hich\af5\dbch\af4\loch\f5 contains mainy\hich\af5\dbch\af4\loch\f5  \hich\af5\dbch\af4\loch\f5 feldspar, quartz and rock fragments. When the lava flows cooled down\hich\af5\dbch\af4\loch\f5  }{\fs24 \hich\af5\dbch\af4\loch\f5 about one billion years ago}
{\fs24 \hich\af5\dbch\af4\loch\f5 , gases separated within the lava flow and gas bu\hich\af5\dbch\af4\loch\f5 bbles preferentially rose to the top of the lava flows and were frozen in.  After the solidification of the lava\hich\af5\dbch\af4\loch\f5 
 these gas bubbles - now empty voids - were filled by hot fluids that circulated throughout the rocks and depo\hich\af5\dbch\af4\loch\f5 
sited new minerals in these empty bubbles. The filled bubbles are now called amygdules. The temperature of the hot fluid determined the mineral assemblage or group of minerals. Zeolites, for example, are deposited at lower temperature than prehnite or pum
\hich\af5\dbch\af4\loch\f5 p\hich\af5\dbch\af4\loch\f5 
ellyite. The most beautiful and distinctive minerals of the park specimens come from these amygdules in the basalt since the basalt provides all the necessary elements for the formation of these minerals but also from veins (mineral-filled cracks) which c
\hich\af5\dbch\af4\loch\f5 u\hich\af5\dbch\af4\loch\f5 t across the sandstone and lava outcrops. 
\par 
\par \hich\af5\dbch\af4\loch\f5 The minerals are part of one of the most famous mineral districts of the world, the Lake Superior Copper District, which was the first great metal mining district in North America.  Isle Royale is most prominentl
\hich\af5\dbch\af4\loch\f5 y known for its greenstone,  a beautiful nodular compact form of pumpellyite that is Michigan state gemstone. The distinctive minerals are listed in the table, with some of their characteristics a\hich\af5\dbch\af4\loch\f5 
s well as \hich\af5\dbch\af4\loch\f5 some hints and tips to identify them.
\par 
\par 
\par \hich\af5\dbch\af4\loch\f5 Where to look for\hich\af5\dbch\af4\loch\f5  minerals:
\par \hich\af5\dbch\af4\loch\f5 
If you want to find minerals at Isle Royale, you should walk the coastlines, especially those that are well wavewashed.  The waves expose the minerals and pebbles  and various minerals can be found on adjacent beaches.   Using a canoe or small b
\hich\af5\dbch\af4\loch\f5 oat, watershoes and plenty of time, walk the shore and watch for veins and amygdaloids (=the amygdaloidal flow top of a lava flow).  Observe the interiors of basalt flows where vesicle cylinders, peg\-
matites, joints and veins may expose these distinctive \hich\af5\dbch\af4\loch\f5 m\hich\af5\dbch\af4\loch\f5 inerals (see diagram).
\par 
\par \hich\af5\dbch\af4\loch\f5 For more Information:
\par \hich\af5\dbch\af4\loch\f5 For more information about the geology of Isle Royale, consult the book by Huber (1983, The Geologic Story of Isle Royale National Park, USGS Bull 1309, 66pp) which is available in the park.   The minerals of t
\hich\af5\dbch\af4\loch\f5 
his area are exhibited all over the world and you surley can find them in your local museum.  The largest and most extensive exhibit of minerals of the Keweenaw and Isle Royale can be seen at the AE Seaman Mineralogical Museum in Houghton, Michigan, near 
\hich\af5\dbch\af4\loch\f5 t\hich\af5\dbch\af4\loch\f5 he IRNP headquarters.  The headquarters itself has a small mineral display.  A new, illustrated book about the Minerals of Michigan by EW Heinrich is in press and will be available in 2001.
\par 
\par 
\par \hich\af5\dbch\af4\loch\f5 Table 1: Distinctive Minerals of Isle Royale
\par 
\par \hich\af5\dbch\af4\loch\f5 The individual min\hich\af5\dbch\af4\loch\f5 
eral is sometimes difficult to identity, even for experts, but certain groups of minerals can be distinguished very easily. All you need is your finger nail. The phyllosilicates chlorite, corrensite and saponite are all of green color and very soft minera
\hich\af5\dbch\af4\loch\f5 l\hich\af5\dbch\af4\loch\f5 
s. You can easily scratch them with your finger nail. The other green minerals as pumpellyite or prehnite are much harder and you will not be able to scratch them with your fingernail. In fact, in pebbles along the shore they stick out
\hich\af5\dbch\af4\loch\f5 ,\hich\af5\dbch\af4\loch\f5  since they are not a\hich\af5\dbch\af4\loch\f5 s easily eroded as the surrounding rock. \hich\af5\dbch\af4\loch\f5 t\hich\af5\dbch\af4\loch\f5 
he pink unusual color of  prehnite of Isle Royale often is the result of very tiny inclusions of native copper which makes it similar to the zeolite thomsonite.The zeolite family is in general difficult to identify.\hich\af5\dbch\af4\loch\f5 
 But the zeolite laumontite can easily b\hich\af5\dbch\af4\loch\f5 e recognized. It is of white or\hich\af5\dbch\af4\loch\f5  pink color and if you touch it with your finger nail it will split up i\hich\af5\dbch\af4\loch\f5 nto\hich\af5\dbch\af4\loch\f5 
 small fibers. 
\par \page 
\par }\pard\plain \widctlpar\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 
\par }\pard\plain \s16\qc\nowidctlpar\adjustright \f4\cgrid {\b\cf1 Table 1: Distinctive Minerals of Isle Royale}{\cf1 
\par }\pard\plain \widctlpar\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 
\par }\trowd \clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrdb\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx1612\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrdb\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx6292
\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrdb\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx7544\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrdb\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx9776
\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrdb\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx12368\pard\plain \s17\qc\nowidctlpar\intbl\adjustright \f4\cgrid {\b\cf1 Mineral *}{\cf1 \cell }\pard\plain 
\s18\qc\nowidctlpar\intbl\adjustright \f4\cgrid {\b\cf1 Chemical Formula}{\cf1 \cell }{\b\cf1 Hardness}{\cf1 \cell }{\b\cf1 Color}{\cf1 \cell }{\b\cf1 Occurrence & Notes**}{\cf1 \cell }\pard\plain \widctlpar\intbl\adjustright 
\loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\trowd \clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx1612\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 
\clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx6292\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx7544\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr
\brdrs\brdrw15 \cltxlrtb \cellx9776\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx12368\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Barite     }{\i\cf1 c}{\cf1 \cell 
BaSO}{\cf1\sub 4}{\cf1  \cell 3-3.5\cell White\cell }{\i\cf1 v}{\cf1 \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Calcite    }{\i\cf1 a}{\cf1 
\cell CaCO}{\cf1\sub 3}{\cf1  \cell 3\cell colorless,white,pink\cell }{\i\cf1 v,am}{\cf1 \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 
Chlorite   }{\i\cf1 a}{\cf1 \cell (Mg,Fe)}{\cf1\sub 5}{\cf1 Al}{\cf1\sub 2}{\cf1 Si}{\cf1\sub 3}{\cf1 O}{\cf1\sub 10}{\cf1 (OH)}{\cf1\sub 8}{\cf1 \cell 2-2.5\cell olive-dk green-black\cell }{\i\cf1 am, ab}{\cf1 \cell }\pard\plain 
\widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Copper    }{\i\cf1  r}{\cf1 \cell Cu\cell 2.5-3\cell copper, green-black\-coatings\cell }{\i\cf1 v,am}{\cf1 \cell 
}\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Corrensite  }{\i\cf1 a}{\cf1 \cell (Mg,Fe,Al)}{\cf1\sub 9}{\cf1 (Si,Al)}{\cf1\sub 8}{\cf1 O}{\cf1\sub 20}
{\cf1 (OH)}{\cf1\sub 10}{\cf1 \u8721\'b7n(H}{\cf1\sub 2}{\cf1 O) \cell 1-2\cell Dk green to black\cell }{\i\cf1 ab,}{\cf1  \u236\'93swelling chlorite\u238\'94\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row 
}\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Datolite   }{\i\cf1  r}{\cf1 \cell  CaBSiO}{\cf1\sub 4}{\cf1 (OH) \cell 5.5\cell white or pink, vari\-ous\cell }{\i\cf1 v, am}{\cf1   porcelaineous, opaque\cell }\pard\plain 
\widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Epidote     }{\i\cf1 c}{\cf1 \cell Ca}{\cf1\sub 2}{\cf1 (Fe,Al)Al}{\cf1\sub 2}{\cf1 (SiO}{\cf1\sub 4}{\cf1 )(Si}{
\cf1\sub 2}{\cf1 O}{\cf1\sub 7}{\cf1 )O(OH) \cell 7\cell pistachio green\cell }{\i\cf1 am, ab}{\cf1   crystalline, amygdules\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain 
\s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Laumontite  }{\i\cf1 c}{\cf1 \cell CaAl}{\cf1\sub 2}{\cf1 Si}{\cf1\sub 4}{\cf1 O}{\cf1\sub 12}{\cf1 \u8721\'b74(H}{\cf1\sub 2}{\cf1 O) \cell 3.5-4\cell wh-brown, gray, pink\cell }{\i\cf1 am}{\cf1 
  bladed aggregates, weathers powdery white\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Microcline   }{\i\cf1 r}{\cf1 \cell KAlSi}{\cf1\sub 3}{
\cf1 O}{\cf1\sub 8}{\cf1  \cell 6\cell flesh-pink\cell }{\i\cf1 v, am}{\cf1 \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Mesolite     }{\i\cf1 
vr}{\cf1 \cell Na}{\cf1\sub 2}{\cf1 Ca}{\cf1\sub 2}{\cf1 Al}{\cf1\sub 6}{\cf1 Si}{\cf1\sub 9}{\cf1 O}{\cf1\sub 30}{\cf1 \u8721\'b78(H2O) \cell 5\cell white-grey-yellow\cell }{\i\cf1 am }{\cf1  needly\cell }\pard\plain \widctlpar\intbl\adjustright 
\loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Natrolite     }{\i\cf1 vr}{\cf1 \cell Na}{\cf1\sub 2}{\cf1 Al}{\cf1\sub 2}{\cf1 Si}{\cf1\sub 3}{\cf1 O}{\cf1\sub 10}{\cf1 \u8721\'b72(H}{\cf1\sub 2
}{\cf1 O) \cell 5.5-6\cell colorless-white\cell }{\i\cf1 am }{\cf1  radiating fibres \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Prehnite     }
{\i\cf1  r}{\cf1 \cell Ca}{\cf1\sub 2}{\cf1 Al}{\cf1\sub 2}{\cf1 Si}{\cf1\sub 3}{\cf1 O}{\cf1\sub 10}{\cf1 (OH)}{\cf1\sub 2}{\cf1  \cell 6-6.5\cell Lt Green-pink\cell }{\i\cf1 v, am, p }{\cf1  globular, pearly\cell }\pard\plain 
\widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Pumpellyite  }{\i\cf1 c}{\cf1 \cell Ca}{\cf1\sub 2}{\cf1 MgAl}{\cf1\sub 2}{\cf1 Si}{\cf1\sub 3}{\cf1 O}{\cf1\sub 11}{
\cf1 (OH)}{\cf1\sub 2}{\cf1   H}{\cf1\sub 2}{\cf1 O\cell 5.5\cell Green\cell }{\i\cf1 am, p}{\cf1   mosaic pattern\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright 
\f4\cgrid {\cf1 Quartz***    }{\i\cf1 c}{\cf1 \cell SiO}{\cf1\sub 2}{\cf1 \cell 7\cell colorless-varied\cell }{\i\cf1 am, v, p }{\cf1 \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain 
\s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Saponite   }{\i\cf1 r}{\cf1 \cell (Ca,Na)}{\cf1\sub 0.3}{\cf1 (Mg,Fe)}{\cf1\sub 3}{\cf1 (Si,Al)}{\cf1\sub 4}{\cf1 O}{\cf1\sub 10}{\cf1 (OH)}{\cf1\sub 2}{\cf1  \u8721\'b74H}{\cf1\sub 2}{\cf1 O\cell 1.5-2
\cell Lt green-yellow-gr\cell }{\i\cf1 am}{\cf1   granular, earthy\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Thomsonite }{\i\cf1 r}{\cf1 
\cell  NaCa}{\cf1\sub 2}{\cf1 Al}{\cf1\sub 5}{\cf1 Si}{\cf1\sub 5}{\cf1 O}{\cf1\sub 20}{\cf1 \u8721\'b76(H}{\cf1\sub 2}{\cf1 O) \cell 5-5.5\cell pink\cell }{\i\cf1 am, p}{\cf1   radiating  xtals\cell }\pard\plain \widctlpar\intbl\adjustright 
\loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 Xonolite   }{\i\cf1 vr}{\cf1 \cell Ca}{\cf1\sub 6}{\cf1 Si}{\cf1\sub 6}{\cf1 O}{\cf1\sub 17}{\cf1 (OH)}{\cf1\sub 2}{\cf1 \cell 6.5\cell 
colorless, gray\cell }{\i\cf1 v}{\cf1   with and like datolite\cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\trowd \clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr
\brdrs\brdrw15 \cltxlrtb \cellx1612\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx6292\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr
\brdrs\brdrw15 \cltxlrtb \cellx7544\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr\brdrs\brdrw15 \cltxlrtb \cellx9776\clvertalt\clbrdrt\brdrs\brdrw15 \clbrdrl\brdrs\brdrw15 \clbrdrb\brdrs\brdrw15 \clbrdrr
\brdrs\brdrw15 \cltxlrtb \cellx12368\pard\plain \s18\nowidctlpar\intbl\adjustright \f4\cgrid {\cf1 \cell \cell \cell \cell \cell }\pard\plain \widctlpar\intbl\adjustright \loch\af4\hich\af4\dbch\f4\cgrid {\cf1 \row }\pard \widctlpar\adjustright {\cf1 

\par }\pard\plain \s15\widctlpar\adjustright \fs20\loch\af6\hich\af6\dbch\f4\cgrid {\fs24 
\par }}