North Cascades Geology
Metamorphic rocks. Cascade Peak held up by Cascade River Schist on the middle left. Next right is Mixup Mountain, carved from Magic Mountain Gneiss. Eldorado Peak underlain by the Eldorado Orthogneiss is on the skyline, left.
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Metamorphic Rocks
Metamorphic rocks are changed rocks, that is, rocks whose original
materials have recrystallized to form new minerals. Generally, this
recrystallization, called metamorphism, takes place when deeply buried
rocks are subjected to great pressure and high temperature. Most metamorphic
rocks have also been squeezed so that their shapes and the shapes of
their constituent minerals have changed during metamorphism, resulting
in a layered or streaky appearance.
Metamorphic rocks in the North Cascades formed
from pre-existing rocks of every kind and
from all of the major rock groups, igneous,
sedimentary, and metamorphic. For example, mica schist,
a common metamorphic rock in the North Cascades, recrystallized from
shale. Gneiss, which looks
like granite that has
been squeezed so that the rock looks streaky. Much North Cascades gneiss
formed from granitic rocks in exactly that way. Gneiss also forms from
schist when the rock remains hot enough for the metamorphic crystals
to grow large. Marble is metamorphosed limestone,
whose calcite crystals have grown large enough
to see without a hand lens.
This brief introduction to petrology, or the
study of rocks, has touched only on a few of
the hundreds of different kinds of rocks found in the North Cascades.
We name and describe many
of the others as the geologic story unfolds.
Phyllite.
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An ideal metamorphic sequence: A Rock's Progress from Shale to Gneiss or from Basalt to Amphibolite
In an ideal metamorphic sequence of increasing heat and pressure, a shale becomes slate and slate becomes phyllite, then schist, and finally gneiss. A shale, when highly squeezed deep in the Earth, first forms slate, as the shale's tiny grains and platy clay minerals slide around under the stress. The rock deforms that is, bends and flows and the minerals align themselves in the direction of yielding, or flow. Slate exhibits cleavage, meaning it can be broken into even, flat chips, slabs, or blackboards (at least in the past). If slate minerals further recrystallize, giving the rocks a shiny appearance, the new rock is phyllite. Phyllite also abounds in the North Cascades
Still further recrystallization produces a flaky crystalline rock called schist, usually mica schist made up of flat mica flakes and other minerals. These rocks exhibit foliation, a tendency to break into thin, curving leaves, or sheets, like the pages of a book (see Diablo Dam). Thorough recrystallization at higher temperature will produce a gneiss, looking rather like granite, but with minerals clearly arranged in a parallel fashion the foliation. In gneiss, the minerals feldspar and quartz have grown to become conspicuous crystals. The rock no longer breaks as easily along the foliation because the feldspar and quartz are
more randomly oriented and commonly have interlocking, irregular crystal
borders.
In progressive metamorphism of a basalt,
the course of change is different because the original basalt reacts
differently to heat and pressure. In fact, it is so stiff and resistent
to the squeezing (unlike wimpy shale) that the first reincarnation
as a metamorphic rock is simple recrystallization to a rock called greenstone named
because it is made of many green metamorphic minerals. Further squeezing
finally overcomes the basalt or greenstone resistance, forming greenschist,
which has many of the same minerals as greenstone but with the flaky
foliation of all schists. Rising temperature and continued squeezing
causes new minerals to crystallize, and what was formerly basalt becomes amphibolite,
a rock that looks like a dark gneiss and is rich in hornblende and
feldspar, but with very little quartz. To see this progression illustrated, click here.
Although all the rocks mentioned in these progressions
occur in the North Cascades, ambitious hikers would
find few places where they could walk continuously from the shale or
basalt into well-metamorphosed
gneiss or amphibolite. In a few places geologists
have found parts of the progression, such as phyllite, grading into
schist, or basalt grading
into greenstone. |