America's Volcanic Past -
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"Though few people in the United States may actually experience an erupting volcano, the evidence for earlier volcanism is preserved in many rocks of North America. Features seen in volcanic rocks only hours old are also present in ancient volcanic rocks, both at the surface and buried beneath younger deposits." -- Excerpt from: Brantley, 1994 |
Volcanic Highlights and Features:
[This list is just a sample of
various Maine volcanic features or events and is by no means inclusive.]
Ancient volcanic rocks are preserved in many parts of Maine, but there have not been
any active volcanoes since the Mesozoic Era.
An interesting aspect of Maine's bedrock is that it records a wide array of
geologic environments that have been present.
All three major rock types, igneous, sedimentary, and
metamorphic, are represented.
Within each of these major types there is a large variety as well.
Igneous rocks include both volcanic and plutonic types
generated in rift environments,
oceanic environments, island arc settings, and
continental collision zones.
Sedimentary rocks include terrestrial breccia and conglomerate with vascular plant fossils,
shallow marine
sandstones, carbonate reefs, anoxic black shales,
variously mature and immature wackes, submarine channel and turbidite deposits, and deep
sea chert. Metamorphic rocks are found in contact aureoles around plutons as
well as in widespread regional metamorphic zones ranging
from sub-chlorite zone in the north to sillimanite +K-feldspar zone in the southwest.
Several episodes of crustal deformation have produced
folds, faults, and shear zones now preserved in the bedrock.
This variety of geologic features has attracted geologists with a diversity of
backgrounds to study in Maine.
Excerpts from: Maine Geologic Survey, Maine Department of Conservation Website, 2001 |
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The Appalachians:4
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Precambrian (545-650 (?) million years ago):2
Early Paleozoic Era (443-545 million years ago):2
Middle Paleozoic Era (360-443 million years ago):2
Late Paleozoic Era (245-360 million years ago):2
Mesozoic Era (66-245 million years ago):2
Cenozoic Era (present to 66 million years ago):2
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Maine's Volcanic Rocks |
Maine's Rocks:1
An interesting aspect of Maine's bedrock
is that it records a wide array of geologic
environments that have been present.
All three major rock types,
igneous, sedimentary, and metamorphic, are represented.
Within each of these major types there is a
large variety as well. Igneous rocks include both
volcanic and plutonic types generated in rift
environments, oceanic environments,
island arc settings, and continental collision zones. Sedimentary rocks
include terrestrial breccia and conglomerate
with vascular plant fossils, shallow
marine sandstones, carbonate reefs, anoxic
black shales, variously mature
and immature wackes, submarine channel and
turbidite deposits, and deep sea chert.
Metamorphic rocks are found in contact
aureoles around plutons as
well as in widespread regional
metamorphic zones ranging from sub-chlorite
zone in the north to sillimanite + K-feldspar
zone in the southwest. Several
episodes of crustal deformation have produced
folds, faults, and shear zones now preserved
in the bedrock. This variety of geologic features has attracted
geologists with a diversity of backgrounds to
study in Maine.
Maine's Granite:1
Granite is an igneous rock that
forms by slow solidification of
magma at depths of several
kilometers below the earth's surface.
Yet, hundreds of granite bodies are exposed
in Maine at the ground surface.
Therefore, the gradual process of
erosion has, over geologic time, removed
several kilometers of rock that used to
rest above what is now the Maine landscape.
Maine granite
comes in many colors and textures,
with each quarry yielding its own variety of
stone. Activity and competition in the
granite industry were highest in the
late 1800's, reaching a
peak in 1901. Many large public buildings such as libraries,
post offices, customs houses, and
museums built at that time in the eastern U.S.,
including New York City, Washington, D.C.,
and Chicago are made of Maine granite. Although
they are almost all inactive, the
old quarries still dot the landscape,
mainly in the coastal region from
Penobscot Bay to Washington County.
Maine's Pegmatite:1
As with any branch of natural history,
bedrock geology is driven by an innate curiosity
to know more about the world in which we live. What is it made of?
How did it form? Many people enjoy discovering,
photographing, sketching, or collecting rocks,
minerals, and fossils. While each type of mineral or fossil
can be expected from only certain kinds of rock,
there is enough uncertainty in our knowledge that
specific discoveries are difficult to predict. For
example, the Oxford County region is well known
for the occurrence of a rock called pegmatite (an intrusive igneous
rock)
that has yielded spectacular mineral discoveries such as
tourmaline, beryl, apatite and lepidolite,
but it is hard to know which pegmatite body will
produce the next big discovery, or which exotic minerals will be
found. Both beginners and experienced collectors
who put in some time may find treasures, large or small.
Maine's Traveler Rhyolite:1
Much of the northern part of Baxter State Park is underlain with
rhyolite, a light-colored volcanic rock
that is similar in composition to
granite, in this case the Katahdin granite,
but that is much finer grained.
In many outcrops the grains are too fine to see with the naked eye. Most of
the peaks (The Traveler, North Traveler, Black Cat Mountain), the cliffs
around Upper and Lower South Branch Ponds, and the mountains
you passed on the way into the park (Horse Mountain) are underlain
with this rock. Most of the unit formed from large eruptions of volcanic
ash rather than by flows of molten magma.
The Traveler Rhyolite is
probably 3,200 meters thick and tilts northward at a moderate angle.
In a close up of the Traveler Rhyolite, the dark streaks in the rock
are flattened pieces of pumice that
formed as a rain of volcanic bombs
that accompanied the ash eruption.
Maine's Vinalhaven Rhyolite:1
The geology of the northern part of Vinalhaven, from Middle Mountain
to Browns Head, is less famous than the Vinalhaven granite but in some ways
more interesting.
A variety of volcanic rocks give clues to an ancient
past when this part of the earth's crust was being formed. Collectively,
these rocks have been named the Vinalhaven Rhyolite,
after the most
common type of volcanic rock there.
We know that this small part of Maine's crust was formed by
volcanic activity much like that which occurs
today in the Caribbean Antilles or the Aegean Sea of the northern Mediterranean.
Unfortunately, the age of the Vinalhaven Rhyolite is difficult
to determine, but the best estimate is that it formed in the
Silurian Period, more than 420 million years ago.
There once were Volcanic Islands:1
During the protracted geologic history
that has brought Maine to the current stage, the movement
of continents by the mechanism of plate
tectonics has caused the earth's surface to evolve.
Volcanic rocks and distinctive fossil shells
show that some of
Maine's rocks formed on volcanic islands
in a wide ocean that no longer exists.
Geologic
similarities between parts of the Maine
coast and parts of Newfoundland and Wales suggest that
these areas formed together on a small
continent far away from North America.
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Acadia National Park |
Cranberry Island Formation:3
About 400 million years ago,
volcanoes belched out their contents of ash which came to rest on a
sea bottom.
During the times when seaweeds dominated
the plant world, pressure and heat
transformed these sediments into rocks known as the
Cranberry Island formation.
Schoodic Peninsula:3
Far below the earth's surface, a huge molasses-like
plug of magma at least 8 miles in diameter
moved upward. And, as it undermined the
overlying bedrock, the heavy roof bedrock began to sag,
eventually sinking and melting into the magma.
The fiery mass incorporated material from the
earlier granites,
from diorite, and from the weak rocks.
Eventually it reached the surface, and
gradually cooled to form the coarse-grained granite.
After the various granites developed, other
minor intrusions of molten material occurred.
The most conspicuous of these consisted of
black diabase
dikes that spread themselves into open fractures of older rock.
The most obvious
examples of these formations in the park are on Schoodic Peninsula.
Baxter State Park |
Mount Katahdin:1
An area of outstanding natural beauty, Baxter State Park is home to
some of Maine's most unique geology.
Mount Katahdin's huge
granite massif
yields northward to lower peaks underlain with volcanic
rhyolite and valleys underlain with sandstone and fossiliferous shale.
For those
willing to put in a little effort, a fabulous
cross section of this geology
can be toured along South Branch Pond Brook between South Branch
Pond and Trout Brook.
Traveler Rhyolite:1
Much of the northern part of Baxter State Park is underlain with
rhyolite, a light-colored volcanic rock that is similar in composition to
granite, in this case the Katahdin granite, but that is much finer grained.
In many outcrops the grains are too fine to see with the naked eye. Most of
the peaks (The Traveler, North Traveler, Black Cat Mountain), the cliffs
around Upper and Lower South Branch Ponds, and the mountains
you passed on the way into the park (Horse Mountain) are underlain
with this rock. Most of the unit formed from large eruptions of volcanic
ash rather than by flows of molten magma.
The Traveler Rhyolite is
probably 3,200 meters thick and tilts northward at a moderate angle.
In a close up of the Traveler Rhyolite, the dark streaks in the rock
are flattened pieces of pumice that
formed as a rain of volcanic bombs
that accompanied the ash eruption.
Trout Valley Formation:1
The Trout Valley Formation
underlies Trout Valley, the most significant valley
in the northern part of the Park.
It consists of a variety of rock types,
including conglomerates at the base (probably of volcanic origin)
followed by sandstone and finally fossiliferous shale along
Trout Brook itself.
The Trout Valley Formation is about 500 meters thick.
The Conglomerate ---
The clasts are almost all rhyolite, with some being recognizable as
sections of the columns seen farther upstream.
Most are sub-angular boulders with a bit of ash between, but many
cobbles and boulders lay directly on others
rather than being supported by the ash.
A Lahar at the base of the Trout Valley Formation ---
is made up of angular pieces of the underlying
volcanic columns and is cemented by
volcanic ash. The rocks were deposited by a lahar, a violent eruption and
flow of ash that rips up pieces of the
underlying rocks as it travels rapidly down a mountain slope.
Lobster Lake and Seboomook Lake |
Lobster Lake:1
Along the shores of this beautiful lake northeast of Moosehead Lake
is some of the most spectacular geology found anywhere in the state. In
outcrop after outcrop, the shore of the lake reveals a complex
geological story that begins with deep-sea sediments,
is punctuated by several
periods of igneous activity and folding,
and ends with
shallow marine sediment that is profusely fossiliferous.
Lobster Mountain Volcanics:1
Much of Lobster Mountain on the west side of the lake and
Big Island is underlain by a variety of volcanic rocks collectively called
the Lobster Mountain volcanics.
These are all Ordovician in age
and probably represent volcanic islands created when part of the oceanic
crust was subducted. Lobster Mountain itself is underlain by a
light greenish gray rhyodacite: an otherwise very fine-grained rock with large
angular crystals of quartz. It weathers a distinctive light gray
and is well exposed on the trail to the summit
that begins at Jackson Cove.
Big Island Diabase Dikes:1
Big Island is underlain by a collection of volcanic rocks and
volcanically related sedimentary rocks.
These include pillow basalt,
siltstone, and sandstone. Some of the sandstone beds contain fossils.
Most of the prominent points and knobs on the island are
underlain by diabase
dikes which are more resistant to erosion.
These formed from
molten magma which forced its way through
cracks in the overlying sedimentary and volcanic material to
solidify at relatively shallow depths. A most interesting aspect of these dikes is
that they have features which indicate that they intruded soft,
wet sediment, not hard rock: isolated blobs of diabase are surrounded by
sedimentary rock; edges of dikes are unusually convoluted.
All this speaks to a very dynamic geologic environment in which sand and mud
were being deposited in a marine basin as magma was forcing its way up from depth.
Seboomook Lake, Northwestern Maine:1
The rocks of Maine record a rich history of geological
events that formed our landscape. Four hundred million years
ago, Maine was a vastly different place,
with an ocean covering most of the northern part of the State,
massive young mountains along the present-day coast,
and volcanoes punctuating all.
Sand and mud -- materials eroded from the young
mountains -- were deposited by ocean currents in layer upon layer.
Lava erupted from fissures into the seawater to form
oddly shaped deposits within the sand and mud.
All of these features are well exposed on Seboomook Lake, a long
narrow lake a few miles northwest of Moosehead Lake.
Seboomook Lake Pillow Lavas:1
Around the western part of Seboomook Lake
there are some volcanic rocks (Canada Falls Member of the Frontenac
Formation). They formed when fissures
opened in the ocean floor and molten rock (lava)
spewed onto the bottom of the
sea.
How do we know this? Within the
volcanic rocks are distinctive shapes,
called pillows by geologists, which form
when lava is suddenly cooled by contact
with cold water. The water immediately
cools and hardens the outer skin of
lava into a rind, but the pressure of the
eruption pushes more lava out until a
partially hardened blobby shape (pillow)
forms and breaks off. The process continues
as more lava erupts, in this way forming a
deposit made up almost entirely
of pillows.
Portland Head and the Cushing Formation |
Portland Head and the Cushing Formation:1
The bedrock that is exposed to view at Portland Head
(southern entrance to Portland Harbor)
belongs to the Cushing Formation.
This formation, named for Cushing Island, underlies
an area that stretches northeasterly across
Casco Bay from the Delano Park area of the
Cape Elizabeth shore through Cushing Island, Peaks
Island, most of Long Island, part of Chebeague Island,
the Goose Islands, and Birch Island to the
Brunswick shore just west of Harpswell
Neck. The Cushing Formation is more resistant to
weathering than the neighboring rock formations,
which is why it forms such prominent
rocky headlands and islands.
A close look at the rocks at Portland Head reveals
clues to its long geologic history.
For safety reasons, access to the rock cliffs below the
chain link fence is strictly prohibited.
You can see many of these features easily
from behind the fence or from the trails leading to the beach
north of the lighthouse.
Seen best on a clean surface,
the rock is a light gray gneiss
composed mainly of the minerals quartz and feldspar in
very small, almost microscopic grains.
Elsewhere, the Cushing Formation contains
larger rock fragments in addition to the minute mineral
fragments.
Such fragments are typical of
deposits produced by a series of explosive volcanic eruptions.
Certain minerals from the Cushing
Formation, carefully collected, processed, selected and analyzed in a
U.S. Geological Survey laboratory, have been dated at approximately
471 million years old (+/- 3 million), which is in the Ordovician Period.
This means that the volcanic eruptions that produced the Cushing
Formation occurred before the Himalayas or Alps had formed,
before the Atlantic Ocean
existed, before the dinosaurs lived, and before the
first land plants had evolved.
The volcanoes that must have existed near here at that
ancient time have long since been eroded; all that is left is a
layer of volcanic debris preserved in the rocks.
At a later time, probably in the Devonian or
Carboniferous periods, all the rocks of
southern Maine were heated, compressed, and twisted
causing the rocks to be stretched and deformed like putty.
This deformation also produced the strong "lineation,"
or alignment of minerals,
that characterizes the Cushing Formation at Portland Head.
The lineation is not horizontal, but is
tilted down toward the southwest at an angle of several degrees.
This lineation angle is what gives the rock an
overall sense of jutting out to the northeast into the sea.
Portland Head's Diabase Dike:1
Beyond the end of the fence below the foghorn, there is a deep,
steep-sided cleft in the rock. You can see the cleft
from across the cove or
look down into it at the fence by the foghorn.
At low tide, a different type of rock is
barely visible in the bottom of the cleft.
It is a dark colored rock called diabase or
basalt.
It formed when molten rock (magma) intruded along a vertical fracture and
solidified underground forming a thin sheet of rock called a dike.
The dike rock is more fractured and therefore weaker than the Cushing
Formation, so through the centuries the cleft has been eroded down
almost to low tide level. Such dikes of black, basaltic rock are common
along the Maine coast. Some are better preserved in the cliffs
just on the other side of the lighthouse,
toward the gift shop. Some of the larger
basaltic dikes in New England have been dated
at about 200 million years old,
indicating that they were intruded during the Mesozoic Era at
the time when Africa and Europe were splitting away from
North America to begin opening the modern Atlantic Ocean.
Seven Hundred Acre Island |
Seven Hundred Acre Island:2
Approximately 650 million years ago:
episode of metamorphism and pegmatite
intrusion in unknown geologic setting (near Islesboro).
Some sedimentary and volcanic rocks
on Seven Hundred Acre Island
were metamorphosed and cut by a
pegmatite
dated at 647 +/- 4 million years old.
The rocks which are cut by the pegmatite must be older,
but we don't know by how much.
Vinalhaven Island |
Vinalhaven Island Granite:1
Vinalhaven Island is a large island in Penobscot Bay, 1 hour and 15
minutes by ferry from Rockland.
The central and southern parts of
Vinalhaven are underlain by a massive body of
pink, medium-grained to fine-grained granite.
The Vinalhaven granite was quarried in the late
1800's and early 1900's as part of the famous Maine granite industry
that provided dimension stone and decorative stonework for large
buildings and bridges in Boston, New York, Chicago, and elsewhere.
Vinalhaven Island Rhyolite:1
The geology of the northern part of Vinalhaven, from Middle Mountain
to Browns Head, is less famous than the granite but in some ways
more interesting.
A variety of volcanic rocks give clues to an ancient
past when this part of the earth's crust was being formed. Collectively,
these rocks have been named the Vinalhaven Rhyolite,
after the most
common type of volcanic rock there.
We know that this small part of Maine's crust was formed by
volcanic activity much like that which occurs
today in the Caribbean Antilles or the Aegean Sea of the northern Mediterranean.
Unfortunately, the age of the Vinalhaven Rhyolite is difficult
to determine, but the best estimate is that it formed in the
Silurian Period, more than 420 million years ago.
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