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YOSEMITE
The Evolution of
the Valley
Heather McNenny
Geology 103, LTCC
Mark Lawlor
June 20, 2013
“It is by far the
grandest of all the
special temples of
Nature I was ever
permitted to enter.” —
John Muir
OVERVIEW
Yosemite has captured the
eyes of photographers and
travelers since it's
increased accessibility by
the Yosemite Valley
Railroad in 1907.
The scenery of the
glaciated landscape
marked the necessity of
preservation as a national
park.
Through this presentation,
the evolution of such
dramatic polished granite
landscape will be
discussed.
THE BEGINNING
The origins of the Sierra
Nevada began with rock
forming on the sea floor of
the western part of North
America. This rock was
lifted above sea level and
formed into a mountain
range, surrounded by
volcanoes. The core of the
Sierra Nevada was formed
by the granite caused by
molten rock from the
volcanoes.
After erosion of
sedimentary and volcanic
rock over the granite took
place , green scenery
covered the land. Streams,
valleys, and hills were
prevalent .
The Merced River flowed
through the forests and
hills.
50 Million Years Ago
OhRanger.com
10 Million Years Ago
Uplifting and westward
tilting causing the Merced
River to flow faster and
stronger, cutting into the
valley.
During this time, there was
an abundance of conifers,
beginning the dominance
of the Sequoia tree. The
climate was drier, and cool.
3 Million Years Ago
The climate was getting
cooler due to the
approaching Ice Age. This
affected the forests,
causing them to die off.
There was continual uplift
in the land, causing the
Merced to cut into it's
valley by 3,000 feet.
OhRanger.com
Glacier Activity
Glacial events occurred,
filling the valley with ice
and snow completely.
Most of the peaks seen
today were completely
engulfed, though Half
Dome still towered at 900
feet.
The valley was shaped into
a "U" form by the
glaciation.
Cascades were formed
above the valley caused by
the tributaries formed by
the run off of the Merced
River.1 Million to 250,000 years
ago
OhRanger.com
The Yosemite Glacier an
event that occurred during
the Tioga Glaciation. This
ice sheet had little impact
to erosion on the valley
because it was very small,
and lacked the powerful
erosion it needed to cut
into the valley.
30,000 Years Ago
10,000 Years Ago
The last glacier melted,
creating Lake Yosemite.
This was something that
occurred after each
freeze/thaw episode.
Eventually the lake filled
with silt, creating the valley
floor. What is left behind is
now called "Mirror Lake." It
is filled by snowmelt in a
similar process.
Mirror Lake
OhRanger.com
Yosemite's
Waterfalls
Though glaciers are not
responsible for the
creation of the waterfalls,
they carved the land that
they fall over. Snowmelt
determines the force and
longevity of the falls each
year.
Yosemite Falls is 2425
feet high, making it the
tallest waterfall in North
America. It dries up by the
end of summer.
Ribbon Falls- Typically the
first fall to dry up towards
summer
All of Yosemite's streams
and waterways end up in
the Tuolumne and Merced
Rivers. The Tuolumne feeds
Lake Eleanor and the Hetch
Hetchy Resevoir, which are
water sources for
California. All of the famed
waterfalls of Yosemite end
up in the Merced at the
valley floor.
National Park Service
TYPES OF ROCK IN
YOSEMITE
Plutonic Igneous
Rock-
Granite
Granodiorite
Tonalite
Quartz monzonite
Quartz monzodiorite
Quartz diorite
Diorite
Gabbro
Plutonic rocks formed
during Cretaceous Period
Formed by continual
intrusions of magma
beneath the Earths surface
into older rocks.
El Capitan-Consists of El
Cap Granite
National Park Service
Volcanic Igneous
Rock
-Basalt Flows
-Latite Tuff
-Latite Lava Flows
Though unable to locate
any for photos, there are
some small amounts of
volcanic igneous rock in
Yosemite Valley. The photo
to the right is an example
of volcanic igneous rock.
Metamorphic Rock can also
be found around Yosemite.
Caused by two northwest
treding belts of
metamorphic rock, on each
side of the batholith before
it's exposure, and creation.
Cathedral Peak
Granodiorite-Photo Credit:
National Park Service
Photo Credit: Mike Dunn
Dunn, Mike. 2006
Yellowstone Ecology
Institute Highlights. National Park Service
References
Yosemite National Park CA. National Park Service. Web. June 15,2013.
Yosemite. Yosemite Online.<yosemtie.ca.us> Web. June 15, 2013.
Yosemite National Park. National Geographic. Seventh Edition, 2012.
Web. June15, 2013.
Evolution of Yosemite Valley. OhRanger.Com. Web. June15,2013.
*Visited Yosemite for 3 days and took most information from Rangers, as
well as information boards on hikes and points of interests.
All photos taken by myself unless otherwise credited appropriately
"North America Wall"- El
Capitan

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Evolution of Yosemite Valley's Glaciated Landscape

  • 1. YOSEMITE The Evolution of the Valley Heather McNenny Geology 103, LTCC Mark Lawlor June 20, 2013 “It is by far the grandest of all the special temples of Nature I was ever permitted to enter.” — John Muir
  • 2. OVERVIEW Yosemite has captured the eyes of photographers and travelers since it's increased accessibility by the Yosemite Valley Railroad in 1907. The scenery of the glaciated landscape marked the necessity of preservation as a national park. Through this presentation, the evolution of such dramatic polished granite landscape will be discussed.
  • 3. THE BEGINNING The origins of the Sierra Nevada began with rock forming on the sea floor of the western part of North America. This rock was lifted above sea level and formed into a mountain range, surrounded by volcanoes. The core of the Sierra Nevada was formed by the granite caused by molten rock from the volcanoes. After erosion of sedimentary and volcanic rock over the granite took place , green scenery covered the land. Streams, valleys, and hills were prevalent . The Merced River flowed through the forests and hills. 50 Million Years Ago OhRanger.com
  • 4. 10 Million Years Ago Uplifting and westward tilting causing the Merced River to flow faster and stronger, cutting into the valley. During this time, there was an abundance of conifers, beginning the dominance of the Sequoia tree. The climate was drier, and cool. 3 Million Years Ago The climate was getting cooler due to the approaching Ice Age. This affected the forests, causing them to die off. There was continual uplift in the land, causing the Merced to cut into it's valley by 3,000 feet. OhRanger.com
  • 5. Glacier Activity Glacial events occurred, filling the valley with ice and snow completely. Most of the peaks seen today were completely engulfed, though Half Dome still towered at 900 feet. The valley was shaped into a "U" form by the glaciation. Cascades were formed above the valley caused by the tributaries formed by the run off of the Merced River.1 Million to 250,000 years ago OhRanger.com
  • 6. The Yosemite Glacier an event that occurred during the Tioga Glaciation. This ice sheet had little impact to erosion on the valley because it was very small, and lacked the powerful erosion it needed to cut into the valley. 30,000 Years Ago 10,000 Years Ago The last glacier melted, creating Lake Yosemite. This was something that occurred after each freeze/thaw episode. Eventually the lake filled with silt, creating the valley floor. What is left behind is now called "Mirror Lake." It is filled by snowmelt in a similar process. Mirror Lake OhRanger.com
  • 7. Yosemite's Waterfalls Though glaciers are not responsible for the creation of the waterfalls, they carved the land that they fall over. Snowmelt determines the force and longevity of the falls each year. Yosemite Falls is 2425 feet high, making it the tallest waterfall in North America. It dries up by the end of summer. Ribbon Falls- Typically the first fall to dry up towards summer All of Yosemite's streams and waterways end up in the Tuolumne and Merced Rivers. The Tuolumne feeds Lake Eleanor and the Hetch Hetchy Resevoir, which are water sources for California. All of the famed waterfalls of Yosemite end up in the Merced at the valley floor. National Park Service
  • 8. TYPES OF ROCK IN YOSEMITE Plutonic Igneous Rock- Granite Granodiorite Tonalite Quartz monzonite Quartz monzodiorite Quartz diorite Diorite Gabbro Plutonic rocks formed during Cretaceous Period Formed by continual intrusions of magma beneath the Earths surface into older rocks. El Capitan-Consists of El Cap Granite National Park Service
  • 9. Volcanic Igneous Rock -Basalt Flows -Latite Tuff -Latite Lava Flows Though unable to locate any for photos, there are some small amounts of volcanic igneous rock in Yosemite Valley. The photo to the right is an example of volcanic igneous rock. Metamorphic Rock can also be found around Yosemite. Caused by two northwest treding belts of metamorphic rock, on each side of the batholith before it's exposure, and creation. Cathedral Peak Granodiorite-Photo Credit: National Park Service Photo Credit: Mike Dunn Dunn, Mike. 2006 Yellowstone Ecology Institute Highlights. National Park Service
  • 10. References Yosemite National Park CA. National Park Service. Web. June 15,2013. Yosemite. Yosemite Online.<yosemtie.ca.us> Web. June 15, 2013. Yosemite National Park. National Geographic. Seventh Edition, 2012. Web. June15, 2013. Evolution of Yosemite Valley. OhRanger.Com. Web. June15,2013. *Visited Yosemite for 3 days and took most information from Rangers, as well as information boards on hikes and points of interests. All photos taken by myself unless otherwise credited appropriately "North America Wall"- El Capitan