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Cold Creek Trail & High
Meadow
Lake Tahoe, California
1
Patrick Rulo
Professor Mark Lawler
Geology 103
June 18,2015
Photo by P. Rulo
High Meadow
Location
Cold Creek Trail is located in South Lake Tahoe and
is a popular mountain biking trail. The trail starts up a
moderate grade through a pine forest and goes
through different zones as elevation changes. At the
top of the trail is High Meadow and then the trail
follows Cold Creek back to the start.
2
Methodology
• During May and June I hiked and rode Cold
Creek trail a couple of times, taking pictures and
collecting samples, while familiarizing myself with
the area.
• Plant ID was performed with Wildflowers of the
Tahoe Sierra
• Rock ID was performed with Rocks & Minerals
3
4
Off to Collect Samples on
Cold Creek Trail
Photo P. Rulo Collection
Overview of Geological History of Lake
Tahoe & Sierra Nevada Mountain Range.
• According to the Geological Society of America,
evidence suggest that the Sierra Nevada are a result
of an uplift from the crust becoming thicker during the
Late Cretaceous or Early Cenozoic Period.(GSA)
• A rain shadow east of the Sierra Nevada has been
around since the middle Miocene Period. (GSA)
5
Overview of Geological History of Lake
Tahoe & Sierra Nevada Mountain Range.
• Lake Tahoe Basin was the result of block faulting
2-3 million years ago. (USGS)
• Around 2.5 years ago glaciation eroded many
parts of the Sierra Nevada. (Wikipedia)
• Uplifting of the Sierra Nevada is on ongoing
process that is still occurring.
Rocks found around Cold
Creek Trail & Lake Tahoe
7
Photo by P. Rulo
Rocks found around Cold
Creek Trail & Lake Tahoe
• The oldest rocks in the Sierra Nevada are
metamorphic rocks such as schists and
slates.(wikipedia)
• Granite was formed as early as the Jurassic Period.
• Much of the course soil and rocks are a result of
glaciation and erosion.
• Quartz is common in surface rocks and igneous
rocks such as granite.
8
Granite
Igneous Rock
Sialic- Silica Rich
9
Basalt
Igneous Rock
10
Schist
Metamorphic Rock
11
Milky Quartz
Silicate
12
Rose Quartz
Silicate
13
Flora & Fauna
14
Mountain Mule Ears
Wythea mollis
15
Photo By P.Rulo
Mountain Mule Ears
Wythea mollis
• Member of the Sunflower Family
• Common in Lake Tahoe from 6250’ to 8500
• Broad leaves covered with white silky hairs to
lessen evaporation.
• One plant can be reproduced if only one flower is
pollinated.
• Range:Sierra Nevada to Oregon.
16
Rosy Sedum
Sedum roseum
17 Photo by P.Rulo
Rosy Sedum
Sedum roseum
• Member of Stonecrop family
• Found in Rocky areas
• Range in Tahoe: 7,000’ to 10,500’
18
Snow Plant
Sarcodes sanguinea
19
Snow Plant
Sarcodes sanguinea
• Member of the Wintergreen Family
• Resembles an asparagus and is edible, although,
it is protected.
• Does not photosynthesize, but is mycotrophic.
• Found on forest floors up to 8,000’.
• Appears in spring in shaded areas.
20
Black Bear
Ursus Americanus
21
Photo from Google
Black Bear
Ursus Americanus
• The American Black Bear is the most common bear species in the
world.
• Despite being called black bears, they can have brown, blonde and
cinnamon colored coats.
• Black bears are omnivorous.
• Bears live in various habitats and can be found from elevations at
1,300’ to 9,800’.
• Black Bears are highly efficient at hibernating through the lean
months of the year.
• Bears live from 18 to 23 years.
22
Invasive Species
Canis Familiarus Daisy
23
Invasive Species
Canis Familiarus Daisy
• Introduced to Tahoe in 2012.
• Member of Canis rulo family.
• Likes to run in packs with mountain bikes.
• Omnivore, prefers kibble and cookies.
24
High Meadow
25
High Meadow and how
meadows form
• Meadows form when sediment fills lakes and ponds and
over a long period of time,water becomes earth. Grasses
and other sun dependent plants form the meadow. An
example of this process is Mirror Lake in Yosemite Valley.
• Meadows serve as a wetland for the mountains by filtering
water.
• As time goes by, the meadow is invaded by various pine
trees.
• The pine trees eventually block the sunlight making the
meadow disappear.
26
High Meadow
27
High Meadow
28
High Meadow
29
Cold Creek Trail
Riparian Area
30
Cold Creek
31
Cold Creek
32
Cold Creek
• Boulders have the appearance of being pushed
into a pile, like a moraine at the snout of a glacier
that I have seen from mountaineering.
• This appears to be evidence of glaciation from
the last ice age, when the Sierra Nevada’s had
significant glaciers.
33
Conclusion
• Geologic Processes have formed the mountains
that we love and those processes will constantly
change them.
34
References
• Baker, Elna, An Island Called California, University of California
Press, Berkeley, 1972
• Blackwell, Laird R. Wildflowers of the Tahoe Sierra, Lone Pine
Publishing, 1997
• Unknown, Rocks & Minerals, St Martins Press,1973
• wikipedia.org Black Bear & Geology of the Sierra Nevada
• USGS.Gov Lake Tahoe Geology overview
• geology.gsapubs.org Henry, Christopher,Uplift of the Sierra
Nevada, Viewed on June 19, 2015
35

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Field assignment

  • 1. Cold Creek Trail & High Meadow Lake Tahoe, California 1 Patrick Rulo Professor Mark Lawler Geology 103 June 18,2015 Photo by P. Rulo High Meadow
  • 2. Location Cold Creek Trail is located in South Lake Tahoe and is a popular mountain biking trail. The trail starts up a moderate grade through a pine forest and goes through different zones as elevation changes. At the top of the trail is High Meadow and then the trail follows Cold Creek back to the start. 2
  • 3. Methodology • During May and June I hiked and rode Cold Creek trail a couple of times, taking pictures and collecting samples, while familiarizing myself with the area. • Plant ID was performed with Wildflowers of the Tahoe Sierra • Rock ID was performed with Rocks & Minerals 3
  • 4. 4 Off to Collect Samples on Cold Creek Trail Photo P. Rulo Collection
  • 5. Overview of Geological History of Lake Tahoe & Sierra Nevada Mountain Range. • According to the Geological Society of America, evidence suggest that the Sierra Nevada are a result of an uplift from the crust becoming thicker during the Late Cretaceous or Early Cenozoic Period.(GSA) • A rain shadow east of the Sierra Nevada has been around since the middle Miocene Period. (GSA) 5
  • 6. Overview of Geological History of Lake Tahoe & Sierra Nevada Mountain Range. • Lake Tahoe Basin was the result of block faulting 2-3 million years ago. (USGS) • Around 2.5 years ago glaciation eroded many parts of the Sierra Nevada. (Wikipedia) • Uplifting of the Sierra Nevada is on ongoing process that is still occurring.
  • 7. Rocks found around Cold Creek Trail & Lake Tahoe 7 Photo by P. Rulo
  • 8. Rocks found around Cold Creek Trail & Lake Tahoe • The oldest rocks in the Sierra Nevada are metamorphic rocks such as schists and slates.(wikipedia) • Granite was formed as early as the Jurassic Period. • Much of the course soil and rocks are a result of glaciation and erosion. • Quartz is common in surface rocks and igneous rocks such as granite. 8
  • 15. Mountain Mule Ears Wythea mollis 15 Photo By P.Rulo
  • 16. Mountain Mule Ears Wythea mollis • Member of the Sunflower Family • Common in Lake Tahoe from 6250’ to 8500 • Broad leaves covered with white silky hairs to lessen evaporation. • One plant can be reproduced if only one flower is pollinated. • Range:Sierra Nevada to Oregon. 16
  • 17. Rosy Sedum Sedum roseum 17 Photo by P.Rulo
  • 18. Rosy Sedum Sedum roseum • Member of Stonecrop family • Found in Rocky areas • Range in Tahoe: 7,000’ to 10,500’ 18
  • 20. Snow Plant Sarcodes sanguinea • Member of the Wintergreen Family • Resembles an asparagus and is edible, although, it is protected. • Does not photosynthesize, but is mycotrophic. • Found on forest floors up to 8,000’. • Appears in spring in shaded areas. 20
  • 22. Black Bear Ursus Americanus • The American Black Bear is the most common bear species in the world. • Despite being called black bears, they can have brown, blonde and cinnamon colored coats. • Black bears are omnivorous. • Bears live in various habitats and can be found from elevations at 1,300’ to 9,800’. • Black Bears are highly efficient at hibernating through the lean months of the year. • Bears live from 18 to 23 years. 22
  • 24. Invasive Species Canis Familiarus Daisy • Introduced to Tahoe in 2012. • Member of Canis rulo family. • Likes to run in packs with mountain bikes. • Omnivore, prefers kibble and cookies. 24
  • 26. High Meadow and how meadows form • Meadows form when sediment fills lakes and ponds and over a long period of time,water becomes earth. Grasses and other sun dependent plants form the meadow. An example of this process is Mirror Lake in Yosemite Valley. • Meadows serve as a wetland for the mountains by filtering water. • As time goes by, the meadow is invaded by various pine trees. • The pine trees eventually block the sunlight making the meadow disappear. 26
  • 33. Cold Creek • Boulders have the appearance of being pushed into a pile, like a moraine at the snout of a glacier that I have seen from mountaineering. • This appears to be evidence of glaciation from the last ice age, when the Sierra Nevada’s had significant glaciers. 33
  • 34. Conclusion • Geologic Processes have formed the mountains that we love and those processes will constantly change them. 34
  • 35. References • Baker, Elna, An Island Called California, University of California Press, Berkeley, 1972 • Blackwell, Laird R. Wildflowers of the Tahoe Sierra, Lone Pine Publishing, 1997 • Unknown, Rocks & Minerals, St Martins Press,1973 • wikipedia.org Black Bear & Geology of the Sierra Nevada • USGS.Gov Lake Tahoe Geology overview • geology.gsapubs.org Henry, Christopher,Uplift of the Sierra Nevada, Viewed on June 19, 2015 35