Field Project
Emerald Bay
By: Erin Whitlow
GEL 103
Background
• 2 million years ago there was a shift in tectonic
plates, and the Tahoe basin sank between the
Sierra crest and the Carson range.
• 10 thousand years ago glaciers formed at the
highest elevation on the north, west, and south
sides.
• The movement of the glaciers is what formed
what we now call emerald bay.
("History of tahoe," )
Granite
• Granite is an igneous rock
made up of crystallized
minerals from felsic magma.
• Consists of potassium,
feldspar, plagroclase, and
quartz.
• Granite is the most common
plutonic rock.
• This granite was formed during
the Mountain building of the
Sierra crest.
• A normal fault can be seen
near the top.
(Monroe & Wicander, 2012)
Sandstone
• Sandstone is a
sedimentary rock.
• It is created when
detrital sedimentary rock
made of solid particles of
sand is compacted over
time and becomes
sandstone.
• This sandstone has a line
of quartz going through it.
(Monroe & Wicander, 2012)
Fern
• The fern is classified as a seedless
vascular plant.
• They evolved from non-vascular
then vascular seedless.
• They evolved during the
Devonian and Carboniferous
periods.
• They have a flagellated sperm
that must swim through water to
get to the egg.
• The vascular plants could grow
taller than non-vascular because
they could transport food and
water more efficiently.
(Reece, Urry, Cain, Wasserman, Mino
rsky & Jackson, 2011)
Lodge Pole Pine
• The lodge pole pine is a conifer
and classified as a gymnosperm.
• They evolved from non-vascular,
then seedless vascular, and finally
seed plants.
• The seed plants evolved pollen
and ovules, so they no longer
needed water to reproduce.
• They evolved when the
Carboniferous changed into the
Permian period because the drier
conditions favored the seed
plants.
(Reece, Urry, Cain, Wasserman,
Minorsky & Jackson, 2011)
Water Outlet
• This water is snow melt
from the top.
• The water is making it’s
way down the mountain
and eroding the land.
• Overtime this water has a
very strong effect on the
landscape and can erode
the rock into sediment
where it can then be
compacted and start the
process all over again.
References
• Monroe, J., & Wicander, R. (2012). The changing
earth exploring geology and evolution. (6th ed.).
Belmon, CA: Brooks/Cole.
• Reece, J., Urry, L., Cain, M., Wasserman, S.,
Minorsky, P., & Jackson, R. (2011). Campbell
biology. (9th ed.). San Francisco, CA: Pearson
Benjamin Cummings.
• History of tahoe. (n.d.). Retrieved from
www.geocaching.com/seek/cache_detail
• All photos are taken by author

Field project

  • 1.
    Field Project Emerald Bay By:Erin Whitlow GEL 103
  • 2.
    Background • 2 millionyears ago there was a shift in tectonic plates, and the Tahoe basin sank between the Sierra crest and the Carson range. • 10 thousand years ago glaciers formed at the highest elevation on the north, west, and south sides. • The movement of the glaciers is what formed what we now call emerald bay. ("History of tahoe," )
  • 3.
    Granite • Granite isan igneous rock made up of crystallized minerals from felsic magma. • Consists of potassium, feldspar, plagroclase, and quartz. • Granite is the most common plutonic rock. • This granite was formed during the Mountain building of the Sierra crest. • A normal fault can be seen near the top. (Monroe & Wicander, 2012)
  • 4.
    Sandstone • Sandstone isa sedimentary rock. • It is created when detrital sedimentary rock made of solid particles of sand is compacted over time and becomes sandstone. • This sandstone has a line of quartz going through it. (Monroe & Wicander, 2012)
  • 5.
    Fern • The fernis classified as a seedless vascular plant. • They evolved from non-vascular then vascular seedless. • They evolved during the Devonian and Carboniferous periods. • They have a flagellated sperm that must swim through water to get to the egg. • The vascular plants could grow taller than non-vascular because they could transport food and water more efficiently. (Reece, Urry, Cain, Wasserman, Mino rsky & Jackson, 2011)
  • 6.
    Lodge Pole Pine •The lodge pole pine is a conifer and classified as a gymnosperm. • They evolved from non-vascular, then seedless vascular, and finally seed plants. • The seed plants evolved pollen and ovules, so they no longer needed water to reproduce. • They evolved when the Carboniferous changed into the Permian period because the drier conditions favored the seed plants. (Reece, Urry, Cain, Wasserman, Minorsky & Jackson, 2011)
  • 7.
    Water Outlet • Thiswater is snow melt from the top. • The water is making it’s way down the mountain and eroding the land. • Overtime this water has a very strong effect on the landscape and can erode the rock into sediment where it can then be compacted and start the process all over again.
  • 8.
    References • Monroe, J.,& Wicander, R. (2012). The changing earth exploring geology and evolution. (6th ed.). Belmon, CA: Brooks/Cole. • Reece, J., Urry, L., Cain, M., Wasserman, S., Minorsky, P., & Jackson, R. (2011). Campbell biology. (9th ed.). San Francisco, CA: Pearson Benjamin Cummings. • History of tahoe. (n.d.). Retrieved from www.geocaching.com/seek/cache_detail • All photos are taken by author