field assgt

30
Emerald Bay, Eagle Falls and the Sierra Nevada Field Assignment Professor Lawler- Geology 103 By Kalie Ceglia

Upload: klygrl

Post on 15-May-2015

145 views

Category:

Travel


7 download

TRANSCRIPT

Page 1: Field assgt

Emerald Bay, Eagle Falls and

the Sierra Nevada

Field Assignment Professor Lawler- Geology

103By Kalie Ceglia

Page 2: Field assgt

Contents:

• Geologic Evolution of Tahoe Basin and the Sierra Nevada• Rock Samples

• Quartz• Agate• Granite

• Plant Sample- ‘snow plant’• References

Page 3: Field assgt

Geologic evolution of Lake Tahoe Basin (started 400 million years ago) • Lake Tahoe was formed by faulting • 3 faults make up the Tahoe Basin- West Tahoe Fault ( Sierra Nevada), East Tahoe Fault ( Carson Range),

and the North Tahoe Fault• ‘Dropped down blocks ‘ formed the Basin in between• Soils include:- Andesitic volcanic rocks- Granodiorite- Metamorphic rock

Tahoefacts.com, 2013

Page 4: Field assgt

T. Macrae, 2009

• The weight of the glaciers cause it to move and flow downhill

• This creates U-shaped glacier valleys and V-shaped stream valleys

Page 5: Field assgt

The glaciers move through canyons like this one

Page 6: Field assgt

Glacier movement through river beds

Page 7: Field assgt

More recently:

• About 10MYR ago, the real uplift of the Sierra Nevada happened:

• Volcanic rock, sedimentary rock, and metamorphic rock were carried away to surrounding valleys, as a result there is still geologic evidence in the Tahoe Basin

• As recent as 10,000yr ago, the last parts of the Ice age, glaciation was happening in the Sierra Nevada

• How the Emerald Bay area was formed is an example of a lateral moraine( where sediment is transported, then deposited along the ridges)

Monroe, 357, 2006

Page 8: Field assgt

Evidence of Scraping

As the glaciermoves it picks up:• rocks• sediment• boulders

• The boulders androcks scrape alongthe bedrock

Page 9: Field assgt

Approx. 6800ft, Near Eagle Falls Trail

Page 10: Field assgt

Lake Tahoe and Basin

Features Metric unit English unit

Maximum depth(second deepest in the U.S.)

501 m 1,645 ft

Average depth 305 m 1,000 ftMaximum diameter(north-south)

35 km 22 mi

Minimum diameter(east-west)

19 km 12 mi

Surface area 495 km2 191 mi2

Average surface elevation(above sea level)

1,897 m 6,225 ft

Highest peak (Freel Peak) 3,320 m 10,891 ft

Tahoe.usgs.gov,2013

Page 11: Field assgt

Topographical map of Emerald Bay

Americansouthwest.net,2013

Page 12: Field assgt

The Glaciers Taking Shape

Glaciers:

• Glaciers are very large bodies of snow and ice combined

• When more snow accumulates than can melt, glaciers are formed

• The snow begins to melt in the day but refreezes at night , this forms the singular sheet of ice

Resendes, 2011

Page 13: Field assgt

Tahoebest.com, 2013

Lower Eagle FallsLocation: South Lake Tahoe, Lake Tahoe Basin, El Dorado CountyStream: Eagle CreekAlternate Names:Height: 140 ft.       Elevation: 6600 ft. (-350 ft.) Lat/Long:38.95185, -120.11029 

Page 14: Field assgt

Americansouthwest.net,2013

Topographical of Upper Eagle Falls and Eagle Falls Lake

Location: South Lake Tahoe, Lake Tahoe Basin, Eldorado County Height: ~20 ft. Elevation: 660 ft. Lat/Long: 38.94999N,120.11618W

Page 15: Field assgt

Lower Eagle Falls • During the Spring the snow melts rush down from above, come mid-summer, it is only a trickle

• Due to the number of visitors, there is an increasing environmental concern for the Eagle Falls area

Page 16: Field assgt

Standing on top of the Lower Eagle Falls

Fannette Island:

This island is made of Granite, which resisted the force of the glacial ice.

Page 17: Field assgt

Upper Eagle Falls

Location: South Lake Tahoe, Lake Tahoe Basin, Eldorado County Height: ~20 ft. Elevation: 6650 ft. Lat/Long: 38.94999N, 120.11618W

Page 18: Field assgt

UPPER EAGLE FALLS

(TAKEN FROM THE BRIDGE LOOKING DOWNSTREAM)

Page 19: Field assgt

Quartz found locally in the Lake Tahoe Basin

Rockshop,2013

Page 20: Field assgt

Quartz: mineral

•Form the continental crust•Most commonly clear, white (milky), or rose in color

• It is considered a hard and stable mineral• In metamorphic rock, it can become veineous and banded in appearance

www.backyardnature.net, 2013

Page 21: Field assgt

• Veins of quartz can provide evidence ofhydrothermal activity

Geology.com, 2013

Page 22: Field assgt

Agate: Semi-precious silica mineral

• Microcrystalline variety of silica

• Associated with and found around volcanic rocks or where volcanic activity once occurred

• Comes in a variety of shapes and colors

• Appears banded when cut

Page 23: Field assgt

More Agate

( This was found in the middle of the trail and was the only other specimen than the picture before during the whole hike)

Page 24: Field assgt

GraniteGranite: The Sierra Nevada was volcanically active. Not a surprise to find granite which was at one time magma

Page 25: Field assgt

Granite: igneous rock, silicate

• Granular• Intrusive• Varies in color: pink, white, gray, red• Mineral content: biotite, quartz, mica, orthoclase feldspar• Granite is part of the continental crust• It is magma from deep in the crust , cooled down and formed into

rock then pushed up to the Earth’s surface

Page 26: Field assgt

SARCODES OR ‘SNOWPLANT’

Page 28: Field assgt

ReferencesBackyard Nature with Jim Conrad. (n.d.). Retrieved from http://www.backyardnature.netEagle Falls Trail Lake Tahoe. (n.d.). Retrieved April 3, 2013, from http://www.tahoesbest.com/eagle-falls-trail-lake-tahoeEmerald Bay SP. (n.d.). Retrieved  2013, from http://www.parks.ca.gov/?page_id=506Facts about Lake Tahoe. (n.d.). Retrieved from http://tahoe.usgs.gov/facts.htmlGoogle Image Result for http://www.aboutlaketahoe.com/hiking/topo-maps/emerald-bay-topo.jpg. (n.d.). Retrieved June 16, 2013, from http://www.google.com/imgres?imgurl=http://www.aboutlaketahoe.com/hiking/topo-maps/emerald-bay-topo.jpg&imgrefurl=http://www.aboutlaketahoe.com/hiking/emerald_bay

Page 29: Field assgt

Granite: Igneous Rock - Pictures, Definition & More. (n.d.). Retrieved from http://geology.com/rocks/granite.shtmlGuyton, B. (1998). Glaciers of California: Modern glaciers, ice age glaciers, origin of Yosemite Valley, and a glacier tour in the Sierra Nevada. Berkeley: University of California Press.Hill, M. (1975). Geology of the Sierra Nevada. Berkeley: University of California Press.Lake Tahoe Facts, Natural History, & Human Histroy. (n.d.). Retrieved June from http://www.tahoeadventuresports.com/misc/tahoefacts.htmMacrae, T. (n.d.). Born of glaciers | Beetles In The Bush. Retrieved April 5, 2013, from http://beetlesinthebush.wordpress.com/2009/03/17/born-of-glaciers/

Page 30: Field assgt

Monroe, J. S., & Wicander, R. (2006). The changing Earth: Exploring geology and evolution. Belmont, CA: Thomson Brooks/Cole.Resendes (2011). Plate tectonics: Continental drift and mountain building. Berlin: Springer-Verlag.Sarcodes - Wikipedia, the free encyclopedia. (n.d.). Retrieved May 15, 2013, from http://en.wikipedia.org/wiki/SarcodesTopographic Map of the Eagle Falls Trail, Lake Tahoe, California. (n.d.). Retrieved from http://www.americansouthwest.net/california/lake_tahoe/eagle-falls-trail-map.htmlWikipedia, the free encyclopedia. (n.d.). Retrieved June 18, 2013, from http://en.wikipedia.org/