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Harbor Seal by ahochstaedter from the GigaPan Seals at Hopkins Marine Lab, Pacific Grove, CA by ahochstaedter
resting
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Hopkins Marine Lab by ahochstaedter from the GigaPan Seals at Hopkins Marine Lab, Pacific Grove, CA by ahochstaedter
Part of Stanford University
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Granite by ahochstaedter from the GigaPan Seals at Hopkins Marine Lab, Pacific Grove, CA by ahochstaedter
coarse grained plutonic rock
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Harbor Seal by ahochstaedter from the GigaPan Seals at Hopkins Marine Lab, Pacific Grove, CA by ahochstaedter
Wathcing me
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Elephant Seal by ahochstaedter from the GigaPan Seals at Hopkins Marine Lab, Pacific Grove, CA by ahochstaedter
Young male
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Pipes by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
Pipes sticking out the wall of the ditch reveal the recent and rapid erosion of this ditch. Observers can see the poorly sorted backfill material that was used to backfill these trenches after the pipe was layed.
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Disturbed sediment by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
The process of digging a trench laying the pipe in the trench and then backfilling the ditch with poorly sorted material is now recorded in the wall of the erosional ditch.
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Cross-Bedded Sands by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
Cross bedding in sands indicative of deposition in a dune environment.
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Soil Horizons by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
nice soil horizons developed in the older dune sands.
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Oxidized Sand by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
The older dune sands have developed an oxidized layer, or B soil horizon. This horizon does not follow the dune surface to the left, indicating that the active dunes to the left have buried the older dunes beneath them.
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Active Dune by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
At the top of the active dune a much smaller soil profile has developed. A small amount of organic matter has been added to the surface of the dune, but a prominent B horizon has not developed.
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Pacific Ocean by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
this snapshot shows the top of the seacliff that is rapidly eroding.
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Interpretive Signs by ahochstaedter from the GigaPan Ft Ord Dunes St Park -- Erosional Ditch by ahochstaedter
Interpretive signs explain the ecology and geology of coastal dunes at Ft Ord Dunes State Park. The top of Stillwell Hall would have been visible about here before it was demolished in 2003.
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Layered Sands by ahochstaedter from the GigaPan Plio-Pleistocene Sediments in the Monterey Area by ahochstaedter
Strongly layered sands with cross bedded structures. Shown in more detail here: zoom.it/S9y4

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Gravels by ahochstaedter from the GigaPan Plio-Pleistocene Sediments in the Monterey Area by ahochstaedter
Gravels with weak layering
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Layered sands by ahochstaedter from the GigaPan Plio-Pleistocene Sediments in the Monterey Area by ahochstaedter
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Golf Course on Flood Plain by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
Golf course built on the Carmel River flood plain.
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Terrace by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
The scarp marking a subtle change in elevation along these bushes delineates the boundary between the flood plain on the right and the fluvial terrace on the left.
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Fluvial Terrace by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
This flat area is a fluvial terrace, a former flood plain of the Carmel River. Since eroding this flat planar area and depositing flood plain sediments upon it, the Carmel River has eroded to a slightly lower elevation, leaving this older flood plain to become a fluvial (river) terrace.
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Cut bank erosion by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
The Carmel River has eroded into the hillside here on the outside of one of its meanders as it flows through the Carmel Valley.
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Carmel River by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
The Carmel river flows though this wooded channel.
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Carmel River by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
Carmel River is visible through the trees.
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Ancient Landslide by ahochstaedter from the GigaPan Carmel Valley View by ahochstaedter
Golf course and housing developments built on ancient landslide deposits.
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The Red Banks by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
The Red Banks are a prominant landmark located on lookers right of the Avalanche Gully climbing route.
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Avalanche Deposit by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
Hummocky topography of the avalanche deposit from ancestral Mt Shasta, deposited some 300- 350 thousand years ago. BIG!
Shasta Valley lies to the left.
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Dillar Canyon by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
A very wild looking place.
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Shastina Summit by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
All of the eruptive products associated with Shastina erupted within a few hundred years about 9500 years ago.
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Not the Whitney Glacier by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
The Whitney Glacier lies just over this ridge.
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Misery Hill by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
An eruptive vent seperate from the summit cone. Misery Hill is so named by climbers who must climb its 1000 foot flanks just before reaching the summit of Mt Shasta.
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The West Face by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
A very nice ski in the late spring and early summer.
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Hidden Valley by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
Favorite camping spot for those climbing the West Face route to the summit of Shasta.
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Casaval Ridge by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
Casaval Ridge separates Avalanch Gulch (behind and to the right) from Hidden Valley (in front and to the left).
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Lake Shastina by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
Lake Shastina is a reservoir nestled in the hummocky topography of avalanche from ansestral Mt Shasta. I've got a Gigapan from this site as well.
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Black Butte Center for Railroad Culture by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
www.bbcrc.org
/From their website:
The Black Butte Center for Railroad Culture was founded in 2008 as a way to support and develop a community-building institution focused on railroad culture in the western United States. The BBCRC is located on the site of a long-abandoned junkyard amid several acres of forest, chaparral, and wetlands directly adjacent to Black Butte Siding, the junction of the Union Pacific and Central Oregon and Pacific railroads right on the southeast edge of Weed, California at Milepost 345. Directly across from our site is the Black Butte water tank, a historic 1926 steam-era structure. Mt. Shasta towers a few miles to the east and Black Butte, a 6300' volcanic cinder cone, is just two miles to our southeast.0 comments
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Weed by ahochstaedter from the GigaPan Mt Shasta from Black Butte by ahochstaedter
The sign at the entrance to Weed reads "Weed like to Welcome You". Weed is also the home of the Hi-Lo Cafe, the best restaurant in town. www.tripadvisor.com/Restaurant_Review-g33245-d1013258-Reviews-Hi_Lo_Cafe-Weed_California.html

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Normal Fault by ahochstaedter from the GigaPan Deer Mountain Tephra Unconformity by ahochstaedter
A small amount of offset has occured along this apparent normal fault.
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Angular Unconformity by ahochstaedter from the GigaPan Deer Mountain Tephra Unconformity by ahochstaedter
This angular unconformity probably does not reflect a long passage of time.
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Spheriodal Weathering by ahochstaedter from the GigaPan Elephant Rocks, MO by ahochstaedter
These boulders are core stones remaining from an extended period of spheroidal weathering.
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Weathering Pans by ahochstaedter from the GigaPan Elephant Rocks, MO by ahochstaedter
Chemical weathering associated with pooled water at the edges of the pan are thought to form weathering pans. The bottom of the these pans is often filled with grus, grains of quartz and feldspar.
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Fractures by ahochstaedter from the GigaPan El Capitan by ahochstaedter
More fractures. You can almost hear the crack of the rock.
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