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Western Sloughs - Global Warming Traditional Cache

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el Jim: Out of Service

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Hidden : 10/21/2006
Difficulty:
1 out of 5
Terrain:
1.5 out of 5

Size: Size:   regular (regular)

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Geocache Description:

The Western Sloughs – a 20,000 year History

Please do not leave the trail. You do not have to cross the fence to find the cache. Thanks


Special Note - Before we get started... you will notice that dogs are not allowed at this cache site. The sign posted nearby does not explain the reasoning.

Dogs

Many of Monterey County's nearby beaches are closed to our K9 friends. This is because Snowy Plovers live here and uncontrolled dogs can be disruptive to the endangered Snowy Plover nesting ground. A Snowy Plover will permanently abandon a nest leaving unhatched eggs if disturbed.

Now, back to our mission...

You are standing between the Pacific Ocean and Bennett Slough. It is cold and there is ice and snow around you. It is 20,000 Years Before Present (YBP). The sea level stands nearly 400 feet below the point where it will stand in the year 2009 AD. Monterey’s shoreline is 5-8 miles west of your present location, except where the Monterey submarine canyon approaches much closer to current shoreline and the Elkhorn channel. Elkhorn is a freshwater river. Moro Cojo also a freshwater system.



Photography by Karen1327

18,000 YBP - Two thousand years later, Ice sheets begin melting and seawater rises rapidly. This pattern continues for ~ 12,000 years, with some variation in sea level rise over time.

10,000 YBP - Ocean water enters river channels on the California coast, including Elkhorn Slough. Rate of sea-level rise exceeds rate of sediment accumulation in these tidal inlets. Oysters colonize mouth of Elkhorn Slough.

8,000 YBP - Native Americans arrive in Elkhorn Slough region. Archaeological site includes fossils of northern seal pups, indicating a local rookery, perhaps on the Moss Landing spit. Humans may have driven this species to local extinction.

6,000 YBP - Near Hudson’s Landing, where Schwartz found salt marsh beginning to colonize landward edge, West found ditchgrass (a pondweed which thrives in salinities between 9 and 20 ppt), willows, cattails, and pickleweed appearing to coexist; suggests a brackish environment in the upper slough. West 1988 Mouth of Elkhorn Slough becoming narrower, based on data from oyster fossils. Oysters and clams colonize Bennett Slough.

4,000 YBP - Elkhorn Slough salt marsh approximately half the extent of what it will be by early 1900s; benthic foraminifers found in this marsh layer indicate assemblage resembling ones found today in Elkhorn Slough. Broad mudflats flank main channel.

3,000 YBP - Native Americans occupy a site near the mouth of Elkhorn Slough (this site had been occupied in the past, from 8,000 to 6,500 YBP). Archaeological data reveal this group regularly hunts sea otters, fur seals, and harbor seals. Less frequently, Stellar sea lions and California sea lion bones appear in midden. Otters and seals may have been found in the local sloughs or in Monterey Bay. Sea lions were probably restricted to the bay.

2,000 YBP - McClusky Slough dominated by salt marsh, but beginning to diminish in size. Broad salt marshes exist throughout Elkhorn Slough. Sedges and cattails disappear at Hudson’s Landing and are replaced with combination of ditchgrass and pickleweed, indicating a brackish environment in upper slough. Clay deposited at mouth of Elkhorn Slough – indicating a relatively quiet water estuary with, perhaps, an indirect opening to the sea.

1769 AD - First European account of north Monterey Co wetlands. Father Crespi and Miguel Costanso place the mouth of the Salinas River near Moss Landing, and describe the river as an estuary that is tidally influenced and brackish to almost the Blanco Crossing, approximately 9 miles southeast of Moss Landing. Near its mouth this estuary is “very full” and deep

1830s - Maps made of Mexican land grants show Elkhorn Slough and Moro Cojo as “esteros’ with salt ponds. They share a mouth with the Salinas, and the location of this mouth is variable. Diseños The Salinas River “runs almost dry” in the summer, but becomes “impassible” during the rainy season, and it often overflows most of the lower Salinas plains in winter. One resident on the lower Tembladero has to be rescued by boat from the roof of his adobe – he “disliked saltwater . . .[and he feared he] might have to take a cruise on [the adobe’s roof] in Monterey bay, by way of the Salinas river against his will.”

1850s - The sloughs near the mouth of the Salinas River are deep enough “to float a medium sized vessel to the Bay of Monterey,” although sand bars at the river’s mouth are a major obstacle in 1854. A State contracted geologist suggests building a breakwater at the Salinas river mouth to improve the area and make these waters navigable, especially since the State will end up with jurisdiction of these “over-flowed and saline lands.”

1872 - Railroad constructed in Elkhorn Slough, restricting tidal flow to many of the eastern wetlands.

1876 - A passenger on the train through Elkhorn Slough remarks on its “worthless salt marsh lands” and its hundreds of pelicans, and great flocks of ducks, gulls, and other birds.

1875 - Reclamation of local tide lands begins. In October 1875, “a levee has been thrown up to a height of five feet [at mid-Moro Cojo]. . .extending from the higher land lying west of the slough to the railroad bridge, a distance of half a mile. . . We think [it will] effectually protect from the tide about 120 acres of land that otherwise would be profitless for any purpose. . . Mr. Castro intends doing further work of this kind where practicable. . .”

1906 - Directly across the slough you will find the Pacific Coast Steamship Company building which was built in 1906 following the San Francisco earthquake. This property has many well-known names associated with it. The simple colonial revival style is in vernacular pyramid cottage form used just after the turn of the century mostly in "company towns". The porch front is simple Tuscan order. The two downstairs front windows are Queen Anne cottage style. The simple fireplaces include bricks salvaged from damaged buildings in the 1906 earthquake made by the Sante Fe masonry. This building has been fully renovated and recently opened as a bed and breakfast, The Captain's Inn by Captain Yohn and Melanie Gideon. The effort to save this building has been awarded a historic preservation award from the Moss Landing Chamber of Commerce.

2010 - You find a Geocache on this spot.

Thank you - Andrea Woolfolk, National Estuarine Research Reserve

CONGRATULATIONS Indigo Moon 10 - "Quick find on a BEAUTIFUL autumn day."

Additional Hints (Decrypt)

Frrx arne gur srapr. Lbh jvyy abg unir gb yrnir gur cngu be pebff gur srapr. N pnzb wne uvqqra ol ornpu qevsgjbbq.

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)