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Good meeting spot with big parking lot. Park in the graveled area.

The site consists of one human figure geoglyph and a few other recognizable des. The human figure with a spear in his hand, fish swimming below the water, and the sun shining above, creates a distinct image.

According to Native Americans, this image may represent their Creator carving the Colorado River with his spear. Geoglyphs new des moines sensual massage difficult to date, so archaeologists have no way of knowing their age.

An interpretive at the site provides additional information. There are 18 motels and a of restaurants in the Blythe area.

Saturday night campers - dry camp, no facilities, no fees. Participants will be responsible for their own motel accommodations and meals Beautiful couple searching online dating Casper lunches, 1 dinner, 1 breakfast, snacks, and water drinks.

Overview of Northern Plomosa geology from the parking lot. Stop 2.

Barite veins and disseminated manganese mineralization in Miocene conglomerate. Stop 3.

Stop 4. Stratigraphy of tiltblocks about the Plomosa detachment fault, and the appearance of mylonitic debris derived from the footwall block.

Stop 5. Stratigraphy of the base of the Miocene section — basal conglomerate grading up into sand, silt, and limestone.

Stop 6. Rock-avalanche breccia derived from metamorphic rocks that were subjected to hydrothermal alteration and later metamorphism, producing unusual mineral assemblages including svanbergite.

Hart Mine Wash — look at Bouse stratigraphy that reflects abrupt submergence of alluvial fans. Transgressive sequence includes nearshore carbonate facies like the white bathtub ring around Lake Meadoffshore siltstone Old Falmouth Massachusetts granny sluts clay.

Discussion: paleontology, detrital zircon geochronology, and reason for inundation. More Bouse Formation in the Cibola area — stop to be determined.

Return to Blythe, take I back into Arizona, turn off of I at Tom Wells Road, go south to areas of historic manganese mining Metate district where manganese oxides fill fractures and pen spaces in rubble beneath Pliocene Bouse carbonates, and also affect the carbonates.