Blue goo is a sticky, plasticky, blueish-grey, clay-textured soil derived from a highly weathered serpentinite mélange. ^{[1] [2]} The name derives from the soil's color; a result of undergoing anaerobic conditions and becoming gleyed. ^[3] A greyer variation is called "grey goo". ^[2] Blue goo is primarily found along the Northern California coast. ^[2]

Parent material

The Franciscan Complex is the bedrock from which blue goo is derived. ^[1] It stretches along the coastline from Central California up to Southern Oregon and contains sheared materials from both the Pacific and North American Plates that have accumulated in the accretionary wedge. ^[1]

The rock types that produce blue goo include: greenstones, cherts, basalts, shales, sandstones, schists, and serpenitites. ^{[1] [2] [4] [5] [6]} These materials mixed together forming a "plum pudding" or a mélange. ^{[1] [2]} This mélange decomposed through weathering to form blue goo. ^[7]

Common features

Clay soils like blue goo have the highest water-holding capacity when compared with other soils, giving them a low draining capacity. ^[3] This kind of habitat is unsuitable for most plants, ^[3] but the Northern California coastline maintains high levels of vegetation year round.

Due to blue goo's clayey texture, it slips when overly saturated. ^[6] This slippage is increased in heavy rainfall areas and in shallow soils; deep soils have more total pore space and are not as prone to slippage. ^[3] These features contribute to the landslide-ridden environments found along the Northern Californian coast. ^{[5] [6]}

Locations

The Franciscan Complex, from which blue goo is derived, extends from Central California up the coast through parts of Southern Oregon. ^[1] But blue goo has only been found in two Northern Californian regions located in Humboldt County: the Trinidad region and the Orick region. Blue goo is thought to also be found in the Eel River region and along the Southern Oregon coastline.

References