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Here's where things get interesting: The 7.1-magnitude earthquake rattled a fault within the Little Lake fault zone — cracks in this spot near Ridgecrest tend to run in the northwest-southeast direction.
"The earthquake on Thursday [July 4] was more complex. And part of that smaller event happened on an unmapped fault that trends NE-SW. This is very interesting geologically, said Michele Cooke, a geoscientist at the University of Massachusetts - Amherst. "We don't have a lot of earthquakes in our record that show simultaneous slip on two perpendicular faults."
"This area does not fit the textbook picture of sides of a plate sliding past one another," and instead the relatively short faults criss-cross each other on more than one plane. (In fact, the 6.4-magnitude quake began at a depth of 6.6 miles, or 10.7 km, while the epicenter of the bigger quake was much deeper, some 10.6 miles, or 17 km, beneath the surfac
originally posted by: jeramie
a reply to: KansasGirl
They look like tumbleweeds, which are very common around here, but I don't know why they look so black and gray in the picture.
originally posted by: KansasGirl
In the picture, what's with the black and gray scrubs/shrubs?
Coso Rock Art District, containing the Big and Little Petroglyph Canyons, is a rock art site containing over 100,000 Paleo-Indian and/or Native American Petroglyphs.[1] The Coso Range is between the Sierra Nevada and the Argus Range. Indian Wells Valley lies to the south of this location.
This north-south trending range of about 400 square miles (1,000 km2) consists of rhyolitic domes and outcrops of volcanic rock. Also known as Little Petroglyph Canyon and Sand Tanks, Renegade Canyon is but one of several major canyons in the Coso Range, each hosting thousands of petroglyphs (other locations include Haiwee Springs, Dead End Canyon, and Sheep Canyon).
The majority of the Coso Range images fall into one of six categories: bighorn sheep, entopic images, anthropomorphic or human-like figures (including animal-human figures known as pattern-bodied anthopomorphs), other animals, weapons & tools, and "medicine bag" images. Most of the Coso Range is on the Naval Air Weapons Station China Lake, where visitation is restricted, vandalism is low, and preservation is most likely.
"emphasis mine"
originally posted by: misskat1
This area is very close to a geothermal pumping site. They pump water into the hot magma which causes steam to run the turbines that make electric for the area.
originally posted by: misskat1
This area is very close to a geothermal pumping site. They pump water into the hot magma which causes steam to run the turbines that make electric for the area.
Abastract
Geothermal areas are long recognized to be susceptible to remote earthquake triggering, probably due to the high seismicity rates and presence of geothermal fluids. However, anthropogenic injection and extraction activity may alter the stress state and fluid flow within the geothermal fields.
Here we examine the remote triggering phenomena in the Coso geothermal field and its surrounding areas to assess possible anthropogenic effects. We find that triggered earthquakes are absent within the geothermal field but occur in the surrounding areas. Similar observation is also found in the Salton Sea geothermal field.
We hypothesize that continuous geothermal operation has eliminated any significant differential pore pressure between fractures inside the geothermal field through flushing geothermal precipitations and sediments out of clogged fractures. To test this hypothesis, we analyze the pore-pressure-driven earthquake swarms, and they are found to occur outside or on the periphery of the geothermal production field.
Therefore, our results suggest that the geothermal operation has changed the subsurface fracture network, and differential pore pressure is the primary controlling factor of remote triggering in geothermal fields.
3.2. Study of Pore-Pressure-Driven Swarms
Our results confirm that areas in the vicinity of but outside the producing geothermal field are susceptible to remote triggering. Here, however, we have clearly established the absence of remote triggering inside the CGF production area. Before we attempt to estimate the stress state, we first test the second kind of remote triggering model.
Among the numerous fluid-related triggering models, the fracture unclogging model can be uniquely applied to geothermal fields in that the geothermal mineral precipitation and sediments lead to clogged fractures, which results in differential pore pressure within fracture network [Brodsky et al., 2003; Brodsky and Prejean, 2005].
This fracture unclogging model has also been used as one of the explanations to the absence of remote triggering in Japan [Harrington and Brodsky, 2006]. We hypothesize that the continuous injection and extraction of geothermal fluid within the reservoir can disturb the clogged fracture and flush the blockages from fractures, which prevents the formation of differential pore pressure, while the fractures in natural settings remain clogged.
originally posted by: KansasGirl
In the picture, what's with the black and gray scrubs/shrubs?
originally posted by: ownbestenemy
a reply to: Observationalist
Good thing we have 4 billion years of geology to catch up on then.
Just because modern tectonics isnt aware doesn't mean its out of the ordinary. I know you were just making a aimilar observation so dont take my reply as snark.