Friday, November 2, 2012

[Geology2] Asteroid Belts of Just the Right Size Are Friendly to Life





This illustration shows three possible scenarios for the evolution of asteroid belts. In the top panel, a Jupiter-size planet migrates through the asteroid belt, scattering material and inhibiting the formation of life on planets. The second scenario shows our solar-system model: a Jupiter-size planet that moves slightly inward but is just outside the asteroid belt. In the third illustration, a large planet does not migrate at all, creating a massive asteroid belt. Material from the hefty asteroid belt would bombard planets, possibly preventing life from evolving. (Credit: Illustration Credit: NASA, ESA, and A. Feild (STScI) / Science Credit: NASA, ESA, R. Martin and M. Livio (STScI))

Asteroid Belts of Just the Right Size Are Friendly to Life

ScienceDaily (Nov. 1, 2012) — Solar systems with life-bearing planets may be rare if they are dependent on the presence of asteroid belts of just the right mass, according to a study by Rebecca Martin, a NASA Sagan Fellow from the University of Colorado in Boulder, and astronomer Mario Livio of the Space Telescope Science Institute in Baltimore, Md.

They suggest that the size and location of an asteroid belt, shaped by the evolution of the Sun's protoplanetary disk and by the gravitational influence of a nearby giant Jupiter-like planet, may determine whether complex life will evolve on an Earth-like planet.

This might sound surprising because asteroids are considered a nuisance due to their potential to impact Earth and trigger mass extinctions. But an emerging view proposes that asteroid collisions with planets may provide a boost to the birth and evolution of complex life.

Asteroids may have delivered water and organic compounds to the early Earth. According to the theory of punctuated equilibrium, occasional asteroid impacts might accelerate the rate of biological evolution by disrupting a planet's environment to the point where species must try new adaptation strategies.

The astronomers based their conclusion on an analysis of theoretical models and archival observations of extrasolar Jupiter-sized planets and debris disks around young stars. "Our study shows that only a tiny fraction of planetary systems observed to date seem to have giant planets in the right location to produce an asteroid belt of the appropriate size, offering the potential for life on a nearby rocky planet," said Martin, the study's lead author. "Our study suggests that our solar system may be rather special."

The findings will appear today in the Monthly Notices of the Royal Astronomical Society: Letters (published by Oxford University Press).

Martin and Livio suggest that the location of an asteroid belt relative to a Jupiter-like planet is not an accident. The asteroid belt in our solar system, located between Mars and Jupiter, is a region of millions of space rocks that sits near the "snow line," which marks the border of a cold region where volatile material such as water ice are far enough from the Sun to remain intact. At the time when the giant planets in our solar system were forming, the region just beyond the snow line contained a dense mix of ices, rock, and metals that provided enough material to build giant planets like Jupiter.

When Jupiter formed just beyond the snow line, its powerful gravity prevented nearby material inside its orbit from coalescing and building planets. Instead, Jupiter's influence caused the material to collide and break apart. These fragmented rocks settled into an asteroid belt around the Sun.

"To have such ideal conditions you need a giant planet like Jupiter that is just outside the asteroid belt [and] that migrated a little bit, but not through the belt," Livio explained. "If a large planet like Jupiter migrates through the belt, it would scatter the material. If, on the other hand, a large planet did not migrate at all, that, too, is not good because the asteroid belt would be too massive. There would be so much bombardment from asteroids that life may never evolve."

In fact, during the solar system's infancy, the asteroid belt probably had enough material to make another Earth, but Jupiter's presence and its small migration towards the Sun caused some of the material to scatter. Today, the asteroid belt contains less than one percent of its original mass. Using our solar system as a model, Martin and Livio proposed that asteroid belts in other solar systems would always be located approximately at the snow line. To test their proposal, Martin and Livio created models of protoplanetary disks around young stars and calculated the location of the snow line in those disks based on the mass of the central star.

They then looked at all the existing space-based infrared observations from NASA's Spitzer Space Telescope of 90 stars having warm dust, which could indicate the presence of an asteroid belt-like structure. The temperature of the warm dust was consistent with that of the snow line. "The warm dust falls right onto our calculated snow lines, so the observations are consistent with our predictions," Martin said.

The duo then studied observations of the 520 giant planets found outside our solar system. Only 19 of them reside outside the snow line, suggesting that most of the giant planets that may have formed outside the snowline have migrated too far inward to preserve the kind of slightly-dispersed asteroid belt needed to foster enhanced evolution of life on an Earth-like planet near the belt. Apparently, less than four percent of the observed systems may actually harbor such a compact asteroid belt.

"Based on our scenario, we should concentrate our efforts to look for complex life in systems that have a giant planet outside of the snow line," Livio said.



Story Source:

The above story is reprinted from materials provided by Space Telescope Science Institute (STScI).

Note: Materials may be edited for content and length. For further information, please contact the source cited above.



Space Telescope Science Institute (STScI) (2012, November 1). Asteroid belts of just the right size are friendly to life. ScienceDaily. Retrieved November 2, 2012, from http://www.sciencedaily.com­ /releases/2012/11/121101131208.htm
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[californiadisasters] On This Date In CA Weather History (November 2)



2011: Strong offshore winds hit 81 mph at Fremont Canyon.
Sustained winds were between 40 and 50 mph.

2002:
Dense fog in south LA led to two pileups on the 710 freeway involving 194 vehicles.
There were no deaths and 41 injuries.

2002: October passed with dry heat and no precipitation across the North State.
Leaves fell but not the rain.
Not a drop of rain fell in October that usually brings the season's first downpours.

2002: The morning low temperature at Lovelock, NV was -1°.

1997: It was 97° in Riverside, the highest temperature on record for November.
This also occurred on 11.21.1924.
It was 98° in Escondido, also the highest temperature on record for November.
This also occurred on 11.10.1956.

1993: Santa Ana winds gusted to over 60 mph on this day through 11.4.
The Old Topanga fire burned from Calabasas to the ocean consuming hundreds of homes.

1987: In the aftermath of the worst forest fires to hit the north state in decades, government agencies scrambled to stem the effects and get the forests on the road to recovery.
At stake were the health of fisheries in rivers and streams far from where the fires burned and the productivity of timberlands for years to come.

1983: Highest minimum temperature records were set each day in San Diego for eight consecutive days, starting on 10.26 and ending on this day.

1977: It was 74° in Big Bear Lake, the highest temperature on record for November.
This also occurred on 11.4.1988 and 11.4.1984.

1966: San Luis Obispo hit 98°, a record high for the month.

1966: It was 80° in Idyllwild, the highest temperature on record for November.
This also occurred on 11.1.1999, 11.13.1999, 11.4.1980, and 11.12.1967.

1959: This was the sunniest November on record in Fresno, with a total of 302 hours and 50 seconds of sunshine – 99% of the total amount possible.

1935: 12" of snow fell at Sierraville, CA and Carson City, NV, with 11.6" of snow being reported at Reno, NV.

Source: NWS Hanford, Reno, & San Diego and the Redding Record-Searchlight


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Re: [Geology2] With new geology map, Idaho rocks



 


With new geology map, Idaho rocks

Published: October 17, 2012 


Geologic_Map_of_Idaho_WEB_V.JPG

The new geologic map of Idaho.

  • Get the map

    The map costs $20, plus shipping and handling.

    To order, visit the IGS website at www.idahogeology.org.


Geological history will be on vivid display Friday, when the Idaho Geological Survey unveils "a piece of art," Director Roy Breckenridge said.

The big map's colors are used to identify different types of rocks, as well as rocks of different ages. The colors are draped over a shaded relief map that highlights mountain slopes and other surface features in sharp detail.

"You don't have to be a geologist to be drawn to it. It encourages inquiry and discovery of the land we live in," Breckenridge said.

The map illustrates Idaho's multibillion-year rock record, a grand narrative that includes rifting and colliding continents, global catastrophes, rising and falling sea levels, and eons of slow, steady erosion.

A dark charcoal-brown is used to identify the oldest rocks in the state, including a relatively small plug of 2.7 billion-year-old gneiss in the Pioneer Mountains southwest of Mackay, and a large swath of 2.67 billion-year-old granitic gneiss, schist and quartzite located between Bovill and the St. Joe River.

They date from a time when modern-style plate tectonics might not have operated, when Earth's mantle was much hotter and when continental crust might have been created in enormous melting events.

At the opposite end of the geological time scale are the roughly 15,000- to 17,000-year-old Lake Missoula and Lake Bonneville flood deposits. They're found in the Rathdrum Prairie and along the Snake and lower Clearwater River drainages, marked in yellow.

Idaho rocks haven't changed much since the last statewide map was produced, but a substantial amount of new mapping has been done since then. The work provided details in areas that were previously just conjecture.

Age-dating technology has also improved dramatically, so the new map provides more accurate information about formation.

THE STORY OF ROCKS

Keegan Schmidt, a geology professor at Lewis-Clark State College who has worked on a number of IGS mapping projects, said geological maps tell a story.

"It starts the first day at the first outcrop," Schmidt said. "You walk up to a rock and mark its location on a map. That rock represents an event."

If it's a type of lava, he said, then you know there was a volcanic eruption. If it's a limestone, there was deposition in a marine or lake environment. A sandstone could be anything from a flood to a beach to a wind-blown dune, but features within the rock will likely distinguish which it is.

"Then you move on to the next rock that's different," Schmidt said. "That represents a different event, so you have to determine the relationship between the two."

Rocks can be folded and faulted as well, he said, so you have to consider the sequence of events. Which rock came first? Was there a time gap before the second rock? When and how were they deformed?

"As you walk along, you're filling in the story," Schmidt said.

USING THE MAP

The practical applications of the story include protecting groundwater, identifying minerals and spotting hazards.

Near Riggins, for example, IGS has done detailed mapping to help identify specific rock units that are causing landslide problems along the U.S. Highway 95 corridor.

The U.S. Geological Survey conducted a number of large mapping projects in Idaho in the '80s and early '90s. And over the past decade or so, IGS has produced more than 160 maps under the auspices of the StateMap project.

Those large-scale maps provide the detailed information needed by geotechnical engineers, industry officials, resource managers and government agencies, he said. They served as the foundation for the new state map.

The Idaho Geological Survey, created in 1919, published its first geological survey map in 1947, followed by the 1978 map, and now by the latest version.

"Geological maps have a certain useful life," Lewis said. "We used to say they were good for 30 years or so, but with the advances in technology I'm beginning to wonder if it's shorter than that. It's a moving target. You can never say you have it all mapped and it's time to go home. This is just a snapshot in time."

http://www.idahostatesman.com/2012/10/17/2313018/with-new-geology-map-idaho-rocks.html
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Thursday, November 1, 2012

[Geology2] With new geology map, Idaho rocks




With new geology map, Idaho rocks

Published: October 17, 2012 


Geologic_Map_of_Idaho_WEB_V.JPG

The new geologic map of Idaho.

Geological history will be on vivid display Friday, when the Idaho Geological Survey unveils "a piece of art," Director Roy Breckenridge said.

The big map's colors are used to identify different types of rocks, as well as rocks of different ages. The colors are draped over a shaded relief map that highlights mountain slopes and other surface features in sharp detail.

"You don't have to be a geologist to be drawn to it. It encourages inquiry and discovery of the land we live in," Breckenridge said.

The map illustrates Idaho's multibillion-year rock record, a grand narrative that includes rifting and colliding continents, global catastrophes, rising and falling sea levels, and eons of slow, steady erosion.

A dark charcoal-brown is used to identify the oldest rocks in the state, including a relatively small plug of 2.7 billion-year-old gneiss in the Pioneer Mountains southwest of Mackay, and a large swath of 2.67 billion-year-old granitic gneiss, schist and quartzite located between Bovill and the St. Joe River.

They date from a time when modern-style plate tectonics might not have operated, when Earth's mantle was much hotter and when continental crust might have been created in enormous melting events.

At the opposite end of the geological time scale are the roughly 15,000- to 17,000-year-old Lake Missoula and Lake Bonneville flood deposits. They're found in the Rathdrum Prairie and along the Snake and lower Clearwater River drainages, marked in yellow.

Idaho rocks haven't changed much since the last statewide map was produced, but a substantial amount of new mapping has been done since then. The work provided details in areas that were previously just conjecture.

Age-dating technology has also improved dramatically, so the new map provides more accurate information about formation.

THE STORY OF ROCKS

Keegan Schmidt, a geology professor at Lewis-Clark State College who has worked on a number of IGS mapping projects, said geological maps tell a story.

"It starts the first day at the first outcrop," Schmidt said. "You walk up to a rock and mark its location on a map. That rock represents an event."

If it's a type of lava, he said, then you know there was a volcanic eruption. If it's a limestone, there was deposition in a marine or lake environment. A sandstone could be anything from a flood to a beach to a wind-blown dune, but features within the rock will likely distinguish which it is.

"Then you move on to the next rock that's different," Schmidt said. "That represents a different event, so you have to determine the relationship between the two."

Rocks can be folded and faulted as well, he said, so you have to consider the sequence of events. Which rock came first? Was there a time gap before the second rock? When and how were they deformed?

"As you walk along, you're filling in the story," Schmidt said.

USING THE MAP

The practical applications of the story include protecting groundwater, identifying minerals and spotting hazards.

Near Riggins, for example, IGS has done detailed mapping to help identify specific rock units that are causing landslide problems along the U.S. Highway 95 corridor.

The U.S. Geological Survey conducted a number of large mapping projects in Idaho in the '80s and early '90s. And over the past decade or so, IGS has produced more than 160 maps under the auspices of the StateMap project.

Those large-scale maps provide the detailed information needed by geotechnical engineers, industry officials, resource managers and government agencies, he said. They served as the foundation for the new state map.

The Idaho Geological Survey, created in 1919, published its first geological survey map in 1947, followed by the 1978 map, and now by the latest version.

"Geological maps have a certain useful life," Lewis said. "We used to say they were good for 30 years or so, but with the advances in technology I'm beginning to wonder if it's shorter than that. It's a moving target. You can never say you have it all mapped and it's time to go home. This is just a snapshot in time."

http://www.idahostatesman.com/2012/10/17/2313018/with-new-geology-map-idaho-rocks.html
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[Volcano_Vista_HS] Hawks Football--SENIOR NIGHT vs. the Cleveland Storm



Volcano Vista Hawks Football
Senior Night

Friday, November 2, 2012

6:15 PM
Game vs. Cleveland High School at 7 PM

Milne Stadium 

We will be presenting the 2013 Seniors at 6:15 pm right before the Hawks/Storm football game.

We would like for all their fans to attend and show their appreciation to the Seniors for all their hard work, dedication, and commitment they have given to the Volcano Vista Football Program!

Bring your friends, your co-workers, your neighbors, your family...just bring everyone and show the Seniors just how much we love them!



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[Geology2] Tabletop Fault Model Reveals Why Some Earthquakes Result in Faster Shaking





Gregory McLaskey (L) and Steven Glaser examine a tabletop model of a fault at UC Berkeley. (Credit: Preston Davis photo)

Tabletop Fault Model Reveals Why Some Earthquakes Result in Faster Shaking

ScienceDaily (Oct. 31, 2012) — The more time it takes for an earthquake fault to heal, the faster the shake it will produce when it finally ruptures, according to a new study by engineers at the University of California, Berkeley, who conducted their work using a tabletop model of a quake fault.

"The high frequency waves of an earthquake -- the kind that produces the rapid jolts -- are not well understood because they are more difficult to measure and more difficult to model," said study lead author Gregory McLaskey, a former UC Berkeley Ph.D. student in civil and environmental engineering. "But those high frequency waves are what matter most when it comes to bringing down buildings, roads and bridges, so it's important for us to understand them."

While the study, to be published in the Nov. 1 issue of the journal Nature and funded by the National Science Foundation, does nothing to bring scientists closer to predicting when the next big one will hit, the findings could help engineers better assess the vulnerabilities of buildings, bridges and other structures when a fault does rupture.

"The experiment in our lab allows us to consider how long a fault has healed and more accurately predict the type of shaking that would occur when it ruptures," said Steven Glaser, UC Berkeley professor of civil and environmental engineering and principal investigator of the study. "That's important in improving building designs and developing plans to mitigate for possible damage."

To create a fault model, the researchers placed a Plexiglas slider block against a larger base plate and equipped the system with sensors. The design allowed the researchers to isolate the physical and mechanical factors, such as friction, that influence how the ground will shake when a fault ruptures.

It would be impossible to do such a detailed study on faults that lie several miles below the surface of the ground, the authors said. And current instruments are generally unable to accurately measure waves at frequencies higher than approximately 100 Hertz because they get absorbed by the earth.

"There are many people studying the properties of friction in the lab, and there are many others studying the ground motion of earthquakes in the field by measuring the waves generated when a fault ruptures," said McLaskey. "What this study does for the first time is link those two phenomena. It's the first clear comparison between real earthquakes and lab quakes."

Noting that fault surfaces are not smooth, the researchers roughened the surface of the Plexiglas used in the lab's model.

"It's like putting two mountain ranges together, and only the tallest peaks are touching," said McLaskey, who is now a postdoctoral researcher with the U.S. Geological Survey in Menlo Park.

As the sides "heal" and press together, the researchers found that individual contact points slip and transfer the resulting energy to other contact points.

"As the pressing continues and more contacts slip, the stress is transferred to other contact points in a chain reaction until even the strongest contacts fail, releasing the stored energy as an earthquake," said Glaser. "The longer the fault healed before rupture, the more rapidly the surface vibrated."

"It is elegant work," said seismologist John Vidale, a professor at the University of Washington who was not associated with the study. "The point that more healed faults can be more destructive is dismaying. It may not be enough to locate faults to assess danger, but rather knowing their history, which is often unknowable, that is key to fully assessing their threat."

Glaser and McLaskey teamed up with Amanda Thomas, a UC Berkeley graduate student in earth and planetary sciences, and Robert Nadeau, a research scientist at the Berkeley Seismological Laboratory, to confirm that their lab scenarios played out in the field. The researchers used records of repeating earthquakes along the San Andreas fault that Nadeau developed and maintained. The data were from Parkfield, Calif., an area which has experienced a series of magnitude 6.0 earthquakes two to three decades apart over the past 150 years.

Thomas and McLaskey explored the records of very small, otherwise identically repeating earthquakes at Parkfield to show that the quakes produced shaking patterns that changed depending on the time span since the last event, just as predicted by the lab experiments.

In the years after a magnitude 6.0 earthquake hit Parkfield in 2004, the small repeating earthquakes recurred more frequently on the same fault patches.

"Immediately after the 2004 Parkfield earthquake, many nearby earthquakes that normally recurred months or years apart instead repeated once every few days before decaying back to their normal rates," said Thomas. "Measurements of the ground motion generated from each of the small earthquakes confirmed that the shaking is faster when the time from the last rupture increases. This provided an excellent opportunity to verify that ground motions observed on natural faults are similar to those observed in the laboratory, suggesting that a common underlying mechanism -- fault healing -- may be responsible for both."

Understanding how forcefully the ground will move when an earthquake hits has been one of the biggest challenges in earthquake science.

"What makes this study special is the combination of lab work and observations in the field," added Roland Burgmann, a UC Berkeley professor of earth and planetary sciences who reviewed the study but did not participate in the research. "This study tells us something fundamental about how earthquake faults evolve. And the study suggests that, in fact, the lab setting is able to capture some of those processes correctly."

Glaser said the next steps in his lab involve measuring the seismic energy that comes from the movement of the individual contact points in the model fault to more precisely map the distribution of stress and how it changes in the run-up to a laboratory earthquake event.



Story Source:

The above story is reprinted from materials provided by University of California - Berkeley. The original article was written by Sarah Yang.

Note: Materials may be edited for content and length. For further information, please contact the source cited above.


Journal Reference:

  1. Gregory C. McLaskey, Amanda M. Thomas, Steven D. Glaser and Robert M. Nadeau. Fault healing promotes high-frequency earthquakes in laboratory experiments and on natural faults. Nature, October 31, 2012

University of California - Berkeley (2012, October 31). Tabletop fault model reveals why some earthquakes result in faster shaking. ScienceDaily. Retrieved November 1, 2012, from http://www.sciencedaily.com­ /releases/2012/10/121031141854.htm
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[californiadisasters] South Ops News & Notes Update (11/01/12-8AM)



Date

Time

News and Notes

11/01

0800

Large fire potential will be low today due to cool and humid conditions.  Again, today's precipitation over the central part of the state is expected to be light and will not be sufficient to change fuel conditions appreciably in the long term.

Source: http://gacc.nifc.gov/oscc/predictive/intelligence/news_notes/index.htm

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