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We can use the following three InSAR images as a timeline for the uplift observed from 1997 through 2003. In the images, each full spectrum of color (from red to purple) represents about 28 mm (1 inch) of uplift. In the first image, rings of color indicate an uplifted area (approximately 35 km by 40 km or 22 x 25 miles) centered on the northern caldera rim. The uplift is in a different location from previously observed deformation episodes at Yellowstone (Wicks, et al., 1998). In the second image, from the fall of 2001, we see a smaller area (approximately 30 km by 20 km) with rings of color indicating that the uplift event is continuing.
YELLOWSTONE VOLCANO OBSERVATORY MONTHLY UPDATE
Tuesday, April 1, 2014 11:57 AM MDT (Tuesday, April 1, 2014 17:57 UTC)
YELLOWSTONE VOLCANO (VNUM #325010)
44°25'48" N 110°40'12" W, Summit Elevation 9203 ft (2805 m)
Current Volcano Alert Level: NORMAL
Current Aviation Color Code: GREEN
Seismicity
During March 2014, the University of Utah reports 277 earthquakes were located in the Yellowstone National Park region. More events will be added as the University of Utah Seismograph Stations, responsible for the operation and analysis of the Yellowstone Seismic Network, processes the remaining March events. The largest event was a light earthquake of magnitude 4.7 on March 30, at 06:34 AM MDT, located four miles north-northeast of Norris Geyser Basin in Yellowstone National Park, Wyoming. The M4.7 main shock was reported felt in Yellowstone National Park, in the towns of Gardiner and West Yellowstone, Montana and throughout the region. This is the largest earthquake at Yellowstone since the early 1980s. Initial source analysis of the M4.7 earthquake suggests a tectonic origin (mostly strike-slip motion).
March 2014 seismicity was dominated by two earthquake clusters in the Norris Geyser Basin region and are described below.
1) A north-south trending series of earthquakes, over seven miles in length, began in September, 2013 and persisted throughout March with 130 events. The largest earthquake (magnitude 3.5) occurred on March 26, at 05:59 PM MDT, located 13 miles south-southwest of Mammoth, WY.
2) The earthquake series containing the March 30 magnitude 4.7 event began on March 27 and continues into April. At the end of March the series consisted of 70 located earthquakes, including the largest earthquake of the month, four magnitude 3 earthquakes, and numerous magnitude 2 and smaller earthquakes.
Earthquake sequences like these are common and account for roughly 50% of the total seismicity in the Yellowstone region.
Yellowstone earthquake activity in March is elevated compared with typical background levels.
Ground deformation
The ground deformation occurring in north-central Yellowstone continues. Since August 1, 2013, the NRWY GPS station has moved about 1.5 cm east, 2 cm north, and 5.5 cm up.
Further south, the caldera subsidence, which began in 2010, has ceased. Since the beginning of 2014, the caldera has been slowly rising at a rate of about 2 cm/yr. All the deformation currently occurring in Yellowstone remains well within historical norms.
The Yellowstone GPS network recorded no deformation associated with the March 30, 2014 M4.7 earthquake. Earthquakes of this size and depth do not typically produce ground displacements large enough to detect with GPS.
Other
The GPS field crew at Yellowstone has traveled around the Park over the past week and has not observed any effects from the earthquake. If any subtle changes have occurred, they are most likely to be found after the snow melts.
YVO's real time temperature data in Norris Geyser Basin indicate no significant changes to the thermal features that are monitored.(volcanoes.usgs.gov...)
The Yellowstone Volcano Observatory (YVO) provides long-term monitoring of volcanic and earthquake activity in the Yellowstone National Park region. Yellowstone is the site of the largest and most diverse collection of natural thermal features in the world and the first National Park. YVO is one of the five USGS Volcano Observatories that monitor volcanoes within the United States for science and public safety.
YVO Member agencies: USGS, Yellowstone National Park, University of Utah, University of Wyoming, UNAVCO, Inc., Wyoming State Geological Survey, Montana Bureau of Mines and Geology, Idaho Geological Survey
CONTACT INFORMATION:
Jacob Lowenstern, Scientist-in-Charge
[email protected]
During March 2014, the University of Utah reports 277 earthquakes were located in the Yellowstone National Park region. More events will be added as the University of Utah Seismograph Stations, responsible for the operation and analysis of the Yellowstone Seismic Network, processes the remaining March events.
Initial source analysis of the M4.7 earthquake suggests a tectonic origin (mostly strike-slip motion).
Yellowstone earthquake activity in March is elevated compared with typical background levels.
The ground deformation occurring in north-central Yellowstone continues. Since August 1, 2013, the NRWY GPS station has moved about 1.5 cm east, 2 cm north, and 5.5 cm up.
Further south, the caldera subsidence, which began in 2010, has ceased. Since the beginning of 2014, the caldera has been slowly rising at a rate of about 2 cm/yr. All the deformation currently occurring in Yellowstone remains well within historical norms.
March 2014 – WYOMING - A number of bloggers are posting videos that show bison and other animals allegedly leaving Yellowstone National Park, prompting theories that as earthquakes ramp up the seismic activity will set off the Yellowstone supervolcano.
Heat, by definition, is the kinetic energy of atomic or molecular translation, and/or rotation, and/or vibration. ... If, in high pressure states, the movement of atoms and molecules is limited, the heat energy content will be low and heat transport slower. Thus temperature and heating capacity are low and the internal energy is in the form of electronic-chemical energy, i.e., free electron movement and/or compression of electron shells within the atoms of the solid.It is only when the electro-chemically stored energy is transformed into kinetic energy of atoms (via vibration, and/or rotation, and/or translation) that the heat content increases. ... Conditions inside Earth where its internal energy can exist and be released as kinetic energy of its atoms, are only possible at, or very near to its surface, i.e. at lower pressures.
The combined logical implications of the observations presented in Tables 1, 2, and 3 lead us naturally and simply to the only physically congruous proposition left to us: that high temperatures and associated igneous melting must surely only be possible in small isolated areas within the upper-most outer ‘‘shell’’ of Earth, i.e., very close to its surface. Such igneous and accompanying metamorphic and hydrothermal processes, as well as asymmetric heat flow patterns, are attributed to highly concentrated electromagnetic phenomena. The localised heating of near-surface rocks is associated with electron accumulation at high local densities, temporary electron storage, and eventual accumulated voltage discharge, once the electromotive-force pressure induced by the mutual repulsion between confined electrons overcomes the localised electrical impedance to free electron flow. Associated with this process is intense radiation emission in the infrared bands (~10^12 to ~10^14 Hz).
Arp has shown that planetary masses (and some other astronomical bodies) are also quantized, they tend to be related with the same type of formula as the quasar redshifts.. Their masses are equal to a base mass times 1.23 to an integral power. The most obvious explanation of this phenomenon is that mass would be created in episodes, where mass already is; and it would be created in proportion to the existing mass. The simplest explanation of Arp’s planetary mass hypothesis is the same as that required to explain the Earth expansion rates advocated by Carey, Scalera and others.