alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
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#           Photogeology: Part N: ejecta blankets of large craters exemplified by King Crater      

      January 1, 1972    

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Details of the ejecta blankets of large, fresh craters provide insight into the mechanics of deposition and the sequence of emplacement of impact debris. King Crater is the freshest of the three large, rayed craters photographed from Apollo 16; the others are Theophilus and Langrenus Craters. King Crater is comparable in youth to Tycho Crater, and the details of its ejecta blanket help to interpret degraded equivalents at older craters. The clarity of detail and the occurrence of new types of lunar landforms rank King Crater among the most significant targets photographed from orbit in the Apollo Program (part M of this section).

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#### Keith A Howard

##### Scientist Emeritus

Geology, Minerals, Energy, and Geophysics Science Center

khoward@usgs.gov

650-439-2843

## Related Content

#### Keith A Howard

##### Scientist Emeritus

Geology, Minerals, Energy, and Geophysics Science Center

khoward@usgs.gov

650-439-2843

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

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#           Precipitation, streamflow, and water-quality data from selected sites in the City of Charlotte and Mecklenburg County, North Carolina, 1995-97      

      December 1, 1998    

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Precipitation data were collected at 46 precipitation sites and 3 atmospheric deposition sites, and hydrologic data were collected at 9 stream sites in the vicinity of Charlotte and Mecklenburg County, North Carolina, from July 1995 through June 1997. Data were collected to identify the type, concentration, and amount of nonpoint-source stormwater runoff within the area. The data collected include measurements of precipitation; streamflow; physical characteristics, such as water temperature, pH, specific conductance, biochemical oxygen demand, oil and grease, and suspended sediment concentrations; and concentrations of nutrients, metals and minor constituents, and organic compounds.

These data should provide valuable information needed for (1) planned watershed simulation models, (2) estimates of nonpoint-source constituent loadings to the Catawba River, and (3) characterization of water quality in relation to basin conditions. Streamflow and rainfall data have been used to provide early warning of possible flooding.

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Roshaud Ulysee HEARD, Appellant, v. STATE of Florida, Appellee.

Case No. 2D15-5567

District Court of Appeal of Florida, Second District.

Opinion filed January 12, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Affirmed.
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#           Simulated water-level declines near Marienthal, west-central Kansas      

      January 1, 1980    

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Intensive study in an area of 12-square miles near Marienthal, Kansas, has shown a decrease of 30 to 50 percent in saturated thickness of the Ogallala Formation since the development of irrigation. Projections from a digital model indicated the additional water-level declines that might occur from 1978 to 1989 if the pumpage in the model area was assumed to be one-half, equal to, or double the 1977 rate. The additional declines would range from 5 to 15 feet, 15 to 30 feet, and 25 to 40 feet, respectively. If pumpage only in the intensive-study area were assumed to be one-half or double the 1977 rate, water-level declines would range from 10 to 20 feet and from 20 to 25 feet, respectively. Reducing pumpage only in the intensive-study area could reduce the water-level declines locally. However, declines would be greatest near the edge of the area as a result of continued pumpage by wells outside the area boundary.

The digital model was more sensitive to changes in pumpage than to changes in hydraulic conductivity, specific yield, and recharge.

## Citation Information

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####               Kansas Water Science Center          

1217 Biltmore DriveLawrence, KS66049United States

(785) 842-9909

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Exemption No. 11069

UNITED STATES OF AMERICA DEPARTMENT OF TRANSPORTATION FEDERAL AVIATION ADMINISTRATION RENTON, WASHINGTON 98057-3356

In the matter of the petition of

PATS Aircraft Systems

for an exemption from § 25.813(e) of Title 14, Code of Federal Regulations Regulatory Docket No. FAA-2014-0267

GRANT OF EXEMPTION By letter dated April 11, 2014, William J. Er tle II, ODA Operations Manager/STC ODA Administrator, PATS Aircraft Systems, 21652 Nanticoke Avenue, Georgetown, DE 19947, petitioned the Federal Aviation Administ ration (FAA) for an exemption from the requirements of § 25.813(e) of Title 14, Code of Federal Regulations (14 CFR) to include electrically actuated interior doors. The proposed exemp tion, if granted, would permit the installation of electrically actuated doors in the passenge r compartment on Boeing Model 737-700IGW and 737-800 airplanes. The propose d exemption is specifically for the installation of executive in teriors on Boeing 737-700IGW and 737-800 airplanes that have been designated as “private use, not for hire, not for common carriage.”
The petitioner requests relief from the following regulations:
Section 25.813(e), Amendment 25-88 – No door may be installed in any partition between passenger compartments.
The petitioner supports its request with the following information:
This section quotes, in pertinent part, the relevant information from the petitioner’s request, with minor edits for clarity. The comple te petition is availabl e at the Department of Transportation’s Federal Docket Ma nagement System, on the Internet at http://regulations.gov, in docket no. FAA-2014-0267. General Background: The proposed exemption is specifically for the installation of electrically operated Pocket Doors in Executive, VIP or H ead of State interi ors installed and designated “private, not-for-hire, not- for-common carriage”. There are TCDS exemptions, i.e. Boeing 737-700IGW (6820 & 6820A), Boeing 737-800 (7609), that already exist and SFAR 109 for Tran sport Category Airplanes that provides
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#           Strontium isotopic geochemistry of the Devils Lake drainage system, North Dakota: A preliminary study and potential paleoclimatic implications      

      January 1, 1997    

A series of water samples (precipitation, surface water and ground water) from the Devils Lake drainage basin in central North Dakota have been analyzed for their ??180 and ??D and 87Sr/86Sr. The ??180 and ??D of snow and most ground water samples fall near the meteoric water line, with the ground water being isotopically heavier than the snow, indicating that a portion of the recharge must come from non-winter precipitation events. One ground water and all the surface water samples fall below the meteoric water line, demonstrating extensive evaporation. The 87Sr/86Sr ratio of the snow is more radiogenic than those of the ground water samples, indicating that the ground water has increased its 86Sr content by the dissolution of mafic rock in the aquifer. Stump Lake has a much inure radiogenic Sr isotopic ratio than the waters of Devils Lake suggesting a source of water different from that of Devils Lake. The East Stump Lake water, on the other hand, appears to be either a mix of Devils Lake and Stump Lake waters, or Devils Lake water diluted with precipitation.

## Citation Information

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#### Dakota Water Science Center- Rapid City

1608 Mountain ViewRapid City, SD57702United States

(605) 394-3200

(605) 355-4523
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#           Public-policy issues associated with the SAFRR Tsunami Scenario      

      September 6, 2013    

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The SAFRR (Science Application for Risk Reduction) tsunami scenario simulates a tsunami generated by a hypothetical magnitude 9.1 earthquake that occurs offshore of the Alaska Peninsula (Kirby and others, 2013). In addition to the work performed by the authors on public-policy issues associated with the SAFRR tsunami scenario, this section of the scenario also reflects the policy discussions of the State of California’s Tsunami Policy Work Group, a voluntary advisory body formed in October 2011, which operates under the California Natural Resources Agency (CNRA), Department of Conservation, and is charged with identifying, evaluating, and making recommendations to resolve issues that are preventing full and effective implementation of tsunami hazard mitigation and risk reduction throughout California’s coastal communities. It also presents the analyses of plans and hazard policies of California’s coastal counties, incorporated cities, and major ports performed by the staff of the California Geological Survey (CGS) and Lauren Prehoda, Office of Environmental and Government Affairs, California Department of Conservation. It also draws on the policy framework and assessment prepared for the ARkStorm Pacific Coast winter storm and catastrophic flooding (Topping and others, 2010).

## Citation Information

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####               Natural Hazards Mission Area Headquarters          

12201 Sunrise Valley DrReston, VA20192United States

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#           Source and site response study of the 2008 Mount Carmel, Illinois, earthquake      

      January 1, 2011    

Two separate inversions are performed using the ground-motion data from the 2008 Mount Carmel, Illinois, earthquake. One uses aftershocks as empirical Green’s functions to determine a finite-fault slip distribution. The second uses mainshock ground-motion spectra to calculate source, path, and site response parameters. The slip inversion reveals a prominent asperity at the hypocenter with an area of approximately 6 km2, moment of 7.0 x 1023 dyn cm (Mw 5.20), and stress drop of about 100 bars. Considering all major and minor slip, the total moment is 1.7 x 1024 dyn cm (Mw=5.45). The rupture velocity is not resolvable due to the small source area. After fixing the geometric spreading, the source, path, and site parameter inversion yields a similar moment of 8.8 x 1023 dyn cm (Mw 5.26) and a corner frequency of 0.89 Hz, which also give a stress drop of approximately 100 bars. Our combined geometric and anelastic attenuation function, Q(f)r-b=1137f0.12r-0.94, fits the regional spectral amplitudes, where the data is more plentiful, as well as previously derived attenuation relationships. Site response spectra show prominent resonant frequencies that correlate with the thickness of Mississippi River sediments and Mississippi embayment deposits. In addition, higher frequency resonance peaks are observed that most likely represent higher mode resonances and resonances from shallower structure.

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#           Progress report on the geology and ground-water hydrology of the Lower Missouri-Souris Unit; Part 1, Crosby-Mohall area, North Dakota      

      January 1, 1949    

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The Crosby-Mohall area covers about 2,700 square miles in the north-western part of North Dakota. This area is included in the 2,500,000-acre Missouri-Souris and Garrison Diversion irrigation projects,which are important units in the general plans for development of the water resources of the Missouri River Basin. Although the Crosby-Mohall area lies outside the drainage basin of the Missouri River, plans have been made for the irrigation of about 1,000,0)0 acres (equivalent to 1,560 square miles) of the most suitable land, with water brought by canal from the Missouri River in Montana. 

The studies that have been undertaken in the area by the Division of Ground Water of the United States Geological Survey form a part of the investigations which have been initiated by the Survey and several other bureaus of the Department of the Interior, especially the Bureau of Reclamation. The studies on which the present report is bas2 were made during the field seasons of 1945, 1946 and 1947, to obtain information on the occurrence, movement, quantity, and quality of the ground water. The report contains data on the several kinds of water-bearing materials, water analyses, and well logs; the records of fluctuation of water level in about 400 wells; and an inventory of 4,636 wells and test holes. 

Later studies for the whole of the Missouri-Souris Unit will supply additional data on ground-water levels and piezometric surfaces, more extensive information on quality of water, a complete inventory of wells, and further geologic information relating to ground-water supplies. Other work that is planned also includes the drilling of additional test holes and the analysis of water samples from representative wells throughout the area. 

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Case 20-12895-PDR Doc 134 Filed 06/18/21 Page 1 of 2
Case 20-12895-PDR Doc 134 Filed 06/18/21 Page 2 of 2
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#           Seasonal flows of international British Columbia-Alaska rivers: The nonlinear influence of ocean-atmosphere circulation patterns      

      February 12, 2016    

The northern portion of the Pacific coastal temperate rainforest (PCTR) is one of the least anthropogenically modified regions on earth and remains in many respects a frontier area to science. Rivers crossing the northern PCTR, which is also an international boundary region between British Columbia, Canada and Alaska, USA, deliver large freshwater and biogeochemical fluxes to the Gulf of Alaska and establish linkages between coastal and continental ecosystems. We evaluate interannual flow variability in three transboundary PCTR watersheds in response to El Niño-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), Arctic Oscillation (AO), and North Pacific Gyre Oscillation (NPGO). Historical hydroclimatic datasets from both Canada and the USA are analyzed using an up-to-date methodological suite accommodating both seasonally transient and highly nonlinear teleconnections. We find that streamflow teleconnections occur over particular seasonal windows reflecting the intersection of specific atmospheric and terrestrial hydrologic processes. The strongest signal is a snowmelt-driven flow timing shift resulting from ENSO- and PDO-associated temperature anomalies. Autumn rainfall runoff is also modulated by these climate modes, and a glacier-mediated teleconnection contributes to a late-summer ENSO-flow association. Teleconnections between AO and freshet flows reflect corresponding temperature and precipitation anomalies. A coherent NPGO signal is not clearly evident in streamflow. Linear and monotonically nonlinear teleconnections were widely identified, with less evidence for the parabolic effects that can play an important role elsewhere. The streamflow teleconnections did not vary greatly between hydrometric stations, presumably reflecting broad similarities in watershed characteristics. These results establish a regional foundation for both transboundary water management and studies of long-term hydroclimatic and environmental change.

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####               Alaska Science Center          

4210 University DriveAnchorage, AK99508United States

(907) 786-7000

(907) 786-7020

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UNITED STATES BANKRUPTCY COURT

SOUTHERN DISTRICT OF FLORIDA

FORT LAUDERDALE DIVISION

CASE NO.: 20-13104-BKC-PDR

PROCEEDING UNDER CHAPTER 13

IN RE:

MARC-AUREL GENECE

XXX-XX-2300

_____________________________/

CERTIFICATE OF SERVICE ON NOTICE OF HEARING

DEBTOR

I HEREBY CERTIFY that I am admitted to the Bar of the United States District Court for the 

Southern District of Florida and I am in compliance with the additional qualifications to practice in this 

Court as set forth in Local Rule 2090-1(A) and that a true and correct copy of the Notice Of Hearing noted 

above was served, via U.S. first class mail, certified mail and/or CM/ECF, upon the parties listed on the 

attached service list this 8th day of April, 2021.

/s/ Robin R. Weiner

ROBIN R. WEINER, ESQUIRE

STANDING CHAPTER 13 TRUSTEE

P.O. BOX 559007

FORT LAUDERDALE, FL 33355-9007

TELEPHONE: 954-382-2001

FLORIDA BAR NO.: 861154

_____________________________________

Case 20-13104-PDR Doc 41 Filed 04/08/21 Page 1 of 2
CERTIFICATE OF SERVICE

CASE NO.: 20-13104-BKC-PDR

SERVICE LIST

COPIES FURNISHED TO:

DEBTOR

MARC-AUREL GENECE

5170 SW 19 ST

PLANTATION, FL 33317

ATTORNEY FOR DEBTOR

JOHN D. SEGAUL, ESQUIRE

300 S PINE ISLAND ROAD

SUITE 304

PLANTATION, FL 33324

CREDITOR(S)

QUICKSILVER CAPITAL, LLC.

BERKOVITCH & BOUSKILA, PLLC.

80 BROAD ST., SUITE 3303

NEW YORK, NY 10004

Case 20-13104-PDR Doc 41 Filed 04/08/21 Page 2 of 2
[Federal Register Volume 60, Number 42 (Friday, March 3, 1995)]
[Corrections]
[Page 12034]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: X95-60303]



-----------------------------------------------------------------------

DEPARTMENT OF THE TREASURY

Internal Revenue Service

26 CFR Part 1

[INTL-933-86]
RIN 1545-AL98


Computation of Foreign Taxes Deemed Paid Under Section 902 
Pursuant to a Pooling Mechanism for Undistributed Earnings and Foreign 
Taxes

Correction

    In proposed rule document 95-173 beginning on page 2049 in the 
issue of Friday, January 6, 1995, make the following correction:


Sec. 1.902-2  [Corrected]

    On page 2063, in the first column, the heading for Sec. 1.902-2 
should read as set forth below:


Sec. 1.902-2  Treatment of deficits in post-1986 undistributed earnings 
and pre-1987 accumulated profits of a first-, second-, or third-tier 
corporation for purposes of computing an amount of foreign taxes deemed 
paid under Sec. 1.902-1.

BILLING CODE 1505-01-D
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#           Radiocarbon dating of tsunami and storm deposits      

      July 31, 2020    

Radiocarbon age determinations can be an expedient and accurate means to assign age to deposits of tsunami or storm origin. Essential to the process of incorporating radiocarbon age determinations in tsunami or coastal storm investigations is an awareness on the part of the investigator that a sample will always return an age from a laboratory, but only carefully selected samples inform deposit age. Samples that inform deposit age are of two fundamentally different sample types, in-growth-position samples and detrital samples. For both in-growth-position samples and detrital samples, stratigraphic context is the critical information needed to evaluate how well sample age can constrain deposit age. Well constrained deposit ages require bracketing samples collected to provide both maximum and minimum limiting ages for the deposit(s) of interest. Therefore, sampling should be carried out with the intention of multiple sample submissions for age in order to optimize the potential for acquiring closely limiting ages. If there are multiple age determinations within a stratigraphic sequence that contains tsunami or storm deposits, then the calibrated radiocarbon ages can be, and should be, framed within a Bayesian model structure to better constrain deposit ages. Such models can be further improved by the incorporation of independent stratigraphic age information.

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#### Rob Witter, Ph.D.

##### Research Geologist

Alaska Science Center

rwitter@usgs.gov

907-786-7404

## Related Content

#### Rob Witter, Ph.D.

##### Research Geologist

Alaska Science Center

rwitter@usgs.gov

907-786-7404

### Contact

####               Alaska Science Center          

4210 University DriveAnchorage, AK99508United States

(907) 786-7000

(907) 786-7020
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#           Shallow lithological structure across the Dead Sea Transform derived from geophysical experiments      

      January 1, 2011    

In the framework of the DEad SEa Rift Transect (DESERT) project a 150 km magnetotelluric profile consisting of 154 sites was carried out across the Dead Sea Transform. The resistivity model presented shows conductive structures in the western section of the study area terminating abruptly at the Arava Fault. For a more detailed analysis we performed a joint interpretation of the resistivity model with a P wave velocity model from a partially coincident seismic experiment. The technique used is a statistical correlation of resistivity and velocity values in parameter space. Regions of high probability of a coexisting pair of values for the two parameters are mapped back into the spatial domain, illustrating the geographical location of lithological classes. In this study, four regions of enhanced probability have been identified, and are remapped as four lithological classes. This technique confirms the Arava Fault marks the boundary of a highly conductive lithological class down to a depth of ∼3 km. That the fault acts as an impermeable barrier to fluid flow is unusual for large fault zone, which often exhibit a fault zone characterized by high conductivity and low seismic velocity. At greater depths it is possible to resolve the Precambrian basement into two classes characterized by vastly different resistivity values but similar seismic velocities. The boundary between these classes is approximately coincident with the Al Quweira Fault, with higher resistivities observed east of the fault. This is interpreted as evidence for the original deformation along the DST originally taking place at the Al Quweira Fault, before being shifted to the Arava Fault.

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#### Paul A Bedrosian

##### Research Geophysicist

Geology, Geophysics, and Geochemistry Science Center

pbedrosian@usgs.gov

303-236-4834

## Related Content

#### Paul A Bedrosian

##### Research Geophysicist

Geology, Geophysics, and Geochemistry Science Center

pbedrosian@usgs.gov

303-236-4834

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#### Geology, Geophysics, and Geochemistry Science Center

West 6th Avenue and Kipling StreetDenver Federal Center Building 20Denver, CO80225United States

303-236-1800

303-236-3200

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Derek OELSCHLAGER, Appellant/Petitioner(s), v. Thomas M. KNIGHT, Sheriff, Appellee/Respondent(s).

CASE NO.: 2D18-2593

District Court of Appeal of Florida, Second District.

July 03, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Granted.