alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
UNPUBLISHED UNITED STATES COURT OF APPEALS FOR THE FOURTH CIRCUIT
No. 95-8551
THOMAS G. RUTHERS, II, Petitioner - Appellant, versus JOHN GULCH, Warden, FCI Bastrop; STATE OF WEST VIRGINIA, Respondents - Appellees.
Appeal from the United States District Court for the Northern District of West Virginia, at Elkins. William M. Kidd, Senior District Judge. (CA-94-206-2) Submitted: April 15, 1996 Decided: May 9, 1996 Before ERVIN and MOTZ, Circuit Judges, and CHAPMAN, Senior Circuit Judge. Dismissed by unpublished per curiam opinion. Thomas G. Ruthers, II, Appellant Pro Se. William David Wilmoth, United States Attorney, Wheeling, West Virginia; Darrell V. McGraw, Jr., Scott E. Johnson, OFFICE OF THE ATTORNEY GENERAL OF WEST VIRGINIA, Charleston, West Virginia, for Appellees. Unpublished opinions are not binding precedent in this circuit. See Local Rule 36(c).2 PER CURIAM:Appellant appeals from the district court's order denying relief on his 28 U.S.C. § 2254 (1988) petition. We have reviewed the record and the district court's opinion and find no reversibleerror. Accordingly, we deny a certificate of probable cause to appeal and dismiss on the reasoning of the district court. Ruthers v. Gulch , No. CA-94-206-2 (N.D.W. Va. Dec. 6, 1995). Appellant identified several issues in his informal brief which he claims were not ruled on by the district court. We find that these issues were either incorporated into the district court's ruling, or wholly without merit. We dispense with oral argument because the facts and legal contentions are adequately presented in the materials before the court and argument would not aid the decisional process.

DISMISSED
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#           Response of lake chemistry to changes in atmospheric deposition and climate in three high-elevation wilderness areas of Colorado      

      November 23, 2011    

Trends in precipitation chemistry and hydrologic and climatic data were examined as drivers of long-term changes in the chemical composition of high-elevation lakes in three wilderness areas in Colorado during 1985–2008. Sulfate concentrations in precipitation decreased at a rate of −0.15 to −0.55 μeq/l/year at 10 high-elevation National Atmospheric Deposition Program stations in the state during 1987–2008 reflecting regional reductions in SO2 emissions. In lakes where sulfate is primarily derived from atmospheric inputs, sulfate concentrations also decreased although the rates generally were less, ranging from −0.12 to −0.27 μeq/l/year. The similarity in timing and sulfur isotopic data support the hypothesis that decreases in atmospheric deposition are driving the response of high-elevation lakes in some areas of the state. By contrast, in lakes where sulfate is derived primarily from watershed weathering sources, sulfate concentrations showed sharp increases during 1985–2008. Analysis of long-term climate records indicates that annual air temperatures have increased between 0.45 and 0.93°C per decade throughout most mountainous areas of Colorado, suggesting climate as a factor. Isotopic data reveal that sulfate in these lakes is largely derived from pyrite, which may indicate climate warming is preferentially affecting the rate of pyrite weathering.

## Citation Information

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#### M. Alisa Mast

##### Research Hydrologist

Colorado Water Science Center

mamast@usgs.gov

303-236-6989

####             David W Clow (Former Employee)          

##### Research Hydrologist

Colorado Water Science Center

## Related Content

#### M. Alisa Mast

##### Research Hydrologist

Colorado Water Science Center

mamast@usgs.gov

303-236-6989

####             David W Clow (Former Employee)          

##### Research Hydrologist

Colorado Water Science Center

### Study Area

### Contact

####               Colorado Water Science Center - Main Office          

West 6th Avenue and Kipling StreetDenver Federal Center, Building 53, MS-415Lakewood, CO80225United States

(303) 236-6900

(303) 236-4912

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<PAGE>
                                                                    EXHIBIT 23.1


                   CONSENT OF INDEPENDENT PUBLIC ACCOUNTANTS

     As independent public accountants, we hereby consent to the incorporation
by reference in this Form 10-K of our report dated January 21, 2002 included in
Registration Statement File No. 333-90965, 333-94317, 333-31420, 333-38828,
333-38834, 333-39440, 333-48460, 333-48464, 333-54566, 333-54568, 333-59602 and
333-81690. It should be noted that we have not audited any financial statements
of the company subsequent to December 31, 2001 or performed any audit procedures
subsequent to the date of our report.

                                   ARTHUR ANDERSEN LLP


San Jose, California
March 6, 2002
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#           Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: November 1981      

      January 1, 1981    

View Document

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.

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                  - Natural Hazards
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                  - College Observatory

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```

[Congressional Bills 114th Congress]
[From the U.S. Government Publishing Office]
[H.R. 4887 Enrolled Bill (ENR)]

        H.R.4887

                     One Hundred Fourteenth Congress

                                 of the

                        United States of America

                          AT THE SECOND SESSION

           Begun and held at the City of Washington on Monday,
           the fourth day of January, two thousand and sixteen

                                 An Act

 
To designate the facility of the United States Postal Service located at 
23323 Shelby Road in Shelby, Indiana, as the ``Richard Allen Cable Post 
                                Office''.

    Be it enacted by the Senate and House of Representatives of the 
United States of America in Congress assembled,
SECTION 1. RICHARD ALLEN CABLE POST OFFICE.
    (a) Designation.--The facility of the United States Postal Service 
located at 23323 Shelby Road in Shelby, Indiana, shall be known and 
designated as the ``Richard Allen Cable Post Office''.
    (b) References.--Any reference in a law, map, regulation, document, 
paper, or other record of the United States to the facility referred to 
in subsection (a) shall be deemed to be a reference to the ``Richard 
Allen Cable Post Office''.

                               Speaker of the House of Representatives.

                            Vice President of the United States and    
                                               President of the Senate.
```
<TABLE> <S> <C>

<PAGE>
<ARTICLE> 9
<LEGEND>
THIS SCHEDULE CONTAINS SUMMARY FINANCIAL INFORMATION EXTRACTED FROM THE
FINANCIAL STATEMENTS OF SPECTRUM BANCORPORATION, INC. FOR THE YEAR ENDED
JUNE 30, 1999 AND IS QUALIFIED IN ITS ENTIRETY BY REFERENCE TO SUCH FINANCIAL
STATEMENTS.
</LEGEND>
<MULTIPLIER> 1,000

<S>                             <C>
<PERIOD-TYPE>                   12-MOS
<FISCAL-YEAR-END>                          JUN-30-1999
<PERIOD-END>                               JUN-30-1999
<CASH>                                          18,389
<INT-BEARING-DEPOSITS>                             792
<FED-FUNDS-SOLD>                                 7,255
<TRADING-ASSETS>                                     0
<INVESTMENTS-HELD-FOR-SALE>                     91,140
<INVESTMENTS-CARRYING>                               0
<INVESTMENTS-MARKET>                                 0
<LOANS>                                        472,990
<ALLOWANCE>                                      6,020
<TOTAL-ASSETS>                                 611,170
<DEPOSITS>                                     506,909
<SHORT-TERM>                                    21,027
<LIABILITIES-OTHER>                              6,243
<LONG-TERM>                                     37,774
<PREFERRED-MANDATORY>                                0
<PREFERRED>                                      1,700
<COMMON>                                            72
<OTHER-SE>                                      35,425
<TOTAL-LIABILITIES-AND-EQUITY>                 611,170
<INTEREST-LOAN>                                 38,924
<INTEREST-INVEST>                                5,963
<INTEREST-OTHER>                                 1,386
<INTEREST-TOTAL>                                46,273
<INTEREST-DEPOSIT>                              19,751
<INTEREST-EXPENSE>                              23,156
<INTEREST-INCOME-NET>                           23,117
<LOAN-LOSSES>                                    1,333
<SECURITIES-GAINS>                                  27
<EXPENSE-OTHER>                                 16,518
<INCOME-PRETAX>                                 11,216
<INCOME-PRE-EXTRAORDINARY>                       7,202
<EXTRAORDINARY>                                      0
<CHANGES>                                            0
<NET-INCOME>                                     6,845
<EPS-BASIC>                                      93.34
<EPS-DILUTED>                                    93.34
<YIELD-ACTUAL>                                    4.29
<LOANS-NON>                                      1,401
<LOANS-PAST>                                     1,016
<LOANS-TROUBLED>                                 4,186
<LOANS-PROBLEM>                                      0
<ALLOWANCE-OPEN>                                 5,599
<CHARGE-OFFS>                                    1,059
<RECOVERIES>                                       147
<ALLOWANCE-CLOSE>                                6,020
<ALLOWANCE-DOMESTIC>                             6,020
<ALLOWANCE-FOREIGN>                                  0
<ALLOWANCE-UNALLOCATED>                              0


</TABLE>
Exhibit 32.2

Certification Pursuant to Section 906 of the Sarbanes-Oxley Act of 2002

Pursuant to 18 U.S.C. §1350, I, the undersigned Chief Financial Officer of Witness Systems, Inc. (the "Company"), hereby certify to my
knowledge and belief that the Quarterly Report on Form 10-Q of the Company for the quarterly period ended June 30, 2003 (the "Report") fully complies with the requirements of
Section 13(a) of the Securities Exchange Act of 1934 and that information contained in the Report fairly presents, in all material respects, the financial condition and results of operations of
the Company.

Dated:
August 14, 2003

| |  | BY: | /s/WILLIAM F. EVANSWilliam F. Evans
Chief Financial Officer
| |  | --- | -----------------------------------------------------------

A
signed original of this written statement required by Section 906, or other document authenticating, acknowledging, or otherwise adopting the signature that appears in typed form within the
electronic version of this written statement required by Section 906, has been provided to Witness Systems, Inc. and will be retained by Witness Systems, Inc. and furnished to the
Securities and Exchange Commission or its staff upon request.

---

QuickLinks
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#           New insight into lunar impact melt mobility from the LRO camera      

      November 1, 2010    

The Lunar Reconnaissance Orbiter Camera (LROC) is systematically imaging impact melt deposits in and around lunar craters at meter and sub-meter scales. These images reveal that lunar impact melts, although morphologically similar to terrestrial lava flows of similar size, exhibit distinctive features (e.g., erosional channels). Although generated in a single rapid event, the post-impact mobility and morphology of lunar impact melts is surprisingly complex. We present evidence for multi-stage influx of impact melt into flow lobes and crater floor ponds. Our volume and cooling time estimates for the post-emplacement melt movements noted in LROC images suggest that new flows can emerge from melt ponds an extended time period after the impact event.

## Citation Information

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                  -              Connect           

#### Laszlo Kestay, Ph.D.

##### Research Geologist

Astrogeology Science Center

laz@usgs.gov

928-556-7002

## Related Content

#### Laszlo Kestay, Ph.D.

##### Research Geologist

Astrogeology Science Center

laz@usgs.gov

928-556-7002

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

####               Southwest Biological Science Center - Flagstaff, AZ, Headquarters          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7094

928-556-7092
[Federal Register Volume 60, Number 103 (Tuesday, May 30, 1995)]
[Rules and Regulations]
[Page 28060]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: X95-10530]



-----------------------------------------------------------------------
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#           Spectrophotometric properties of materials observed by Pancam on the Mars Exploration Rovers: 2. Opportunity      

      January 1, 2006    

The Panoramic Camera (Pancam) on the Mars Exploration Rover Opportunity acquired visible/near‐infrared multispectral observations of soils and rocks under varying viewing and illumination geometries that were modeled using radiative transfer theory to improve interpretations of the microphysical and surface scattering nature of materials in Meridiani Planum. Nearly 25,000 individual measurements were collected of rock and soil units identified by their color and morphologic properties over a wide range of phase angles (0–150°) at Eagle crater, in the surrounding plains, in Endurance crater, and in the plains between Endurance and Erebus craters through Sol 492. Corrections for diffuse skylight incorporated sky models based on observations of atmospheric opacity throughout the mission. Disparity maps created from Pancam stereo images allowed inclusion of local facet orientation estimates. Outcrop rocks overall exhibited the highest single scattering albedos (≤0.9 at 753 nm), and most spherule‐rich soils exhibited the lowest (≤0.6 at 753 nm). Macroscopic roughness among outcrop rocks varied but was typically larger than spherule‐rich soils. Data sets with sufficient phase angle coverage (resulting in well‐constrained Hapke parameters) suggested that models using single‐term and two‐term Henyey‐Greenstein phase functions exhibit a dominantly broad backscattering trend for most undisturbed spherule‐rich soils. Rover tracks and other compressed soils exhibited forward scattering, while outcrop rocks were intermediate in their scattering behaviors. Some phase functions exhibited wavelength‐dependent trends that may result from variations in thin deposits of airfall dust that occurred during the mission.

## Citation Information

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####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

## Related Content

####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

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                  - Mars

View All **
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#           St. Louis area earthquake hazards mapping project; seismic and liquefaction hazard maps      

      November 9, 2016    

We present probabilistic and deterministic seismic and liquefaction hazard maps for the densely populated St. Louis metropolitan area that account for the expected effects of surficial geology on earthquake ground shaking. Hazard calculations were based on a map grid of 0.005°, or about every 500 m, and are thus higher in resolution than any earlier studies. To estimate ground motions at the surface of the model (e.g., site amplification), we used a new detailed near‐surface shear‐wave velocity model in a 1D equivalent‐linear response analysis. When compared with the 2014 U.S. Geological Survey (USGS) National Seismic Hazard Model, which uses a uniform firm‐rock‐site condition, the new probabilistic seismic‐hazard estimates document much more variability. Hazard levels for upland sites (consisting of bedrock and weathered bedrock overlain by loess‐covered till and drift deposits), show up to twice the ground‐motion values for peak ground acceleration (PGA), and similar ground‐motion values for 1.0 s spectral acceleration (SA). Probabilistic ground‐motion levels for lowland alluvial floodplain sites (generally the 20–40‐m‐thick modern Mississippi and Missouri River floodplain deposits overlying bedrock) exhibit up to twice the ground‐motion levels for PGA, and up to three times the ground‐motion levels for 1.0 s SA. Liquefaction probability curves were developed from available standard penetration test data assuming typical lowland and upland water table levels. A simplified liquefaction hazard map was created from the 5%‐in‐50‐year probabilistic ground‐shaking model. The liquefaction hazard ranges from low (<40% of area expected to liquefy) in the uplands to severe (>60% of area expected to liquefy) in the lowlands. Because many transportation routes, power and gas transmission lines, and population centers exist in or on the highly susceptible lowland alluvium, these areas in the St. Louis region are at significant potential risk from seismically induced liquefaction and associated ground deformation

## Citation Information

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#### Oliver S Boyd, Ph.D.

##### Research Geophysicist

Earthquake Hazards Program

olboyd@usgs.gov

303-273-8617

## Related Content

#### Oliver S Boyd, Ph.D.

##### Research Geophysicist

Earthquake Hazards Program

olboyd@usgs.gov

303-273-8617

### Study Area

### Contact

#### Geologic Hazards Science Center

1711 Illinois St.Golden, CO80401United States

303-273-8500

### Explore Search

                  - Natural Hazards
                  - United States
                  - Alabama
                  -  Arkansas
                  -  Illinois
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52940067;1 

UNITED STATES BANKRUPTCY COURT 

SOUTHERN DISTRICT OF FLORIDA 

West Palm Beach Division 

www.flsb.uscourts.gov

In re: Chapter 11

TOOJAY’S MANAGEMENT LLC, et al., Case No. 20-14792-EPK 

(Jointly Administered) 

Debtors. 

/ 

EX PARTE ORDER GRANTING DEBTOR’S MOTION TO REDACT DEBTORS’ 

EMERGENCY MOTION FOR ENTRY OF AN ORDER AUTHORIZING DEBTORS TO 

USE CASH COLLATERAL AND PROVIDE ADEQUATE PROTECTION (ECF NO. 11) 

THIS MATTER came before the Court upon Debtor’s Ex Parte Motion to Redact 

Debtors' Emergency Motion for Entry of an Order Authorizing Debtors to Use Cash Collateral 

and Provide Adequate Protection (the “Motion to Redact”). The Court, having reviewed the 

Motion to Redact, ORDERS as follows: 

1. The Motion to Redact is GRANTED. 

Erik P. Kimball, Judge

United States Bankruptcy Court

_____________________________________________________________________________

ORDERED in the Southern District of Florida on May 1, 2020.

Case 20-14792-EPK Doc 27 Filed 05/01/20 Page 1 of 2
2 

52940067;1 

2. The Clerk of Court shall take all steps necessary to make the Debtors' Emergency 

Motion for Entry of an Order Authorizing Debtors to Use Cash Collateral and Provide Adequate 

Protection (ECF No. 11) no longer publicly accessible. 

### 

SUBMITTED BY: 

Amanda Klopp, Esq. 

Akerman LLP 

Las Olas Centre II, Suite 1600 

350 East Las Olas Boulevard 

Fort Lauderdale, FL 33301-2999 

Phone: (954) 463-2700 

Fax: (954) 463-2224 

Copies furnished to: 

Amanda Klopp, Esq. [Attorney Klopp is directed to serve copies of this order on all interested 

parties and file a certificate of service with the Clerk of Court.] 

Case 20-14792-EPK Doc 27 Filed 05/01/20 Page 2 of 2
## F IRST 

## D ISTRICT 

## C OURT OF 

## A PPEAL 

## S TATE OF 

## F LORIDA

_____________________________
No. 1 D 2 0 2 4

- 1052

_____________________________
D AKODA W EINSTEIN , Appellant,

v.

S TATE OF F LORIDA D EPARTMENT OF R EVENUE C HILD S UPPORT P ROGRAM and C ARLOS C ABRERA , Appellee s

.

_____________________________

On appeal from the Division of Administrative Hearings. Andrew D. Manko , Judge

.

June 26, 2024

P ER C URIAM

. The Court dismisses the appeal as untimely filed. See Fla. R. App. P. 9.110(b)

.
L EWIS , N ORDBY , and T ANENBAUM , JJ., concur.

_____________________________ Not final until disposition of any timely and authorized motion under Fla. R. App. P. 9.330 or 9.331

.

_____________________________2 Dakoda Weinstein
, pro se, Appellant.

Ashley Moody, Attorney General, and Sarah C. Prieto, Assistant Attorney General, Tallahassee
, for Appellee Department of Revenue

.
November 13 , 2014



### JUDGMENT 

## The Fourteenth Court of Appeals

JONATHAN ALBERT LEAL , Appellant

NO. 14

- 13

- 00208

- CR V.
THE STATE OF TEXAS , Appellee

________________________________ This cause was heard on the transcript of the record of the court below. The record reveals error in the judgment. The Court orders the judgment REVERSED and REMANDED for further proceedings in accordance with its opinion. We order THE STATE OF TEXAS to pay all costs incurred in this appeal.
We further order this decision certified below for observance.
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#           The "terminal Triassic catastrophic extinction event" in perspective: a review of carboniferous through Early Jurassic terrestrial vertebrate extinction patterns      

      January 1, 1992    

A catastrophic terminal Triassic extinction event among terrestrial vertebrates is not supported by available evidence. The current model for such an extinction is based on at least eight weak or untenable assumptions: (1) a terminal Triassic extinction-inducing asteroid impact occurred, (2) a terminal Triassic synchronous mass extinction of terrestrial vertebrates occurred, (3) a concurrent terminal Triassic marine extinction occurred, (4) all terrestrial vertebrate families have similar diversities and ecologies, (5) changes in familial diversity can be gauged accurately from the known fossil record, (6) extinction of families can be compared through time without normalizing for changes in familial diversity through time, (7) extinction rates can be compared without normalizing for differing lengths of geologic stages, and (8) catastrophic mass extinctions do not select for small size. These assumptions have resulted in unsupportable and (or) erroneous conclusions. Carboniferous through Early Jurassic terrestrial vertebrate families mostly have evolution and extinction patterns unlike the vertebrate evolution and extinction patterns during the terminal Cretaceous event. Only the Serpukhovian (mid Carboniferous) extinction event shows strong analogy to the terminal Cretaceous event. Available data suggest no terminal Triassic extinction anomaly, but rather a prolonged and nearly steady decline in the global terrestrial vertebrate extinction rate throughout the Triassic and earliest Jurassic. ?? 1992.

## Citation Information