alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
### OFFICE ,OFTHE ATTORNEY GENERAL OF TEXAS AUSTINTare@ Prison Syetem, T‘ase3 .~

a&&it 

### be,* and a.6this aubjeot, Joe **‘ Igylor,**  has bean lmprleoned here slnoe July 26th, 1941, under the 

### sentenoefrom Stephens County, it eeema thet the Court rrom Stephens County and the Court from Young County have iseua& ccnfliating order&, and we are at e 1~s~ 8,e to properly determining the oorreot steps to take in this matter.” Under the faots stated in 9@ur letter, et the the See ‘Igylor wee aonviated in the Dietriot Court of Stephens County, Texas, he haQ been convloteQ In the I?letriot Court of Your Couot9, Texae, In four cesee. ‘;he 0618~8in wblah the 

### QelendantheQ been convloted In the TY?+riot Cqurt at Young County had been appeslrd, ?Q while such ceeee %iere on appeal he wee 

### tried in the biatriot Court:~or .%ephene 

### 0ouJJty.Xylem mar aonvloteQ tn 

### the ,Dletriot Oourt bl 

### Stephe,ns

Qounty@qbl

8ontemoeQta tna yemrrin the pealtentier& be Ma reaoliedet t&M Pr:%am on 8tJ%Ft $6, .&W%, urd his r%~Wn~ in tR* ~Btephans 

### UI%QBQowe U&S to R&J% whw’ eantanoae 

### in $he iour oans tram %NII& 

### bounty oeemd tie

fn other wards the sentenoe la thenWephene COWI- ~~~Z*was cumulative I4 the sentenoea in the oa8ea from Young tmlntg.

Ths oeaa or AL?A.J~ ‘I. Btete, 606 25, w. 345, holde 

### that

## notle*0rapperlin a pxwoeaing oee* 

## didnot deprive 

### the court or. the 

### parer ta ouWIle* fha ten tn tka l 

### *aand. aaeo,whkoh wntanoe 

### in the easonQqaeow&Q l

### trrt whOh’ that 

### in .$heproaddiagoasa oeaeed’toape,mkr ~~ ‘: ‘~ Although tha wee& iram Young U~ity’w~ru on appeal at tba time the aaae we* triad ia tie. aria @OUatp the uowt, i.n 6d.d had the paw to 0 uufai? ate th6 santano* e santenoea in thr other oaees rrcm ovide that the eantewe in that aasq 

### senterioee

in the o%eeB freei Young Uounty. onsod to aperote.

We or% 

### iaft#raeQ

by the Glerk of the Court of Cx ’iPliJhel Appmle $hst ma~Qe$~~ **iS6WJd** CatQber 17, 194~1, in 8810 

### four 4086s apmaled iram Young Gouaty. Be sppmls in 8hea.e OPJJO# were Qismiased upon the rspae%t CC ’ the detendant. In the asteeof 70~ell **V.** State, 63 3. F. (2d] 712, it Is statedr.

ATT0FdE-i G-
## Breadcrumb

-  Publications 
-  Articles 

#           Water alteration of rocks and soils on Mars at the Spirit rover site in Gusev crater      

      January 1, 2005    

Gusev crater was selected as the landing site for the Spirit rover because of the possibility that it once held a lake. Thus one of the rover's tasks was to search for evidence of lake sediments. However, the plains at the landing site were found to be covered by a regolith composed of olivine-rich basaltic rock and wind-blown 'global' dust. The analyses of three rock interiors exposed by the rock abrasion tool showed that they are similar to one another, consistent with having originated from a common lava flow. Here we report the investigation of soils, rock coatings and rock interiors by the Spirit rover from sol (martian day) 1 to sol 156, from its landing site to the base of the Columbia hills. The physical and chemical characteristics of the materials analysed provide evidence for limited but unequivocal interaction between water and the volcanic rocks of the Gusev plains. This evidence includes the softness of rock interiors that contain anomalously high concentrations of sulphur, chlorine and bromine relative to terrestrial basalts and martian meteorites; sulphur, chlorine and ferric iron enrichments in multilayer coatings on the light-toned rock Mazatzal; high bromine concentration in filled vugs and veins within the plains basalts; positive correlations between magnesium, sulphur and other salt components in trench soils; and decoupling of sulphur, chlorine and bromine concentrations in trench soils compared to Gusev surface soils, indicating chemical mobility and separation.

## Citation Information

## Related Content

                  -              Connect           

####             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

### Explore Search

                  - Gusev Crater; Mars
                  - Gusev Crater
                  -  Mars

View All **
This disposition is not appropriate for publication and is not precedent *

except as provided by 9th Cir. R. 36-3.

The panel unanimously concludes this case is suitable for decision **

without oral argument. See Fed. R. App. P. 34(a)(2).

NOT FOR PUBLICATION

UNITED STATES COURT OF APPEALS

 FOR THE NINTH CIRCUIT

ZEATLY KARAMONY,

 Petitioner,

 v.

ERIC H. HOLDER, Jr., Attorney General,

 Respondent.

No. 07-74988

Agency No. A096-346-448

MEMORANDUM*

On Petition for Review of an Order of the

Board of Immigration Appeals

Submitted August 10, 2010** 

Before: LEAVY, HAWKINS, and IKUTA, Circuit Judges. 

Zeatly Karamony, a native and citizen of Indonesia, petitions for review of

the Board of Immigration Appeals’ (“BIA”) order dismissing his appeal from an

immigration judge’s decision denying his application for withholding of removal. 

We have jurisdiction under 8 U.S.C. § 1252. We review for substantial evidence,

FILED

AUG 31 2010

MOLLY C. DWYER, CLERK

U.S. COURT OF APPEALS
2 07-74988

Lolong v. Gonzales, 484 F.3d 1173, 1178 (9th Cir.2007) (en banc), and we deny

the petition for review.

Substantial evidence supports the BIA’s denial of withholding because the

harassment Karamony suffered during the 1998 riots does not rise to the level of

persecution. See Halim v. Holder, 590 F.3d 971, 975-76 (9th Cir. 2009). Further,

Karamony has not provided sufficient evidence that she has been, or is likely to be,

specifically targeted for persecution as a Chinese Christian in Indonesia. See

Lolong, 484 F.3d at 1180 n.4 (rejecting petitioner’s claim where she failed to show

that she was “more likely to be targeted for persecution or harassment than any

other member of Indonesia’s Chinese Christian community”); see also Wakkary v.

Holder, 558 F.3d 1049, 1066 (9th Cir. 2009) (“An applicant for withholding of

removal will need to adduce a considerably larger quantum of individualized-risk

evidence to prevail”). Accordingly, Karamony’s withholding of removal claim

fails.

PETITION FOR REVIEW DENIED.
APETY AVENTURA, LLC, et al., Appellant(s)/Petitioner(s), v. Albert HANOUNA, Appellee(s)/Respondent(s),

CASE NO.: 3D17-2615

District Court of Appeal of Florida, Third District.

JANUARY 04, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Dismissed.
## Breadcrumb

-  Publications 
-  Conference Papers 

#           Numerical model characterization of sediment transport potentials pre- and post-construction of an artificial island in Foggy Island Bay, Alaska      

      April 15, 2023    

The anticipated construction of the Liberty Development Island near Prudhoe Bay, Alaska, has created a need to understand how the island may influence sediment transport patterns and deposition on the nearby Boulder Patch ecosystem. This study uses a numerical model to characterize sediment transport pathways in Foggy Island Bay with and without the artificial island in place. We present the Delft3D-based model setup and application that yields an improved quantification and understanding of the region’s hydrodynamic, wave, and sediment transport patterns. The results for the present show mainly east-west directed, alongshore transport of silt and clay. Insertion of the planned island results in limited changes to the overall hydrodynamic and sediment transport patterns within the Bay but reverses erosional tendencies across a boulder patch, situated within a kilometer of the planned construction location, to being net depositional.

## Citation Information

## Related Content

                  -              Connect           

#### Cornelis (Kees) Nederhoff

##### Modeling Scientist (contractor)

Pacific Coastal and Marine Science Center

cnederhoff@usgs.gov

831-460-7573

#### Li Erikson

##### Research Oceanographer

Pacific Coastal and Marine Science Center

lerikson@usgs.gov

831-460-7563

#### Anita Engelstad

##### Oceanographer

Pacific Coastal and Marine Science Center

aengelstad@usgs.gov

831-460-7588

## Related Content

#### Cornelis (Kees) Nederhoff

##### Modeling Scientist (contractor)

Pacific Coastal and Marine Science Center

cnederhoff@usgs.gov

831-460-7573

#### Li Erikson

##### Research Oceanographer

Pacific Coastal and Marine Science Center

lerikson@usgs.gov

831-460-7563

#### Anita Engelstad

##### Oceanographer

Pacific Coastal and Marine Science Center

aengelstad@usgs.gov

831-460-7588

### Study Area

### Contact

####               Pacific Coastal and Marine Science Center          

2885 Mission StreetSanta Cruz, CA95060United States

831-460-7401

### Explore Search

                  - United States
                  - Alaska
                  - Foggy Island Bay

View All **
## Breadcrumb

-  Publications 
-  Reports 

#           Superposed epoch analysis and storm statistics from 25 years of the global geomagnetic disturbance index, USGS-Dst      

      August 21, 2012    

View Document

Statistics on geomagnetic storms with minima below -50 nanoTesla are compiled using a 25-year span of the 1-minute resolution disturbance index, U.S. Geological Survey Dst. A sudden commencement, main phase minimum, and time between the two has a magnitude of 35 nanoTesla, -100 nanoTesla, and 12 hours, respectively, at the 50th percentile level. The cumulative distribution functions for each of these features are presented. Correlation between sudden commencement magnitude and main phase magnitude is shown to be low. Small, medium, and large storm templates at the 33rd, 50th, and 90th percentile are presented and compared to real examples. In addition, the relative occurrence of rates of change in Dst are presented.

## Citation Information

### Contact

#### Geologic Hazards Science Center

1711 Illinois St.Golden, CO80401United States

303-273-8500

### Explore Search

                  - Natural Hazards

View All **
## Breadcrumb

-  Publications 
-  Articles 

#           Surface energy balance of sub-Arctic roads with varying snow regimes and properties in permafrost regions      

      August 30, 2021    

Surface energy balance (SEB) strongly influences the thermal state of permafrost, cryohydrological processes, and infrastructure stability. Road construction and snow accumulation affect the energy balance of underlying permafrost. Herein, we use an experimental road section of the Alaska Highway to develop a SEB model to quantify the surface energy components and ground surface temperature (GST) for different land cover types with varying snow regimes and properties. Simulated and measured ground temperatures are in good agreement, and our results show that the quantity of heat entering the embankment center and slope is mainly controlled by net radiation, and less by the sensible heat flux. In spring, lateral heat flux from the embankment center leads to earlier disappearance of snowpack on the embankment slope. In winter, the insulation created by the snow cover on the embankment slope reduces heat loss by a factor of three compared with the embankment center where the snow is plowed. The surface temperature offsets are 5.0°C and 7.8°C for the embankment center and slope, respectively. Furthermore, the heat flux released on the embankment slope exponentially decreases with increasing snow depth, and linearly decreases with earlier snow cover in fall and shorter snow-covered period in spring.

## Citation Information

## Related Content

                  -              Connect           

#### Clifford I Voss, Ph.D.

##### Research Hydrologist Emeritus

Water Resources Mission Area

cvoss@usgs.gov

650-329-5885

## Related Content

#### Clifford I Voss, Ph.D.

##### Research Hydrologist Emeritus

Water Resources Mission Area

cvoss@usgs.gov

650-329-5885

### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

### Explore Search

                  - canada
                  - Beaver Creek area
                  - Yukon

View All **
114TH CONGRESS 

2D SESSION H. R. 4902 

AN ACT 

To amend title 5, United States Code, to expand law enforcement availability pay to employees of U.S. Customs and 

Border Protection’s Air and Marine Operations. 

1 Be it enacted by the Senate and House of Representa2 tives of the United States of America in Congress assembled, 
2 

•HR 4902 EH

1 SECTION 1. LAW ENFORCEMENT AVAILABILITY PAY FOR 

2 EMPLOYEES OF CUSTOMS AND BORDER PRO3 TECTION’S AIR AND MARINE OPERATIONS. 

4 (a) IN GENERAL.—Section 5545a(i) of title 5, United 

5 States Code, is amended— 

6 (1) by striking ‘‘apply to a pilot employed by 

7 the United States Customs Service’’ and inserting 

8 ‘‘apply to any employee of the U.S. Customs and 

9 Border Protection’s Air and Marine Operations, or 

10 any successor organization,’’; and 

11 (2) by striking ‘‘such pilot’’ and inserting ‘‘such 

12 employee’’. 

13 (b) APPLICABILITY.—The amendments made by sub14 section (a) shall take effect on the first day of the first 

15 applicable pay period beginning on or after the date that 

16 is 14 days after the date of enactment of this Act. 

Passed the House of Representatives June 21, 2016. 

Attest: 

Clerk. 

114TH CONGRESS 

2D SESSION H. R. 4902 

AN ACT 

To amend title 5, United States Code, to expand 

Marine Operations. U.S. Customs and Border Protection’s Air and law enforcement availability pay to employees of
Exhibit
32.1





CERTIFICATION


OF


CHIEF
EXECUTIVE OFFICER


AND


CHIEF
FINANCIAL OFFICER


PURSUANT
TO 18 U.S.C. 1350,


AS
ADOPTED PURSUANT TO


SECTION
906 OF THE SARBANES-OXLEY ACT OF 2002





I, Jacov
Vaisman, certify, pursuant to 18 U.S.C. 1350, as adopted pursuant to Section 906
of the Sarbanes-Oxley Act of 2002, that the Quarterly Report on Form 10-Q of
Advanced Medical Institute Inc. for the quarter ended December 31, 2008 fully
complies with the requirements of Section 13(a) or 15(d) of the Securities
Exchange Act of 1934 in all material respects and that information contained in
such Quarterly Report on Form 10-Q fairly presents, in all material respects,
the financial condition and results of operations of Advanced Medical Institute
Inc.




I, Dilip
Shrestha, certify, pursuant to 18 U.S.C. 1350, as adopted pursuant to Section
906 of the Sarbanes-Oxley Act of 2002, that the Quarterly Report on Form 10-Q of
Advanced Medical Institute Inc. for the quarter ended December 31, 2008 fully
complies with the requirements of Section 13(a) or 15(d) of the Securities
Exchange Act of 1934 in all material respects and that information contained in
such Quarterly Report on Form 10-Q fairly presents, in all material respects,
the financial condition and results of operations of Advanced Medical Institute
Inc.




February
17, 2009




By:
                      /s/ Jacov
      VaismanJacov
      VaismanChief
      Executive OfficerBy:
                      /s/ 
      Dilip ShresthaDilip
      ShresthaChief
      Financial
Officer
[Federal Register Volume 62, Number 101 (Tuesday, May 27, 1997)]
[Corrections]
[Page 28760]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: X97-10527]



Federal Register/Vol. 62, No. 101/Tuesday, May 27, 1997/Corrections

[[Page 28760]]



DEPARTMENT OF ENERGY

Federal Energy Regulatory Commission
[Docket No. RP97-116-003]


Koch Gateway Pipeline Company; Notice of Compliance Filing

Correction

    In notice document 97-13137 appearing on page 27597 in the issue of 
Tuesday, May 20, 1997, make the following correction:
    On page 27597, in the second column, in the first document, the 
Docket No. should read as set forth above.
BILLING CODE 1505-01-D
## Breadcrumb

-  Publications 
-  Articles 

#           Temperature profile around a basaltic sill intruded into wet sediments      

      July 1, 2015    

The transfer of heat into wet sediments from magmatic intrusions or lava flows is not well constrained from field data. Such field constraints on numerical models of heat transfer could significantly improve our understanding of water–lava interactions. We use experimentally calibrated pollen darkening to measure the temperature profile around a basaltic sill emplaced into wet lakebed sediments. It is well known that, upon heating, initially transparent palynomorphs darken progressively through golden, brown, and black shades before being destroyed; however, this approach to measuring temperature has not been applied to volcanological questions. We collected sediment samples from established Miocene fossil localities at Clarkia, Idaho. Fossils in the sediments include pollen from numerous tree and shrub species. We experimentally calibrated changes in the color of Clarkia sediment pollen and used this calibration to determine sediment temperatures around a Miocene basaltic sill emplaced in the sediments. Results indicated a flat temperature profile above and below the sill, with T > 325 °C within 1 cm of the basalt-sediment contact, near 300 °C at 1–2 cm from the contact, and ~ 250 °C at 1 m from the sill contact. This profile suggests that heat transport in the sediments was hydrothermally rather than conductively controlled. This information will be used to test numerical models of heat transfer in wet sediments on Earth and Mars.

## Citation Information

## Related Content

                  -              Connect           

#### Colin Dundas, Ph.D.

##### Research Geologist

Astrogeology Science Center

cdundas@usgs.gov

928-556-7143

#### Laszlo Kestay, Ph.D.

##### Research Geologist

Astrogeology Science Center

laz@usgs.gov

928-556-7002

## Related Content

#### Colin Dundas, Ph.D.

##### Research Geologist

Astrogeology Science Center

cdundas@usgs.gov

928-556-7143

#### 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
## Breadcrumb

-  Publications 
-  Articles 

#           Storage in California’s reservoirs and snowpack in this time of drought      

      November 17, 2015    

The San Francisco Bay and Sacramento–San Joaquin Delta (Delta) are the recipients of inflows from a watershed that spans much of California and that has ties to nearly the entire state. Historically, California has buffered its water supplies and flood risks both within—and beyond—the Delta’s catchment by developing many reservoirs, large and small, high and low. Most of these reservoirs carry water from wet winter seasons—when water demands are low and flood risks are high—to dry, warm seasons (and years) when demands are high and little precipitation falls. Many reservoirs are also used to catch and delay (or spread in time) flood flows that otherwise might cause damage to communities and floodplains. This essay describes the status of surface-water and snowpack storage conditions in California in spring 2015, providing context for better understanding where the state’s water stores stand as we enter summer 2015.

## Citation Information

## Related Content

## Related Content

### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

### Explore Search

                  - United States
                  - california

View All **
Candice Lynn WOLFSON, Appellant(s)/Petitioner(s), v. Howard WOLFSON, Appellee(s)/Respondent(s),

CASE NO.: 3D17-0974

District Court of Appeal of Florida, Third District.

JANUARY 31, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Dismissed.
DISTRICT COURT OF APPEAL OF THE STATE OF FLORIDA

FOURTH DISTRICT

RAUL REYNOSO,

Appellant,

v.

CITY OF BOCA RATON,

Appellee.

No. 4D18-2427

[April 24, 2019]

Appeal from the Circuit Court for the Fifteenth Judicial Circuit, Palm 

Beach County; Gerard Joseph Curley, Jr., Judge; L.T. Case No. 50-2016-

CA-000250-XXXX-MB.

Richard A. Sicking and Mark A. Touby of Touby, Chait & Sicking, P.L., 

Coral Gables, for appellant.

Laura K. Wendell, Daniel L. Abbott and Richard B. Rosengarten of 

Weiss Serota Helfman Cole & Bierman, P.L., Fort Lauderdale, for appellee.

PER CURIAM.

Affirmed. See Baker v. Airguide Mfg., LLC, 151 So. 3d 38 (Fla. 3d DCA 

2014).

MAY, CIKLIN and KLINGENSMITH, JJ., concur.

* * *

Not final until disposition of timely filed motion for rehearing.
[Federal Register Volume 61, Number 229 (Tuesday, November 26, 1996)]
[Notices]
[Page 60154]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: X96-31126]


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

ENVIRONMENTAL PROTECTION AGENCY

[SWH-FRL-5628-5]


Recovered Materials Advisory Notice

Correction

    In notice document 96-28735, beginning on page 57760, in the issue 
of Thursday, November 7, 1996, make the following correction:
    On page 57762, in Table C-5, in the third column, line 3 should 
read ``90-100''.

BILLING CODE 1505-01-D