alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
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#           Moon-forming impactor as a source of Earth’s basal mantle anomalies      

      November 1, 2023    

Seismic images of Earth’s interior have revealed two continent-sized anomalies with low seismic velocities, known as the large low-velocity provinces (LLVPs), in the lowermost mantle. The LLVPs are often interpreted as intrinsically dense heterogeneities that are compositionally distinct from the surrounding mantle. Here we show that LLVPs may represent buried relics of Theia mantle material (TMM) that was preserved in proto-Earth’s mantle after the Moon-forming giant impact. Our canonical giant-impact simulations show that a fraction of Theia’s mantle could have been delivered to proto-Earth’s solid lower mantle. We find that TMM is intrinsically 2.0–3.5% denser than proto-Earth’s mantle based on models of Theia’s mantle and the observed higher FeO content of the Moon. Our mantle convection models show that dense TMM blobs with a size of tens of kilometres after the impact can later sink and accumulate into LLVP-like thermochemical piles atop Earth’s core and survive to the present day. The LLVPs may, thus, be a natural consequence of the Moon-forming giant impact. Because giant impacts are common at the end stages of planet accretion, similar mantle heterogeneities caused by impacts may also exist in the interiors of other planetary bodies.

## Citation Information

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#### Travis S.J. Gabriel, Ph.D.

##### Research Physical Scientist

Astrogeology Science Center

tgabriel@usgs.gov

## Related Content

#### Travis S.J. Gabriel, Ph.D.

##### Research Physical Scientist

Astrogeology Science Center

tgabriel@usgs.gov

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014
Certificate Number: 12433-FLS-DE-033343372

Bankruptcy Case Number: 19-20376

12433-FLS-DE-033343372

CERTIFICATE OF DEBTOR EDUCATION

I CERTIFY that on September 3, 2019, at 8:08 o'clock PM EDT, Angel Antonio

Cainzo completed a course on personal financial management given by internet

by Solid Start Financial Education Services, LLC, a provider approved pursuant

to 11 U.S.C. 111 to provide an instructional course concerning personal financial

management in the Southern District of Florida.

Date: September 3, 2019 By: /s/Lance Brechbill

Name: Lance Brechbill

Title: Teacher

Case 19-20376-AJC Doc 20 Filed 09/04/19 Page 1 of 1
# L_2004305EN.01006101.xml

| 1.10.2004 | EN | Official Journal of the European Union | L 305/61 |
| --- | --- | --- | --- |

1.10.2004

EN

Official Journal of the European Union

L 305/61

---

COMMISSION REGULATION (EC) No 1718/2004

of 30 September 2004

concerning tenders notified in response to the invitation to tender for the export of oats issued in Regulation (EC) No 1565/2004

THE COMMISSION OF THE EUROPEAN COMMUNITIES,

Having regard to the Treaty establishing the European Community,

Having regard to Council Regulation (EC) No 1784/2003 of 29 September 2003 on the common organisation of the market in cereals (1), and in particular Article 7 thereof,

Having regard to Commission Regulation (EC) No 1501/95 of 29 June 1995 laying down certain detailed rules for the application of Council Regulation (EEC) No 1766/92 on the granting of export refunds on cereals and the measures to be taken in the event of disturbance on the market for cereals (2), and in particular Article 7 thereof,

Having regard to Commission Regulation (EC) No 1565/2004 of 3 September 2004 on a special intervention measure for cereals in Finland and Sweden for the 2004/2005 marketing year (3),

Whereas:

| (1) | An invitation to tender for the refund for the export of oats produced in Finland and Sweden for export from Finland and Sweden to all third countries, with the exception of Bulgaria, Norway, Romania and Switzerland was opened pursuant to Regulation (EC) No 1565/2004. |
| --- | --- |

(1)

An invitation to tender for the refund for the export of oats produced in Finland and Sweden for export from Finland and Sweden to all third countries, with the exception of Bulgaria, Norway, Romania and Switzerland was opened pursuant to Regulation (EC) No 1565/2004.

| (2) | On the basis of the criteria laid down in Article 1 of Regulation (EC) No 1501/95, a maximum refund should not be fixed. |
| --- | --- |

(2)

On the basis of the criteria laid down in Article 1 of Regulation (EC) No 1501/95, a maximum refund should not be fixed.

| (3) | The measures provided for in this Regulation are in accordance with the opinion of the Management Committee for Cereals, |
| --- | --- |

(3)

The measures provided for in this Regulation are in accordance with the opinion of the Management Committee for Cereals,

HAS ADOPTED THIS REGULATION:

Article 1

No action shall be taken on the tenders notified from 24 to 30 September 2004 in response to the invitation to tender for the refund for the export of oats issued in Regulation (EC) No 1565/2004.

Article 2

This Regulation shall enter into force on 1 October 2004.

This Regulation shall be binding in its entirety and directly applicable in all Member States

Done at Brussels, 30 September 2004.

For the Commission

Franz FISCHLER

Member of the Commission

---

(1)  
  OJ L 270, 21.10.2003, p. 78.

1

(2)  
  OJ L 147, 30.6.1995, p. 7. Regulation as last amended by Regulation (EC) No 1431/2003 (OJ L 203, 12.8.2003, p. 16).

2

(3)  
  OJ L 285, 4.9.2004, p. 3.

3

---
Case 19-01298-MAM Doc 474-9 Filed 10/22/20 Page 1 of 2
Case 19-01298-MAM Doc 474-9 Filed 10/22/20 Page 2 of 2
## Breadcrumb

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#           Planetary caves: A Solar System view of processes and products      

      October 28, 2022    

We provide the first solar system wide compendium of speleogenic processes and products. An examination of 15 solar system bodies revealed that six cave-forming processes occur beyond Earth including volcanic (cryo and magmatic), fracturing (tectonic and impact melt), dissolution, sublimation, suffusion, and landslides. Although no caves (i.e., confirmed entrances with associated linear passages) have been confirmed, 3,545 SAPs (subsurface access points) have been identified on 11 planetary bodies and the potential for speleogenic processes (and thus SAPs) was observed on an additional four planetary bodies. The bulk of our knowledge on extraterrestrial SAPs is based upon global databases for the Moon and Mars, which are bodies for which high-resolution imagery and other data are available. To further characterize most of the features beyond the Moon and Mars, acquisition (preferably global coverage) and subsequent analysis of high-resolution imagery will be required. The next few decades hold considerable promise for identifying and potentially characterizing caves across the solar system.

## Citation Information

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#### Timothy Neal Titus, Ph.D.

##### Research Space Scientist

Astrogeology Science Center

ttitus@usgs.gov

928-556-7201

## Related Content

#### Timothy Neal Titus, Ph.D.

##### Research Space Scientist

Astrogeology Science Center

ttitus@usgs.gov

928-556-7201

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

### Explore Search

                  - solar system

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## Breadcrumb

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#           Practitioners' views of science needs for the Great Lakes coastal ecosystem      

      January 1, 2015    

In 2014, the U.S. Geological Survey Great Lake Science Center (USGS-GLSC) and the USGS-Michigan Water Science Center partnered with the Great Lakes Commission (GLC) to conduct a series of four workshops with coastal practitioners and managers across the Great Lakes basin to highlight the need for, and get input on, a Great Lakes regional coastal science strategy. To this end, this report is intended to help guide USGS coastal and nearshore science priorities, but may also help guide other science agencies.

The USGS-GLSC partnership on this effort was part of a broader five-year Memorandum of Understanding between the USGS-GLSC and the GLC to enhance communications between coastal science and management communities within the Great Lakes region.

This report presents a summary and analysis of participant feedback from the four workshops held in 2014. Participant feedback included participant worksheets as well as interactive drawing sessions, individual notes and group flip chart notes from each workshop. The results are presented as a series of findings that can be used to guide USGS coastal/nearshore science priorities in support of management needs at local, state and regional scales.

## Citation Information

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#### Lisa Reynolds Fogarty

##### Chief Science Officer

Upper Midwest Water Science Center

lrfogart@usgs.gov

517-887-8968

## Related Content

#### Lisa Reynolds Fogarty

##### Chief Science Officer

Upper Midwest Water Science Center

lrfogart@usgs.gov

517-887-8968

### Contact

####               Great Lakes Science Center          

1451 Green RoadAnn Arbor, MI48105United States

734-994-3331

734-994-8780
Case 19-01298-MAM Doc 472-46 Filed 10/22/20 Page 1 of 1
EX PARTE Farris BURRELL

CR-15-1438

Court of Criminal Appeals of Alabama.

April 3, 2017

**DECISION WITHOUT PUBLISHED OPINION**

Mand. pet. dismissed.
## Breadcrumb

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#           Lake water temperature modeling in an era of climate change: Data sources, models, and future prospects      

      February 11, 2024    

Lake thermal dynamics have been considerably impacted by climate change, with potential adverse effects on aquatic ecosystems. To better understand the potential impacts of future climate change on lake thermal dynamics and related processes, the use of mathematical models is essential. In this study, we provide a comprehensive review of lake water temperature modeling. We begin by discussing the physical concepts that regulate thermal dynamics in lakes, which serve as a primer for the description of process-based models. We then provide an overview of different sources of observational water temperature data, including in situ monitoring and satellite Earth observations, used in the field of lake water temperature modeling. We classify and review the various lake water temperature models available, and then discuss model performance, including commonly used performance metrics and optimization methods. Finally, we analyze emerging modeling approaches, including forecasting, digital twins, combining process-based modeling with deep learning, evaluating structural model differences through ensemble modeling, adapted water management, and coupling of climate and lake models. This review is aimed at a diverse group of professionals working in the fields of limnology and hydrology, including ecologists, biologists, physicists, engineers, and remote sensing researchers from the private and public sectors who are interested in understanding lake water temperature modeling and its potential applications.

## Citation Information

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#### Samantha K Oliver, PhD

##### Hydrologist

Water Resources Mission Area

soliver@usgs.gov

608-821-3824

## Related Content

#### Samantha K Oliver, PhD

##### Hydrologist

Water Resources Mission Area

soliver@usgs.gov

608-821-3824

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

####               Upper Midwest Water Science Center - Madison, WI, Office          

1 Gifford Pinchot DriveMadison, WI53726United States

608-828-9901

608-821-3817
UNITED STATES BANKRUPTCY COURT 

SOUTHERN DISTRICT OF FLORIDA 

FORT LAUDERDALE DIVISION 

www.flsb.uscourts.gov 

In re: 

Louis Tino Fisher, 

 Debtor. 

Chapter 7 

Case No. 19-19710-SMG 

ORDER DISMISSING CASE 

 This matter came before the Court for hearing on October 22, 2019 at 9:30 a.m. 

upon Creditor Theodore Roberts’s Renewed Motion to Dismiss Case or in the 

Alternative, for Relief from the Automatic Stay (ECF No. 24) (the “Motion”), and 

Debtor’s Response in Opposition (ECF No. 32) (the “Response”). Upon consideration 

of the Motion, the Response, and the record in this case, the Court finds that this case 

was filed ten days before a state court-ordered sale pursuant to a final judgment of 

ORDERED in the Southern District of Florida on October 25, 2019.

Scott M. Grossman, Judge

United States Bankruptcy Court

_____________________________________________________________________________

Case 19-19710-SMG Doc 35 Filed 10/25/19 Page 1 of 2
2 

specific performance, and that this case is a two-party dispute between the Debtor 

and the movant, in which the Debtor is seeking relief from the state court judgment. 

The Rooker-Feldman doctrine, however, prohibits a collateral attack on the state 

court judgment in this Court. Target Media Partners v. Specialty Mktg. Corp., 881 

F.3d 1279, 1285–86 (11th Cir. 2018). For these reasons, and those stated orally on 

the record in open court, cause exists under 11 U.S.C. § 707(a) to dismiss this case. 

Accordingly, it is ORDERED that: 

1. The Motion is GRANTED. 

2. This case is DISMISSED. 

3. Creditor Theodore Roberts’s Objection to Debtor’s Claimed Homestead 

Exemption, (ECF No. 25), set for hearing on November 13, 2019 is DENIED as moot 

and the November 13 hearing is cancelled. 

# # # 

Copies furnished to: 

Jason Slatkin, Esq., who must serve a copy of this Order on all interested parties and 

file a certificate of service.

Case 19-19710-SMG Doc 35 Filed 10/25/19 Page 2 of 2
EXHIBIT 10.10


 


 


The Landmark
Bancorp, Inc. Compensation Committee oversees the bonuses for all
executive officers.  Individual bonus
awards are made pursuant to an annual cash bonus plan that is recommended by
the Compensation Committee and was approved by the full board.  Potential bonus awards are based on
achievement of certain objective criteria, including a minimum threshold of 4%
earnings per share growth with 10% growth required to receive the maximum bonus
amount related to earnings per share and a minimum threshold on return on
average equity is 9% with the top tier of the goal at 12% and the return on
average assets has minimum and maximum threshold of 0.8% and 1.25%
respectively.  Additionally, the
Compensation Committee and the board consider subjective performance measures
in addition to objective measures, which subjective component comprises up to
forty percent of the potential bonus award for each executive officer.
EXHIBIT 32.2


                           SECTION 1350 CERTIFICATION


     In connection with the Quarterly Report of Flickering Star Financial,  Inc.
(the  "Company")  on Form 10-QSB for the  quarter  ending June 30, 2006 as filed
with the Securities and Exchange  Commission on the date hereof (the  "Report"),
I, Gerald W.  Quealy,  Treasurer  and Chief  Financial  Officer of the  Company,
certify,  pursuant to 18 U.S.C. Section 1350, as adopted pursuant to Section 906
of the Sarbanes-Oxley Act of 2002, that, to my knowledge:

     (1)  The Report fully  complies with the  requirements  of section 13(a) or
          15(d) of the Securities Exchange Act of 1934; and

     (2)  The  information  contained  in the  Report  fairly  presents,  in all
          material respects,  the financial  condition and results of operations
          of the Company.


Date: August 11, 2006



                                        By: /s/ GERALD W. QUEALY
                                            ___________________________
                                                Gerald W. Quealy
                                                Treasurer and
                                                Chief Financial Officer
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#           The Mirror Lake fractured-rock research site: A multidisciplinary research effort in characterizing ground-water flow and chemical transport in fractured rock      

      August 1, 1995    

View Document

No abstract available.

## Citation Information

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                  -              Connect           

####             Allen M. Shapiro, Ph.D. (Former Employee)          

##### Research Hydrologist

Water Resources Mission Area

## Related Content

####             Allen M. Shapiro, Ph.D. (Former Employee)          

##### Research Hydrologist

Water Resources Mission Area

### Study Area

### Contact

####               Ecosystems Mission Area Headquarters          

12201 Sunrise Valley DrReston, VA20192United States

### Explore Search

                  - United States
                  - mirror lake
                  - New Hampshire

View All **
## Breadcrumb

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#           A multidisciplinary study of the Lower Cretaceous Cedar Mountain Formation, Mussentuchit Wash, Utah: a determination of the paleoenvironment and paleoecology of the Eolambia caroljonesa dinosaur quarry      

      January 1, 2007    

A quarry within the Cedar Mountain Formation in Mussentuchit Wash, Emery County, Utah, produced a fossil assemblage containing the remains of at least eight juvenile iguanodontid dinosaurs (Eolambia caroljonesa). The Cedar Mountain Formation lies stratigraphically between the Tithonian-Berriasian (Upper Jurassic) Brushy Basin Member of the Morrison Formation and the Cenomanian (Upper Cretaceous) Dakota Formation. Detailed stratigraphic, sedimentological, geochronological, palynological, and paleontological data have been collected along a measured section at the site of the Cifelli #2 Eolambia caroljonesa Quarry. These data provide a chronostratigraphic and a biostratigraphic framework for the Cedar Mountain Formation and allow a detailed reconstruction of the paleoenvironment and the paleoecology of the local paleogeographic area from which E. caroljonesa have been recovered. Three 40Ar/39Ar ages ranging from 96.7 to 98.5 Ma have been obtained three stratigraphically distinct altered volcanic ash layers within the Mussentuchit Member, one of which passes through the E. caroljonesa quarry, that indicate that the quarry is latest Albian in age and that the stratigraphic boundary between the Mussentuchit Member of the Cedar Mountain Formation and the overlying Dakota Formation is at or near the Albian/Cenomanian boundary. Sedimentological and biostratigraphic data suggest that significant long-term and short-term climatic changes are recorded in the Cedar Mountain Formation. During deposition of the lower part of the formation, climatic conditions were warm and arid to semi-arid. During deposition of the upper part of the formation, conditions became more humid. The progressive change in climatic conditions was probably related to the transgression of the Mowry Sea from the north. Cyclic sedimentation in the Mussentuchit Member suggests high-frequency changes from wet to dry periods. ?? 2007 Elsevier Ltd. All rights reserved.

## Citation Information
# L_2004320EN.01001401.xml

| 21.10.2004 | EN | Official Journal of the European Union | L 320/14 |
| --- | --- | --- | --- |

21.10.2004

EN

Official Journal of the European Union

L 320/14

---

COMMISSION REGULATION (EC) No 1820/2004

of 20 October 2004

amending Regulation (EC) No 2208/2002 laying down detailed rules for applying Council Regulation (EC) No 814/2000 on information measures relating to the common agricultural policy

THE COMMISSION OF THE EUROPEAN COMMUNITIES,

Having regard to the Treaty establishing the European Community,

Having regard to Council Regulation (EC) No 814/2000 of 17 April 2000 on information measures relating to the common agricultural policy (1), and in particular Article 9 thereof,

Whereas:

| (1) | Commission Regulation (EC) No 2208/2002 (2), provides for a call for proposals to ensure that the grants provided for in Regulation (EC) No 814/2000 receive the widest publicity and that the best measures are selected. The call for proposals must be published by 31 July each year. In the interests of sound administration, connected, in particular, with the extension of the scheme provided for in Regulation (EC) No 814/2000 to citizens of the new Member States, that date should be put back by three months. |
| --- | --- |

(1)

Commission Regulation (EC) No 2208/2002 (2), provides for a call for proposals to ensure that the grants provided for in Regulation (EC) No 814/2000 receive the widest publicity and that the best measures are selected. The call for proposals must be published by 31 July each year. In the interests of sound administration, connected, in particular, with the extension of the scheme provided for in Regulation (EC) No 814/2000 to citizens of the new Member States, that date should be put back by three months.

| (2) | Regulation (EC) No 2208/2002 should therefore be amended. |
| --- | --- |

(2)

Regulation (EC) No 2208/2002 should therefore be amended.

| (3) | The measures provided for in this Regulation are in accordance with the opinion of the EAGGF Committee, |
| --- | --- |

(3)

The measures provided for in this Regulation are in accordance with the opinion of the EAGGF Committee,

HAS ADOPTED THIS REGULATION:

Article 1

In Article 3 of Regulation (EC) No 2208/2002, the date 31 July is hereby replaced by 31 October.

Article 2

This Regulation shall enter into force on the third day following that of its publication in the Official Journal of the European Union.

This Regulation shall be binding in its entirety and directly applicable in all Member States.

Done at Brussels, 20 October 2004.

For the Commission

Franz FISCHLER

Member of the Commission

---

(1)  
  OJ L 100, 20.4.2000, p. 7.

1

(2)  
  OJ L 337, 13.12.2002, p. 21.

2

---
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#           Modeling groundwater nitrate concentrations in private wells in Iowa      

      August 5, 2015    

Contamination of drinking water by nitrate is a growing problem in many agricultural areas of the country. Ingested nitrate can lead to the endogenous formation of N-nitroso compounds, potent carcinogens. We developed a predictive model for nitrate concentrations in private wells in Iowa. Using 34,084 measurements of nitrate in private wells, we trained and tested random forest models to predict log nitrate levels by systematically assessing the predictive performance of 179 variables in 36 thematic groups (well depth, distance to sinkholes, location, land use, soil characteristics, nitrogen inputs, meteorology, and other factors). The final model contained 66 variables in 17 groups. Some of the most important variables were well depth, slope length within 1 km of the well, year of sample, and distance to nearest animal feeding operation. The correlation between observed and estimated nitrate concentrations was excellent in the training set (r-square = 0.77) and was acceptable in the testing set (r-square = 0.38). The random forest model had substantially better predictive performance than a traditional linear regression model or a regression tree. Our model will be used to investigate the association between nitrate levels in drinking water and cancer risk in the Iowa participants of the Agricultural Health Study cohort.

## Citation Information

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### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

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                  - iowa

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