alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
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#           Landslide inventory for the Little North Santiam River Basin, Oregon      

      January 1, 2010    

This geodatabase is an inventory of existing landslides in the Little North Santiam River Basin, Oregon (2009). Each landslide feature shown has been classified according to a number of specific characteristics identified at the time recorded in the GIS database. The classification scheme was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009).  Several significant landslide characteristics recorded in the database are portrayed with symbology on this map. The specific characteristics shown for each landslide are the activity of landsliding, landslide features, deep or shallow failure, type of landslide movement, and confidence of landslide interpretation. These landslide characteristics are determined primarily on the basis of geomorphic features, or landforms, observed for each landslide. This work was completed as part of the Master's thesis "Turbidity Monitoring and LiDAR Imagery Indicate Landslides are Primary Source of Suspended-Sediment Load in the Little North Santiam River Basin, Oregon, Winter 2009-2010" by Steven Sobieszczyk, Portland State University and U.S. Geological Survey. Data layers in this geodatabase include: landslide deposit boundaries (Deposits); field-verfied location imagery (Photos); head scarp or scarp flanks (Scarp_Flanks); and secondary scarp features (Scarps).The geodatabase template was developed by the Oregon Department of Geology and Mineral Industries (Burns and Madin, 2009).

## Citation Information

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                  -              Connect           

#### Steven Sobieszćzyk

##### Media Lead - Natural Hazards

Communications and Publishing

##### Hydrologist/PIO2

Wildland Fire Science

ssobie@usgs.gov

503-853-3425

## Related Content

#### Steven Sobieszćzyk

##### Media Lead - Natural Hazards

Communications and Publishing

##### Hydrologist/PIO2

Wildland Fire Science

ssobie@usgs.gov

503-853-3425

### Study Area

### Contacts

#### Steven Sobieszćzyk

##### Media Lead - Natural Hazards

Communications and Publishing

##### Hydrologist/PIO2

Wildland Fire Science

ssobie@usgs.gov

503-853-3425

### Explore Search

                  - Natural Hazards
                  - United States
                  - Little North Santiam River Basin
                  - Oregon

View All **
Case 20-14205-PGH Doc 43 Filed 08/03/20 Page 1 of 3
Case 20-14205-PGH Doc 43 Filed 08/03/20 Page 2 of 3
Case 20-14205-PGH Doc 43 Filed 08/03/20 Page 3 of 3
----

| (1) | The Annual Report on Form 10-K for the period ending December 31, 2012 of FindEx.com, Inc. (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 FindEx.com, Inc. |
|-----|----------------------------------------------------------------------------------------------------------------------------------------------------------|

|   | By:    | /s/ Steven Malone                                      |
|--------|--------|--------------------------------------------------------|
|   |   | Steven Malone                                          |
|   |   | President                                              |
|   |   | Chief Executive Officer (Principal Executive Officer)  |
|   |   | Chief Financial Officer (Principal Accounting Officer) |

----
Exhibit
      32.1





**CERTIFICATION
      OF PRINCIPAL EXECUTIVE OFFICER**


**PURSUANT
      TO**


**18
      U.S.C. SECTION 1350,**


**AS
      ADOPTED PURSUANT TO**


**SECTION
      906 OF THE SARBANES-OXLEY ACT OF 2002**





The
      undersigned hereby certifies, pursuant to, and as required by, 18 U.S.C. Section
      1350, as adopted pursuant to Section 906 of the Sarbanes-Oxley Act of 2002,
      that
      the Quarterly Report of Vista International Technologies, Inc. (the “Company”)
      on Form 10-Q for the period ended September 30, 2008 fully complies with the
      requirements of Section 13(a) or 15(d) of the Securities Exchange Act of 1934,
      as amended, 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 the Company.





Dated:
      November 14, 2008





By:
            */s/
                Barry J. Kemble*Barry
                J. Kemble
              Chief
                Executive Officer
UNITED STATES BANKRUPTCY COURT

SOUTHERN DISTRICT OF FLORIDA

FORT LAUDERDALE DIVISION

In re: CASE NO.: 10-28935-SMG

Global Energies, LLC, CHAPTER 7

Debtor(s).

____________________________________/

ORDER OF RECUSAL

This case came before the Court sua sponte. Upon consideration, the Court 

must recuse itself from this case pursuant to 28 U.S.C. § 455(a). Accordingly, it is 

ORDERED that:

1. I hereby recuse myself from this bankruptcy case and any associated 

adversary proceedings.

2. Pursuant to Local Rule 1073-1(B), this bankruptcy case and any 

associated adversary proceedings are hereby referred to the Clerk of the Court for 

reassignment and transfer to another Judge.

ORDERED in the Southern District of Florida on December 13, 2019.

Scott M. Grossman, Judge

United States Bankruptcy Court

_____________________________________________________________________________

Case 15-01447-RAM Doc 517 Filed 12/13/19 Page 1 of 2
2

3. The Clerk of the Court is directed to provide all interested parties with 

the Notice of Reassignment and Transfer.

4. The current trustee Barry Mukamal will remain as trustee. 

###

Copies Furnished to:

AUST 

Barry E Mukamal, Trustee

All other interested parties and creditors by the Clerk of Court

Case 15-01447-RAM Doc 517 Filed 12/13/19 Page 2 of 2
This section of the FEDERAL REGISTER

contains editorial corrections of previously

published Presidential, Rule, Proposed Rule,

and Notice documents. These corrections are

prepared by the Office of the Federal

Register. Agency prepared corrections are

issued as signed documents and appear in

the appropriate document categories

elsewhere in the issue.

Corrections Federal Register

62927

Vol. 60, No. 235

Thursday, December 7, 1995

FEDERAL COMMUNICATIONS

COMMISSION

47 CFR Part 80

[PR Docket No. 93-133, FCC 95-447]

Maritime Communications

Correction

In rule document 95–28826 beginning

on page 58243, in the issue of Monday,

November 27, 1995, make the following

correction:

§80.1065 [Corrected]

On page 58245, in the second column,

in §80.1065 (b)(5)(iii), in the second

line, ‘‘§8.933.’’ should read ‘‘§80.933.’’.

BILLING CODE 1505–01–D

DEPARTMENT OF HOUSING AND

URBAN DEVELOPMENT

Office of the Assistant Secretary for

Policy Development and Research

[Docket No. FR-3960-N-01]

Notice of Request for Cooperative

Agreement Applications for the

Community Renaissance Fellows

Program

Correction

In notice document 95–29228

beginning on page 61634 in the issue of

Thursday, November 30, 1995, make the

following correction:

On page 61634, in the second column,

under FOR FURTHER INFORMATION

CONTACT, the last line should read

‘‘JanelR.lKaradbil@hud.gov’’.

BILLING CODE 1505–01–D

DEPARTMENT OF JUSTICE

Drug Enforcement Administration

Herman E. Walker, Jr., M.D.;

Revocation of Registration

Correction

In notice document 95–24949,

beginning on page 52705, in the issue of

Tuesday, October 10, 1995, make the

following correction:

On page 52707, in the second column,

the second paragraph, the last line,

‘‘832’’ should read ‘‘823.’’

BILLING CODE 1505–01–D
**Exhibit 31.2**
 
 **CERTIFICATIONS OF CHIEF FINANCIAL OFFICER**
 **UNDER**
 **SECTION 302 OF THE SARBANES-OXLEY ACT**
 
 I, Michael J. Lewis, Chief Financial Officer of Collectors Universe, Inc., certify that:
 
 1.
I have reviewed this annual report on Form 10-K of Collectors Universe, Inc., for the fiscal year ended June 30, 2004; 
 2.
Based on my knowledge, this report does not contain any untrue statement of a material fact or omit to state a material fact necessary to make the statements made, in light of the circumstances under which such statements were made, not misleading with respect to the period covered by this report; 
 3.
Based on my knowledge, the financial statements, and other financial information included in this report, fairly present in all material respects the financial condition, results of operations and cash flows of the registrant as of, and for, the periods presented in this report. 
 4.
The registrants other certifying officer and I are responsible for establishing and maintaining disclosure controls and procedures (as defined in Rules 13a-15(e) and 15d-15(e) of the Exchange Act) for the registrant and we have: 
 (a)
designed such disclosure controls and procedures, or caused such disclosure controls and procedures to be designed under our supervision, to ensure that material information relating to the registrant, including its consolidated subsidiaries, is made known to us by others within those entities, particularly during the period in which this report is being prepared; 
 (b)
evaluated the effectiveness of the registrants disclosure controls and procedures and presented in this report our conclusions about the effectiveness of the disclosure controls and procedures as of the end of the period covered by this report based on such evaluation; and 
 (c)
disclosed in this report any change in the registrant's internal control over financial reporting that occurred during the registrant's most recent fourth fiscal quarter that has materially affected, or is reasonably likely to materially affect, the registrant's internal control over financial reporting. 
 5.
The registrants other certifying officer and I have disclosed, based on our most recent evaluation of internal control over financial reporting, to the registrants auditors and the audit committee of the registrants board of directors (or persons performing the equivalent function): 
 (a)
all significant deficiencies and material weaknesses in the design or operation of internal control over financial reporting which are reasonably likely to adversely affect the registrants ability to record, process, summarize and report financial information; and 
 (b)
any fraud, whether or not material, that involves management or other employees who have a significant role in the registrants internal control over financial reporting. 
 
 Date: September 24, 2004/s/ MICHAEL J. LEWISMichael J. LewisChief Financial Officer
Order entered April 27 , 2020

In The 

### Court of Appeals Fifth District of Texas at Dallas
No. 05
- 19
- 01378
- CR ENRIQUESINGER GARCIA , Appellant

V. THE STATE OF TEXAS, Appellee On Appeal from the 29 6th Judicial District Court

Collin County, Texas Trial Court Cause No. 296
- 80082
- 2018

O RDER Appellant, who was convicted of continuous sexual abuse of a child under
fourte e n years of age , filed his brief on April 21 , 2020 . In his brief, appellant
identi fie s t he victi m by name while quoting a portion of the record

. This Court does not allow a party to file a brief that discloses the names of victims or witnesses who were children at the time of the offen ses , or t he name s of any other
children discussed or i dentified at trial

. Se e T EX
. R. A PP
. P . 9. 10(b) (“Unless a
court orders otherwise, an electronic or paper filing w ith the court, including thecontents of any appendices, must not contain sensitive dat a.”), id. 9.10(a)(3)

(“ Sensitive Data Defined. Sensiti ve data consists of . . . a birth date, a h ome address, and the name of a ny person who was a minor at the time the offense was committed.”). Accordingly, we STRIKE appellant’s brief.
We ORDE R appellant to file, within TEN DAYS of the date of this order,

a n amended brief that id entifies the victim and a ny other s who were children at the time of this or any other off ense either generically (fo r example, “victim” ) or by
initials on ly, including when quo ting relevan t portions of the record, giving a

statement of the ca se, or atta ching an appendix.
We D IRECT the Clerk to send copies of this order to Robert Herrington and
the Collin County District A ttorney

.

/s/ BILL PEDERSEN, III JUSTICE
## Breadcrumb

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#           Petrology of the Caribou Mountain Pluton, Klamath Mountains, California      

      February 1, 1992    

The Caribou Mountain pluton is a small trondhjemitic body that intruded semipelitic schist of the Stuart Fork terrane in late Middle Jurassic to Early Cretaceous time. Its emplacement followed the intrusion of an adjoining body of hornblende quartz diorite called the Middle Fork pluton and the mode of its emplacement was as an asymmetric ballooning diapir (Davis, 1963), as shown by concentric foliation, radial late-stage dikes, foliated enclaves, and folded blocks of schlieren-banded tonalite. Coarse-grained hornblende-bearing trondhjemite is the dominant rock type in the Caribou Mountain pluton, and it is called the ‘main trondhjemite’. It was followed by medium-grained ‘late trondhjemite’ and by late-stage trondhjemitic and granodioritic dikes. All the trondhjemitic rock types are characterized by low alkali contents, high light rare earth elements, low initial 87Sr/86Sr, and low δ18O. However, the late trondhjemite has higher Na2O and a higher initial 87Sr/86Sr value than the main trondhjemite, and the two units cannot be related by fractional crystallization. The late granodioritic dikes are richer in Ba, Rb, Y, and Sc than the late trondhjemite and probably reflect assimilation of Stuart Fork metasedimentary rocks by late-stage trondhjemitic magma.

Mafic enclaves in the main trondhjemite contain xenocrysts of quartz and plagioclase derived from the host by magma mixing. The enclaves have K2O, Ba, and Rb contents similar to, or higher than those of the host rocks. Their rare earth element (REE) patterns display strong middle REE enrichment caused by accumulation of hornblende, probably as the result of filter pressing.

The main trondhjemite cannot be derived from Middle Fork magma because the initial 87Sr/86Sr of the Middle Fork pluton is lower than that of the trondhjemite. The absence of parental mafic magmas of appropriate composition suggests that the Caribou Mountain trondhjemitic magmas formed by partial melting of an amphibolitic source rock compositionally similar to low-K tholeiite.

## Citation Information

### Study Area

### Explore Search

                  - United States
                  - california
                  - Caribou Mountain
                  -  Klamath Mountains

View All **
AGENDA

Meeting Title: EPA and HHT Overview

Date: October 22, 2014

Time: 11 a.m. (ET)

Location: EPA HQ

Clinton Building South

1200 Pennsylvania Avenue NW

Washington DC 20460

Meeting Owner: VP Berger

Attendees: VP Berger, Julius Banks, Rafael Sanchez

Tentative: Edward Messina, Rick Duffy

Purpose of Meeting: Share organizational structure, process and product pipeline.

Desired Results: 

 Better understanding of each others’ business

 Assessment of capacity and promise times

 Opportunities for HHT to help improve communication process of projects and timelines

Meeting Cost: 3 of attendees X $150/hr avg. X Length of Meeting 1 = $450

Start time/End time Agenda Topics Member 

Responsible

11:00 a.m.  Thank members for being on time

 Restate purpose of meeting and desired result

11:05 a.m.  HNI/HHT Overview

– Product in review and coming

VP Berger

11:20 a.m.  Certification 

– Process

– Throughput time

– Capacity

Julius Banks

11:40 a.m.  NSPS Pending ruling and impact on process/capacity (if any) Julius

11:50 a.m.  Q&A All

 Review the decision records and gain consensus.

 Review the action items for follow up who is responsible.

12:00 Noon  Adjourn

Additional Instructions:

 Turn off cell phones





Agenda should be sent out 24 hours in advance of meeting start
*Pursuant to Local Rule 47.5, the Court has determined that

this opinion should not be published and is not precedent except

under the limited circumstances set forth in Local Rule 47.5.4.

IN THE UNITED STATES COURT OF APPEALS

FOR THE FIFTH CIRCUIT

 

No. 95-50388

 

UNITED STATES OF AMERICA,

Plaintiff-Appellee,

versus

ANTONIO MARTINEZ-CORTEZ,

Defendant-Appellant.

 

Appeal from the United States District Court for the

Western District of Texas

EP-94-CA-187-H

 

May 7, 1996

Before GARWOOD, HIGGINBOTHAM and BENAVIDES, Circuit Judges.*

PER CURIAM:

After considering the briefs and record, the Court concludes

that the district court correctly denied relief under 28 U.S.C. §

2255. We are in essential agreement with the district court’s

reasoning. It is clear that the prejudice prong of Strickland v.

Washington, 466 U.S. 668 (1984), is not met on the undisputed facts

here. There was no need for an evidentiary hearing.
2

AFFIRMED
UNITED STATES BANKRUPTCY COURT

SOUTHERN DISTRICT OF FLORIDA

MIAMI DIVISION

CASE NO.: 19-21621-BKC-AJC

PROCEEDING UNDER CHAPTER 13

IN RE:

MARY Z MIRIAN

_____________________________/

NOTICE CONTINUING DEBTOR'S MOTION TO MODIFY CONFIRMED PLAN

YOU ARE HEREBY NOTIFIED that the Debtor's Motion to Modify Confirmed Plan has been 

continued to November 17, 2020 at 9:00 AM by TELEPHONE through CourtSoutions LLC. To 

participate through CourtSolutions, you must make a reservation in advance no later than 3:00 p.m., one 

business day before the date of the hearing. Reservations should be arranged online at 

https://www.court-solutions.com If a party is unable to register online, a reservation may also be made by 

telephone at (917)746-7476.

I HEREBY CERTIFY that a true and correct copy of the foregoing Notice Continuing Debtor's 

Motion to Modify Confirmed Plan was mailed to those parties listed on this 2nd day of November, 2020.

DEBTOR

_____________________________________ /s/ Nancy K. Neidich

NANCY K. NEIDICH, ESQUIRE

STANDING CHAPTER 13 TRUSTEE

P.O. BOX 279806

MIRAMAR, FL 33027-9806

Case 19-21621-AJC Doc 91 Filed 11/02/20 Page 1 of 2
 NOTICE CONTINUING DEBTOR'S MOTION TO MODIFY CONFIRMED PLAN

CASE NO.: 19-21621-BKC-AJC

SERVICE LIST

COPIES FURNISHED TO:

NANCY K. NEIDICH

STANDING CHAPTER 13 TRUSTEE

P.O. BOX 279806

MIRAMAR, FL 33027-9806

DEBTOR

MARY Z MIRIAN

2750 NE 183 STREET APT 1811

NORTH MIAMI BEACH, FL 33160

ATTORNEY FOR DEBTOR

CAROLINA A. LOMBARDI, ESQUIRE

LEGAL SERV. OF GREATER MIAMI

4343 W FLAGLER STREET

SUITE 100

MIAMI, FL 33134

CAROLINA A. LOMBARDI, ESQUIRE IS HEREBY DIRECTED TO MAIL A CONFORMED COPY 

OF THIS NOTICE TO ALL CREDITORS AND INTERESTED PARTIES IMMEDIATELY UPON 

RECEIPT THEREOF.

Case 19-21621-AJC Doc 91 Filed 11/02/20 Page 2 of 2
## Breadcrumb

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#           Modelling the transport and deposition of ash following a magnitude 7 eruption: The distal Mazama tephra      

      September 2, 2022    

Volcanic ash transport and dispersion models (VATDMs) are necessary for forecasting tephra dispersal during volcanic eruptions and are a useful tool for estimating the eruption source parameters (ESPs) of prehistoric eruptions. Here we use Ash3D, an Eulerian VATDM, to simulate the tephra deposition from the ~ 7.7 ka climactic eruption of Mount Mazama. We investigate how best to apply a VATDM using the ESPs characteristic of a large magnitude eruption (M ≥ 7). We simplify the approach to focus on the distal deposit as if it were formed by a single phase of Plinian activity. Our results demonstrate that it is possible to use modern wind profiles to simulate the tephra dispersal from a prehistoric eruption; however, this introduces an inherent uncertainty to the subsequent simulations where we explore different ESPs. We show, using the well-documented distal Mazama tephra, that lateral umbrella cloud spreading, rather than advection–diffusion alone, must be included in the VATDM to reproduce the width of the isopachs. In addition, the Ash3D particle size distribution must be modified to simulate the transport and deposition of distal fine-grained (< 125 μm) Mazama ash. With these modifications, the Ash3D simulations reproduce the thickness and grain size of the Mazama tephra deposit. Based on our simulations, however, we conclude that the exact relationship between mass eruption rate and the scale of umbrella cloud spreading remains unresolved. Furthermore, for ground-based grain size distributions to be input directly into Ash3D, further research is required into the atmospheric and particle processes that control the settling behaviour of fine volcanic ash.

## Citation Information

## Related Content

                  -              Connect           

#### Larry G. Mastin, Ph.D.

##### Physical Volcanologist

Cascades Volcano Observatory

lgmastin@usgs.gov

360-993-8925

## Related Content

#### Larry G. Mastin, Ph.D.

##### Physical Volcanologist

Cascades Volcano Observatory

lgmastin@usgs.gov

360-993-8925

### Study Area

### Contact

#### USGS Volcano Science Center

1300 SE Cardinal CourtVancouver, WA38683United States

360-993-8900

### Explore Search

                  - canada
                  -  United States

View All **
## Breadcrumb

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#           Predicting earthquakes along the major plate tectonic boundaries in the Pacific      

      January 1, 1978    

In an article in the last issue of the Earthquake Information Bulletin ("Earthquakes and Plate Tectonics," by Henry Spall), we saw how 90 percent of the world's earthquakes occur at the margins of the Earth's major crustal plates. however, when we look at the distribution of earthquakes in detail, we see that a number of nearly aseismic regions, or seismic gaps, can be found along the present-day plate boundaries. Why is this? And can we regard these areas as being more likely to be the sites for future larger earthquakes than those segments of the plate boundaries that have ruptured recently. 

## Citation Information
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#           Preliminary geologic interpretation of a seismic reflection profile across the Queen Charlotte Island fault system, Dixon Entrance, Canada-United States      

      January 1, 1981    

View Document

View Plate

No abstract available.

## Citation Information
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#           Manual for leveling at gaging stations in North Carolina      

      January 1, 1981    

This manual was prepared to serve several purposes in the U.S. Geological Survey North Carolina District. This manual sets forth District policy as to frequency of levels, accuracy criteria, procedures for checking the datum and setting of the various types of gages, general rules to follow in establishing the original datum of a gage, and contains sample notes to be used as guides in level notekeeping. The manual also serves as a training tool in that the reasoning behind District policy is explained and reasons are given for following the recommended techniques to assist in a better understanding of the purpose of levels and maintaining gage datum.

## Citation Information

### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

### Explore Search

                  - United States
                  - North Carolina

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