text:
Q: express.js: show toastr message I'm trying to get Toastr library to work in my ExpressJS app! I scaffolded the app with the yeoman 'standard' Express Generator...
I've required the lib express-toastr and did the following:
in app.js:
const cookieParser = require('cookie-parser');
const session = require('express-session');
const flash = require('connect-flash');
const toastr = require('express-toastr');

app.use(cookieParser());
app.use(session( {secret: 'xxx', saveUninitialized: true, resave: true} ));
app.use(flash());
app.use(toastr());

in index.js
const express = require('express');
const router = express.Router();
const httpntlm = require('httpntlm');

router.post('/', function (req, res, next) {

    // parse inputs
    let user = req.body.user || "";
    let password = req.body.password || "";

    // save in session
    req.session.user = {user: user, password: password};

    // appropriate response to login attempt
    if (!req.session.user) {
        res.status(401).send();
    }
    else {
        req.toastr.success('Successfully logged in.', "You're in!");

        res.render('groups', {
            req: req
        });
    }
});

module.exports = router;

In index.jade
#{req.toastr.render()}

I'm loading these files in my <head> section:
link(rel='stylesheet', href='//cdnjs.cloudflare.com/ajax/libs/toastr.js/2.0.2/css/toastr.min.css')
script(src='/components/jquery/dist/jquery.min.js')
script(src='//cdnjs.cloudflare.com/ajax/libs/toastr.js/2.0.2/js/toastr.min.js')

Nothing is showing. What am I missing???
-- UPDATE! --
Here is my complete app.js file. I now try to use express-flash and making a dedicated route for showing a flash message. Still not working. Please help!
'use strict';

const express = require('express');
const path = require('path');
const favicon = require('serve-favicon');
const logger = require('morgan');
const cookieParser = require('cookie-parser');
const bodyParser = require('body-parser');

const expressSanitizer = require('express-sanitizer');

const login = require('./routes/login');
const apply = require('./routes/apply');
const admin = require('./routes/admin');

var session = require('express-session');
var flash = require('express-flash');

var app = express();

// view engine setup
app.set('views', path.join(__dirname, 'views'));
app.set('view engine', 'jade');

// uncomment after placing your favicon in /public
//app.use(favicon(path.join(__dirname, 'public', 'favicon.ico')));
app.use(logger('dev'));
app.use(bodyParser.json());
app.use(bodyParser.urlencoded({extended: false}));
app.use(cookieParser());
app.use(express.static(path.join(__dirname, 'public')));

app.use(session({
    cookie: { maxAge: 60000 },
    store: new session.MemoryStore,
    saveUninitialized: true,
    resave: 'true',
    secret: 'secret'
}));
app.use(flash());

// Route that creates a flash message using the express-flash module
app.all('/express-flash', function( req, res ) {
    req.flash('success', 'This is a flash message using the express-flash module.');
    res.redirect(301, '/');
});

// sanitize inputs
app.use(expressSanitizer());

app.use('/', apply);
app.use('/apply', apply);
app.use('/login', login);
app.use('/admin', admin);

// catch 404 and forward to error handler
app.use(function (req, res, next) {
    var err = new Error('Not Found');
    err.status = 404;
    next(err);
});

// error handlers

// development error handler
// will print stacktrace
if (app.get('env') === 'development') {
    app.use(function (err, req, res, next) {
        res.status(err.status || 500);
        res.render('error', {
            message: err.message,
            error: err
        });
    });
}

// production error handler
// no stacktraces leaked to user
app.use(function (err, req, res, next) {
    res.status(err.status || 500);
    res.render('error', {
        message: err.message,
        error: {}
    });
});

module.exports = app;

A: Try using this middleware in your app.js, I found this here
app.use(function (req, res, next)
{
    res.locals.toasts = req.toastr.render()
    next()
});

and then access locals in your view as follows:
#{toasts}

This worked for me.

A: So I am not familiar with your syntax in your index.jade file(!=). What does it do? If you change that line in your index to #{req.toastr.render()} it should work.


text:
DOJ Defies Order
PUBLISHED: 8:33 PM 10 May 2018
UPDATED: 8:45 PM 10 May 2018
Justice Department Agrees To Meet With Nunes, Gowdy, Won't Disclose Info
The Intelligence Committee has requested this information for months, but the DOJ was subpoenaed last week.
by Mark Megahan
Politics Republicans
Rosenstein managed to convince Kelly that turning things over to Chairman Nunes "could risk lives by potentially exposing the source, a U.S. citizen who has provided intelligence to the CIA and FBI."
In the latest episode of "as Washington turns," top officials at the Department of Justice invited ranking House lawmakers to sit down for a game of show and tell on Thursday. But amazingly, after dragging their feet for months, they still won't be bringing anything to show.
The DOJ continues to defy House Intelligence Committee Chairman Devin Nunes' (R-Ca.) order, claiming the documents are too dangerous to be seen. Instead, in a last-ditch effort to avoid criminal charges, they offered to verbally tell Nunes and ranking republican Trey Gowdy (R-S.C.) all they know. The lawmakers took them up on the offer but aren't making any promises until they hear what the Justice Department has to say.
Nunes is still seriously considering charging Attorney General Jeff Sessions and other DOJ and Federal Bureau of Investigation officials with contempt of Congress, for refusing to turn over the documents that the House Intelligence Committee Chairman wanted months ago.
When DOJ didn't respond to his polite request, he turned up the heat and demanded the materials with an official subpoena. Deputy Attorney General Rod Rosenstein again "declined" to respond.
On Tuesday, Rosenstein raced from the New York office, back to Washington, D.C. for a hastily convened West-wing meeting between himself, his deputy Ed O'Callahan, and John Kelly, the White House Chief of Staff.
Sources with knowledge of the conference report that Kelly was insistent on working out a solution that would appease the Intelligence Committee.
After presenting their case to Kelly for sitting on the information, which allegedly involves an individual source so sensitive that even top-secret-clearance-holding watchdogs might compromise him, they worked out a potential deal.
Dialing straight from the White House, they got Chairman Nunes and Rep. Gowdy both on speaker phone and offered the private briefing.
Exactly what "classified" information Nunes requested originally isn't known, because it was sealed, but the follow-up subpoena he issued last week demands "all documents referring or related to the individual referenced in Chairman Nunes' April 24, 2018, classified letter to Attorney General Sessions."
Nunes got a response letter telling him that the Justice Department "is not in a position to provide information responsive to your request regarding a specific individual."
The letter signed by Assistant AG Stephen Boyd stated, "disclosure of responsive information to such requests can risk severe consequences, including potential loss of human lives, damage to relationship with valued international partners, compromise of ongoing criminal investigations and interferences with intelligence activities."
Nunes went ballistic. "We discovered that they are not going to comply with our subpoena," he told Fox news. "The only thing left to do is we have to move quickly to hold the attorney general of the United States in contempt and that is what I will press for this week."
Nunes shot back, insisting that despite the language of the subpoena, the classified-document request did not refer to an individual. "They are citing spurious national security concerns to evade congressional oversight while leaking information to the Washington Post ostensibly about classified meetings," he scolded.
He wants the documents related to the Mueller investigation. He already knows who the individual is, he named him in the classified request.
"We're interested in documents that should have been given to us at least last fall. That's what we're looking for, and any claim to the contrary is wrong, and they know it's wrong."
"Congress has a right and a duty to get this information and we will succeed in getting this information, regardless of whatever fantastic stories the DOJ and FBI spin to the Post," he added.
House Majority Leader Kevin McCarthy (R-Ca.) weighed in on the issue, siding with Nunes. The DOJ is only fighting disclosure because it would make them look bad and prove they "are trying to discredit this president," he ventured on Laura Ingraham's show on Wednesday.
McCarthy pointed out that everyone has been waiting for the requested information a very long time. Out of 1.2 million pages of records that already should have been delivered, only "a couple thousand" were actually provided.
More important than that, he declares, Devin Nunes "runs a special committee, that deals with classified matters. The idea for people to say that they can't send them classified information doesn't hold."
The DOJ has used the same stunt already, McCarthy reminds everyone.
"Every time we've gotten information, lo and behold when they've said they had to hold something for us because it was classified and redacted, it had nothing to do with that, but it was an embarrassment to what these people are trying to do because they have their own personal beliefs, a few of them, and are trying to discredit this president.
Another thing that Chairman Nunes is furious about is the fact that the Justice Department won't even turn over the memo spelling out the Scope of Robert Mueller's powers and duties as a special counsel in the overarching Russia collusion investigation.

redpajama_set_name: RedPajamaCommonCrawl


The two travel together over the years, by airplane and truck, yet always yearn to return home together. One evening, Corky venture out at sunset. Jim begins to wonder where Corky is. Search with Jim, as he traverses the land looking for his best friend. Even while Corky is missing, Jim knows in his heart that he is still outdoors, exploring new things.
CORKY'S TRAVELS is the story about a lifelong bond between us and those we love, and the spirit that binds us together.
CORKY'S TRAVELS is also available on AMAZON.com in eBook and paperback formats!


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text:
EU Official Publications
Management: EU Official Publications
Finding Journal Articles
Key Databases
Statistics / Data sets
Official Publications Toggle Dropdown
UK Parliamentary Papers
Northern Ireland Official Publications
Reference Management Toggle Dropdown
Citing and referencing
Finding literature for your studies
The European Documentation Centre
As a European Documentation Centre (EDC), the Library at Queen's is entitled to receive most of the publications issued by the European Union. The current collection dates back to the early 1950s.
All European Union documents are shelved at JY in the compact shelving area of Floor 2 of the McClay Library. A selection of current material is displayed in the law and official publications current journals and reports area close to the Floor 2 Enquiry Desk.
Arrangement of the Collection
Within JY the publications are arranged under their issuing body with a general section at the beginning. Due to the quantity of Commission publications these are sub-divided by subject.
The classification assigned to the collection is JY10 – JY850. Some publications are arranged under their issuing body, e.g. JY100, European Parliament. Due to the quantity of documents produced, many are assigned a general classification, e.g. JY300, Enlargement.
Barcoded items in the official publications area are available for loan and can be borrowed from the main Borrower Services Desk.
Tracing EU Publications
EU Bookshop (Advanced Search)
The EU Bookshop search pages provide details of EU publications from 1952 onwards. PDF versions are usually available and free to access.
The Archive of European Integration (founded 2002) includes official European Community/European Union documents alongside independently-produced research materials and official European Community/European Union documents
Some Important Publications
Official Journal – Legislation (L series) and Information and Notices (C series).
Full text from the EUR-Lex website (1952 onwards)
The Legislation section (L) of the Official Journal contains secondary legislation enacted by the Commission and the Council. Publication of this legislation is mandatory. The Information & Notices section (C) of the Official Journal contains proposals for legislation and new research programmes, reports of activities of the main institutions, and official announcements. 'Calls for Proposals' relating to new research programmes are also published here. The Library no longer holds print copies of the Official Journal; issues for 1952-1957 are held on microfiche at MifB/JY50.P1 .
Preparatory acts (including Commission Documents)
Preparatory acts from the EUR-Lex website (1972 onwards)
These are documents used to prepare EU legislation and include Commission documents, Council positions, legislative proposals from the European Parliament and opinions from the European Economic and Social Committee and the Committee of the Regions.
These contain working documentation of the EU and include reports, communications and draft legislation. Each document is coded by document type, year and serial number.
Documents from the European Commission for example are coded and sometimes referred to as 'COM' documents. COM(2006) 370 is the 370th document issued in 2006. The Library holds COM documents for the period 1983-1999 are available on microfiche. Selected print copies of COM documents for the period up to 2002 are shelved in the EU collection by subject.
European Parliament website
The full text of debates along with other Parliamentary business can be found under the 'Plenary' heading in the European Parliament website.
Committee reports, opinions etc. from 2004 onwards can be found on the 'Committee' pages of the European Parliament website. Positions adopted by Parliament, joint texts etc from 1999 onwards can be found under the 'Plenary' heading. Print copies of European Parliament Working Documents and are held in the Library for the period 1976-1989. They are shelved in numerical order at JY100(P2). Documents for 1985-1997 are available on microfiche and are shelved at MIcfB JY100.P2
Economic and SocIal Committee – Opinions and Reports
ECSC website
The European Economic and Social Committee (EESC) is a consultative body of the European Union. Early Opinions and reports are shelved at MicfBJY91.P1 1984-2001. Later issues are available on the ECSC website.
Statistical Office Publications
Eurostat website
The Statistical Office produces a comprehensive range of EU statistical material, in its Eurostat series. The Library holds a selection of detailed tables and yearbooks organised by Eurostat theme, shelved at JY600. Key statistical information is available from the Eurostat website.
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Last Updated: Jul 3, 2019 9:29 AM
URL: https://libguides.qub.ac.uk/management
Subjects: Management
Tags: accounting, business, economics, finance, management


text:
Stella Maris Shellharbour
A Catholic Parish Primary School
About Stella Maris
Take a Virtual Tour of Our School
Our Catholic Identity and Parish
School Song & Prayer
Learning at Stella Maris
Co-Curricular Opportunities
Diverse Learning Needs
Assessment & Reporting
Pastoral Care & Wellbeing
Caring for the Whole Child
Positive Behaviours for Learning (PB4L)
Counselling & Other CatholicCare Services
Online Safety & Anti-Bullying Support
Term Dates & Bell Times
Kindergarten Transition to School
Policies, Procedures & Forms
School Fees Information
At Stella Maris Catholic Primary School, we assist students to work towards their full potential spiritually, physically, socially, intellectually and emotionally.
Pastoral Care is based on a deep respect for the dignity and uniqueness of the individual person as we are all made in the image of God (Genesis 1:27). By providing a strong sense of wellbeing and belonging, students, parents and staff of our school community are affirmed in their dignity and worth.
Pastoral care at Stella Maris is based on the ideals of a Christian community.
Pastoral care is love in action and is founded upon:
The loving concern God has always shown for his people throughout the history of salvation;
The value and uniqueness of the individual person created in the image of God;
The fact that 'the Catholic School is committed to the development of the whole person, since in Christ, the Perfect Man, all human values find their fulfilment and unity' (The Catholic School, 1977, n35);
The recognition that the ministry of each member of the school community contributes to the development of the climate of the school;
The understanding that, 'the entire effort of the Catholic teacher is oriented towards an integral formation of each student';
Our Catholic Education Diocese of Wollongong (CEDoW) 'Path to Life Framework', which contains 10 pathways for schools to help focus on areas of need in pastoral care through their school review and improvement process; and
Our Catholic Education Diocese of Wollongong (CEDoW) Student Pastoral Care and Wellbeing Policy.
Student wellbeing is of the utmost importance at Stella Maris. We are eager to ensure that all our students enjoy a healthy mind, body and spirit, and we integrate a number of programs to support this.
Counselling for students and their families is also available from CatholicCare. A school counsellor visits the school regularly for individual sessions as well as advising and supporting staff on appropriate programs for small groups and classes. Read more about the school counselling available to students.
If a staff member or parent feels that counselling may help a student, they need to discuss this with the principal who may discuss this with the counsellor and/or parent and arrange the appropriate permission forms and questionnaires to be completed by parents and staff.
Supporting Families
Living as an authentically Catholic community, we strive to be welcoming, inclusive and compassionate to all. In addition to the wellbeing of students at Stella Maris, the pastoral care and wellbeing of our parents and families is important to us and gives witness to our Catholic faith in action.
When families are in need of extra assistance, whether financial, emotional or otherwise, the school is here to provide support to families in a variety of ways while maintaining confidentiality and dignity.
Families are encouraged to speak with the principal or a member of the school leadership team if they feel they need support of any kind.
Read more about our partnership with parents in the Parent-School Partnership Framework
Counselling and Other CatholicCare Services
16 Wentworth Street
Shellharbour NSW 2529
info@smsdow.catholic.edu.au
About Us What We Offer Learning & Teaching Pastoral Care & Wellbeing For Parents & Carers News & Events
Latest Newsletter Compass Parent Login Frequently Asked Questions Enrolment Information Tour our School Contact Us
Stella Maris Shellharbour is a Catholic parish primary school in the Diocese of Wollongong.
We acknowledge and pay respect to the Dharawal people past and present, the traditional custodians of the land on which our school is built.
Website by Greenhouse Creative


text:
How to determine the ideal level of torque when specifying hinges
By Michelle Froese | October 16, 2019
By James Stroud, Commercial Product Manager
Southco, Inc.
Counterbalance technology can help reduce fatigue and improve operator efficiency by making heavy lids and panels on large pieces of equipment, such as
industrial copiers or blood centrifuges, feel lightweight.
One of the most common and widely used devices used today is the door hinge. It is so ubiquitous that it's often taken for granted. However, industrial and systems designers know that hinge technology offers a range of functionality and design options that can be used to improve even simple operations.
When designing an application that hinges two panels together — whether it's for simple enclosures or large, complex medical equipment — choosing the appropriate level of torque is essential for reliable operation and an intuitive end-user experience. A proper understanding of the different levels of torque and which applications they are best suited for can help device and systems designers choose the ideal hinge solution.
A closer look at torque
Torque has a relatively simple definition: It is the amount of energy or effort needed to move a door or panel from its closed position to an open position. The energy required depends on the weight of the door and the travel distance or arc of motion from closed to open (and back again). It's also important to consider function and the need to move the panel to one point in the arc of motion and hold it, or to have the motion go from fully open to completely closed.
Today's suppliers of hinge and positioning technology have portfolios that supply a "torque continuum," or a range of hinge products with different torque characteristics. Industrial designers can choose the ideal options to meet functionality, ergonomic requirements, quality, and unique features.
Holding doors open or closed, and moving panels securely into position without secondary supports or additional components
Creating an intuitive, zero-drift motion so that when a door or cover is opened, it holds a user-defined or predefined position securely, and with one motion
Providing specific tactile feedback to enhance the quality perception of the hinged device
Eliminating additional components (such as gas struts) or routine maintenance (tightening screws to maintain hinge resistance), thereby helping to lower overall costs
Providing a smoother, more substantial feel to opening and closing action, or to eliminate vibration The torque profile in a selected hinge can change – or elevate – the user's perception about a particular device
Consider the airplane tray table. Seating designers must use extremely lightweight plastic components in these applications to help airlines reduce fleet weight and conserve fuel. However, a tray table that flops down upon opening can lead a passenger to question the quality of the aircraft itself.
Newer innovations in counterbalance hinges use torsion bar technology. This is typically combined with cam and roller systems to meter out that energy through the full arc of motion. The result: opening a 200-lb engine hood will feel like lifting a door that weighs only 5 to 10 lbs.
Using a constant torque hinge with a factory-set level of resistance, the tray can be lowered by the passenger with just the right level of force, making the tray feel more substantial — and creating a positive perception of the inflight environment. Additionally, constant torque hinges designed and manufactured with high-quality materials retain the desired resistance after thousands of flights, without maintenance or replacement of parts.
Choosing the right hinge
The most common hinge is also the simplest: the standard, free-swinging hinge for opening and closing, with no resistance. It requires people to exert all the necessary energy to open or close a panel or uses gravity to complete the same operation.
Beyond this basic device, hinge technology can be broken down into four major categories, or "building blocks," based on the type of torque and controlled motion they supply.
Constant torque – enables the device to be held securely at every position along the range of motion
Detent and bistable – these hinges automatically drive to and hold a specific position, such as to 90 degrees
Damping – hinges that control the speed of motion automatically, without holding
Counterbalance – hinges with technology that enables heavier objects to feel lighter when opened, or pop open with a simple touch
Although many applications would require only one type of hinge, these different categories can also be combined into hinges that provide multi-functional positioning options in a single device. There are three key factors to consider when selecting the ideal hinge with the ideal torque profile: weight, center of gravity, and direction of movement.
Weight: If a panel is sufficiently light — under a few pounds, for example — then a simple hinge with no torque can offer the most cost-effective solution. As the weight of the door or panel increases, constant torque or detent hinges become more effective solutions. The level of torque in these hinges requires the user to exert some force, but prevents the door from falling. As a door panel's weight approaches 15 to 20 lbs, and upwards of 500 lbs, counterbalance technology provides a more effective option. With a counterbalance hinge, the hinge prevents the door from falling and makes that door feel lighter so that extra effort is not required to open or close the door.
Center of gravity: The center of gravity for a door or panel is affected by the width and shape of the panel, as well as the location of additional components that are attached to the panel. A light door that has a center of gravity far from the hinge point might feel the same as a heavier door with a center of gravity close to the hinge point. For example, a tractor hood covering an engine compartment might be narrow and made of lightweight material, but because it's so long, the center of gravity is farther out and requires more torque to lift it than a box or a panel that's only 12 or 18 inches deep.
Direction of movement: First, it is important to determine whether the panel or door is hinged vertically or horizontally. If the door is hinged vertically and moves side to side, it is working with gravity. The opposite is true for horizontally hinged panels. In some cases, a horizontally hinged door may also need to be moved and held into place in a vertical position. This way, a technician can access and work on the interior of a machine. The energy needed in this situation to move the door from horizontal to vertical will be greater, so a constant torque or counterbalance hinge might make more sense — and particularly when a technician is working underneath a door that needs to be held open overhead.
Constant torque positioning hinges, like Southco's E6 Series, provide reliable positioning with consistent operating efforts, and eliminate the need for secondary support components to hold doors or panels in position.
A secure hold: Constant torque
Constant torque hinges offer a device intuitive movement, so that the amount of effort to move it is just enough to respond to deliberate motion. However, the device will hold in place for basic touch interactions.
One example of this is a touchscreen monitor at a supermarket's checkout counter. A constant torque hinge attached to the monitor's base lets a user tilt the monitor up and down for optimum viewing and interaction. At the same time, tapping the icons on the screen can be performed without the screen moving from the desired position. Also, a constant torque hinge provides one-handed operation of the screen, rather than pushing a button or flipping a lever to position it.
While constant torque hinges have been available for some time, there are suppliers who continue to introduce new innovations in this technology. One-way, constant-torque hinges, for example, provide constant torque in only one direction of movement against gravity — while providing free-swinging motion in the other. This type of product can be useful in applications such as storage cabinets with large doors. By removing the friction from the hinge in one direction, the door can be easily opened, while torque applied in the other direction holds the door open for access.
Drive and hold: Detent hinges
Detent hinges provide specific motion and tactile feedback. The door or device is opened and locks into place at a preset angle, typically with a distinctive "click" that can be felt. These types of hinges are often useful for lightweight cabinet doors or other devices that must be consistently opened to remain out of the user's way.
Detent hinges require the user to keep moving the device until it reaches the right position for the working environment — say, at a preset angle of 90 degrees. Bistables are variations on detent hinges and offer a built-in spring mechanism that automatically drives the door or device to the preset angle once the door is open. This functionality is useful for doors, access panels, or covers that must be opened to a minimum angle for easy entry, or to avoid collisions with surrounding equipment.
A controlled opening: Damping hinges
A door, compartment, or other device using a damping hinge means it will move steadily to an open or closed position when force is exerted, rather than popping open or requiring the user to push it closed. This smooth, steady motion is becoming widely preferred in a number of high-end applications, such as car interiors, where the operator expects a more intuitive user experience.
For items, such as eyeglass storage compartments, USB port carriers, or other compartments that are opened and closed, damping hinges add to the user experience and present a high-tech, finely engineered interior.
Minimal effort required: Counterbalance
Counterbalance hinges expand the torque continuum by allowing heavy doors and panels to open or move easily. They incorporate spring mechanisms that store energy when the door or panel is closed. Then, on opening, the energy is released and balances the effort required to move the panel through its range of motion to a fully open position.
For applications where operators are routinely opening and closing heavy doors – industrial copiers are one example – counterbalance technology can help reduce fatigue and improve operator efficiency. For instance, a door with a symmetrical torque hinge may require 56 lbs of effort to open from fully closed to 90-degrees open. By using a counterbalance hinge, the energy required to open the door can be reduced to 3 lbs.
For applications that require the lifting of larger lids and panels, counterbalance torsion spring systems, such as Southco's CB counterbalance hinge series, can be used to neutralize the weight of heavy doors, providing motion control for easy and safer opening and closing.
For heavy doors, designers once used gas struts or other such devices, but these are prone to technical problems and failure over time. Counterbalance hinges are a more economical, single-device choice.
The newest counterbalance hinges can also incorporate a latch to support pop-up opening. So, when first opened, a heavy door will lift a few degrees, allowing the end-user to establish a firm grip on the panel. Newer innovations in counterbalance hinges use torsion bar technology to create the counterbalance energy, combined with cam and roller systems to meter out that energy through the full arc of motion.
The result: opening an 80-lb panel feels like lifting a door that weighs 5 lbs. Plus, the effort feels balanced throughout the whole range of opening and closing motions.
Value adds
Designers recognize that every time an end-user opens, closes, or moves a hinged device, the user is exerting a force and undergoing a distinctive tactile experience. New hinge technology that uses the full torque continuum offers designers the opportunity to create more sophisticated solutions for a variety of different applications.
Different types of hinges with different torque profiles can also be combined to satisfy multiple requirements. For example, detent and damping functionality can be combined in a single hinge, so that a door easily opens to a fixed position and clicks in place, and then moves on its own to the closed position when pushed shut.
The key to success is determining the use case for each application, which means deciphering the ideal ergonomics for opening, closing, and positioning a panel or door. To do so, user feedback is essential. Fortunately, well-established hinge suppliers have extensive experience working with end-users to determine the optimum solution and ideal torque for each application.
James Stroud is a commercial product manager for Southco, Inc. He has over 26 years of experience working in various roles supporting Southco, globally, including in Europe and Asia. In his current role, Stroud manages a portfolio of access hardware products, evaluates industry trends and market needs, and launches new solutions to further expand Southco's product line.


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text:
namespace flutter {

class FlutterWindowsEngine;

// An object managing the registration of an external texture.
// Thread safety: All member methods are thread safe.
class FlutterWindowsTextureRegistrar {
 public:
  explicit FlutterWindowsTextureRegistrar(FlutterWindowsEngine* engine,
                                          const GlProcs& gl_procs);

  // Registers a texture described by the given |texture_info| object.
  // Returns the non-zero, positive texture id or -1 on error.
  int64_t RegisterTexture(const FlutterDesktopTextureInfo* texture_info);

  // Attempts to unregister the texture identified by |texture_id|.
  // Returns true if the texture was successfully unregistered.
  bool UnregisterTexture(int64_t texture_id);

  // Notifies the engine about a new frame being available.
  // Returns true on success.
  bool MarkTextureFrameAvailable(int64_t texture_id);

  // Attempts to populate the given |texture| by copying the
  // contents of the texture identified by |texture_id|.
  // Returns true on success.
  bool PopulateTexture(int64_t texture_id,
                       size_t width,
                       size_t height,
                       FlutterOpenGLTexture* texture);

  // Populates the OpenGL function pointers in |gl_procs|.
  static void ResolveGlFunctions(GlProcs& gl_procs);

 private:
  FlutterWindowsEngine* engine_ = nullptr;
  const GlProcs& gl_procs_;

  // All registered textures, keyed by their IDs.
  std::unordered_map<int64_t, std::unique_ptr<flutter::ExternalTextureGL>>
      textures_;
  std::mutex map_mutex_;
};

};  // namespace flutter

#endif  // FLUTTER_SHELL_PLATFORM_WINDOWS_FLUTTER_WINDOWS_TEXTURE_REGISTRAR_H_

redpajama_set_name: RedPajamaGithub


We have a very advanced engineering program. Our education program is one of the best there is. And our football team is in the process of "restoring the glory." We have good basketball teams and last year our men were the Cinderella team at the National Championships. We spent a week as the target of jokes on the Jimmy Fallon Late Night Show.
UTC is best known for the Business Program that is offers. Also, the school offers various departments, giving students many options to choose from if they attend school here. With so many various departments, this gives students the opportunity to pick a major and/or minor of so many different possibilities.
UTC is known for its education program and the Physical Therapy department. It is also known for the surrounding outdoor active environment with plenty of places to go hiking, rock climbing, backpacking, or biking.
Our school is best known for the beautiful campus and also they amazing apartments we have! Most student, in fact come to UTC to be able to have their own apartment!
The business program is known for being one of the top 100 in the country and we are also known for having a really bad football team.
Oddly enough, my school is known for its beautiful housing. It also has a great program for Education majors.


This summer, Special Forces candidates will participate in the Robin Sage training exercise, held within 15 North Carolina counties as the final test of their Special Forces Qualification Course training.
Between July 21 and Aug. 1, approximately 100 of these students will participate in this exercise before graduating the course and moving on to their first assignments in the Army's Special Forces community. Robin Sage is a two-week exercise run eight times a year, once for each class of Special Forces candidates.
These candidates are students at the U.S. Army John F. Kennedy Special Warfare Center and School, based out of Fort Bragg.
The exercise's notional country of Pineland encompasses 15 counties in North Carolina including Alamance, Anson, Cabarrus, Chatham, Davidson, Guilford, Hoke, Montgomery, Moore, Randolph, Richmond, Rowan, Scotland, Stanly and Union counties. Throughout the exercise, Special Forces candidates and Robin Sage role-players not only conduct training missions such as controlled assaults and key-leader engagements, but also live, eat and sleep in these civilian areas.
All Robin Sage movements and events have been coordinated with public safety officials throughout and within the towns and counties hosting the training. Residents may hear blank gunfire and see occasional flares. Controls are in place to ensure there is no risk to persons or property. Residents with concerns should contact local law enforcement officials, who will immediately contact exercise control officials.
With the help of civilian authorities and local citizens, Robin Sage has been conducted since 1974; before that time, similar exercises were run under the names Devil's Arrow, Swift Strike and Guerilla USA.
• Formal written notification to the chiefs of law enforcement agencies in the affected counties, with a follow-up visit from a unit representative.
• All civilian and non-student military participants are briefed on procedures to follow if there is contact with law enforcement officials.
• Students will only wear civilian clothes if the situation warrants, as determined by the instructors, and will wear a distinctive armband during these instances. Personnel role-playing as Pineland law enforcement officers wear distinctive hats and armbands, as well.
• Training areas and vehicles used during exercises are clearly labeled.
Approximately 200 military service members from units across Fort Bragg will also support the exercise. These military members act as realistic opposing forces and guerrilla freedom fighters, also known as Pineland's resistance movement. These troops play a critical role in the training exercise. To add realism of the exercise, civilian volunteers throughout the state act as role-players. Participation by these volunteers is crucial to the success of this training, and past trainees attest to the realism they add to the exercise.
Robin Sage is the U.S. military's premiere unconventional warfare exercise and the final test of over a year's worth of training for aspiring Special Forces Soldiers. Candidates are placed in an environment of political instability characterized by armed conflict, forcing Soldiers to analyze and solve problems to meet the challenges of this "real-world" training.
During this exercise, these future Special Forces Soldiers must infiltrate areas in small groups and train guerilla forces to independently and effectively use tactical force to liberate Pineland by teaching them to communicate, move, fight and provide medical aid.
U.S. Army students who successfully complete this iteration of the Robin Sage exercise will graduate the Special Forces Qualification Course in a ceremony Aug. 9 in Fayetteville. In addition, foreign military soldiers participating in Robin Sage and the SFQC as part of exchange programs will graduate the course and return to their nation's military.
We appreciate the support and consideration the citizens of North Carolina extend to the Soldiers participating in the exercise and thank them for their understanding of any inconveniences the training may cause. Questions concerning the exercise should be referred to the U.S. Army John F. Kennedy Special Warfare Center and School Public Affairs Office at (910) 396-9394, or by e-mail at pao_swcs@soc.mil. The Robin Sage operations center, run by D Company, 1st Battalion, 1st Special Warfare Training Group (Airborne), can be reached at (910) 432-6455.
In the event of an emergency, please contact your local law enforcement agency.


text:
Городская усадьба Крутовских — жилой особняк в Яранске. Объект культурного наследия России, памятник архитектуры.

История
Памятник находится по адресу улица Кирова, 12. По смежной улице Свободы имеет номер 23. Дом был построен в середине XIX века яранским торговцем железоскобяным товаром В. И. Крутовских, позднее перешёл во владение его сына П. В. Крутовских. В советское и постсоветское время в здании кроме квартир располагалась прокуратура, юридическая консультация, Яранский районный суд.

Соседний, также двухэтажный полукаменный, дом по улице Свободы, 25 принадлежал брату В. И. Крутовских — . В начале XX века часть помещений занимал Дворянский клуб, позже Яранское уездное отделение государственного контроля. Ныне в нём располагаются жилые квартиры.

Памятник архитектуры
Угловой 2-этажный полукаменный дом. Первый этаж сложен из кирпича, второй — деревянный.

Примечания

Ссылки

Крутовских

redpajama_set_name: RedPajamaWikipedia


text:
The geochemistry of carbon is the study of the transformations involving the element carbon within the systems of the Earth. To a large extent this study is organic geochemistry, but it also includes the very important carbon dioxide. Carbon is transformed by life, and moves between the major phases of the Earth, including the water bodies, atmosphere, and the rocky parts. Carbon is important in the formation of organic mineral deposits, such as coal, petroleum or natural gas. Most carbon is cycled through the atmosphere into living organisms and then respirated back into the atmosphere. However an important part of the carbon cycle involves the trapping of living matter into sediments. The carbon then becomes part of a sedimentary rock when lithification happens.
Human technology or natural processes such as weathering, or underground life or water can return the carbon from sedimentary rocks to the atmosphere. From that point it can be transformed in the rock cycle into metamorphic rocks, or melted into igneous rocks. Carbon can return to the surface of the Earth by volcanoes or via uplift in tectonic processes. Carbon is returned to the atmosphere via volcanic gases.
Carbon undergoes transformation in the mantle under pressure to diamond and other minerals, and also exists in the Earth's outer core in solution with iron, and may also be present in the inner core.

Carbon can form a huge variety stable compounds. It is an essential component of living matter.
Living organisms can live in a limited range of conditions on the Earth that are limited by temperature and the existence of liquid water. The potential habitability of other planets or moons can also be assessed by the existence of liquid water.

Carbon makes up only 0.08% of the combination of the lithosphere, hydrosphere, and atmosphere. Yet it is the twelfth most common element there. In the rock of the lithosphere, carbon commonly occurs as carbonate minerals containing calcium or magnesium. It is also found as fossil fuels in coal and petroleum and gas. Native forms of carbon are much rarer, requiring pressure to form. Pure carbon exists as graphite or diamond.

The deeper parts of Earth such as the mantle are very hard to discover. Few samples are known, in the form of uplifted rocks, or xenoliths. Even fewer remain in the same state they were in where the pressure and temperature is much higher. Some diamonds retain inclusions held at pressures they were formed at, but the temperature is much lower at the surface. Iron meteorites may represent samples of the core of an asteroid, but it would have formed under different conditions to the Earth's core. Therefore, experimental studies are conducted in which minerals or substances are compressed and heated to determine what happens in similar conditions to the planetary interior.

The two common isotopes of carbon are stable. On Earth, carbon 12, 12C is by far the most common at 98.894%. Carbon 13 is much rarer averaging 1.106%. This percentage can vary slightly and its value is important in isotope geochemistry whereby the origin of the carbon is suggested.

Origins

Formation
Carbon can be produced in stars at least as massive as the Sun by fusion of three helium-4 nuclei: 4He + 4He + 4He --> 12C. This is the triple alpha process.
In stars as massive as the Sun, carbon 12 is also converted to carbon 13 and then onto nitrogen 14 by fusion with protons. 12C + 1H --> 13C + e+. 13C + 1H --> 14N. In more massive stars, two carbon nuclei can fuse to magnesium, or a carbon and an oxygen to sulfur.

Astrochemistry
In molecular clouds, simple carbon molecules are formed, including carbon monoxide and dicarbon. Reactions with the trihydrogen cation of the simple carbon molecules yield carbon containing ions that readily react to form larger organic molecules. Carbon compounds that exist as ions, or isolated gas molecules in the interstellar medium, can condense onto dust grains. Carbonaceous dust grains consist mostly of carbon. Grains can stick together to form larger aggregates.

Earth formation
Meteorites and interplanetary dust shows the composition of solid material at the start of the Solar System, as they have not been modified since its formation. Carbonaceous chondrites are meteorites with around 5% carbon compounds. Their composition resembles the Sun's minus the very volatile elements like hydrogen and noble gases.
The Earth is believed to have formed by the gravitational collapse of material like meteorites.

Important effects on Earth in the first Hadian Era include strong solar winds during the T-Tauri stage of the Sun. The Moon forming impact caused major changes to the surface. Juvenile volatiles outgased from the early molten surface of the Earth. These included carbon dioxide and carbon monoxide. The emissions probably did not include methane, but the Earth was probably free of molecular oxygen. The Late Heavy Bombardment was between 4.0 and 3.8 billion years ago (Ga). To start with, the Earth did not have a crust as it does today. Plate tectonics in its present form commenced about 2.5 Ga.

Early sedimentary rocks formed under water date to 3.8 Ga. Pillow lavas dating from 3.5 Ga prove the existence of oceans. Evidence of early life is given by fossils of stromatolites, and later by chemical tracers.

Organic matter continues to be added to the Earth from space via interplanetary dust, which also includes some interstellar particles. The amounts added to the Earth were around 60,000 tonnes per year about 4 Ga.

Isotope
Biological sequestration of carbon causes enrichment of carbon-12, so that substances that originate from living organisms have a higher carbon-12 content. Due to the kinetic isotope effect, chemical reactions can happen faster with lighter isotopes, so that photosynthesis fixes lighter carbon-12 faster than carbon-13. Also lighter isotopes diffuse across a biological membrane faster. Enrichment in carbon 13 is measured by delta 13C(o/oo) = [(13C/12C)sample/(13C/12C)standard - 1] * 1000.
The common standard for carbon is Cretaceous Peedee formation belemnite.

Stereoisomers
Complex molecules, in particular those containing carbon can be in the form of stereoisomers. With abiotic processes they would be expected to be equally likely, but in carbonaceous chondrites this is not the case. The reasons for this are unknown.

Crust
The outer layer of the Earth, the crust along with its outer layers contain about 1020 kg of carbon. This is enough for each square meter of the surface to have 200 tons of carbon.

Sedimentation
Carbon added to sedimentary rocks can take the form of carbonates, or organic carbon compounds. In order of source quantity the organic carbon comes from phytoplankton, plants, bacteria and zooplankton. However terrestrial sediments may be mostly from higher plants, and some oxygen deficient sediments from water may be mostly bacteria. Fungi and other animals make insignificant contributions. On the oceans the main contributor of organic matter to sediments is plankton, either dead fragments or faecal pellets termed marine snow. Bacteria degrade this matter in the water column, and the amount surviving to the ocean floor is inversely proportional to the depth. This is accompanied by biominerals consisting of silicates and carbonates. The particulate organic matter in sediments is about 20% of known molecules 80% of material that cannot be analysed. Detritivores consume some of the fallen organic materials. Aerobic bacteria and fungi also consume organic matter in the oxic surface parts of the sediment. Coarse-grained sediments are oxygenated to about half a meter, but fine grained clays may only have a couple of millimetres exposed to oxygen. The organic matter in the oxygenated zone will become completely mineralized if it stays there long enough.

Deeper in sediments where oxygen is exhausted, anaerobic biological processes continue at a slower rate. These include anaerobic mineralization making ammonium, phosphate and sulfide ions; fermentation making short chain alcohols, acids or methyl amines; acetogenesis making acetic acid; methanogenesis making methane, and sulfate, nitrite and nitrate reduction. Carbon dioxide and hydrogen are also outputs. Under freshwater, sulfate is usually very low, so methanogenesis is more important. Yet other bacteria can convert methane, back into living matter, by oxidising with other substrates. Bacteria can reside at great depths in sediments. However sedimentary organic matter accumulates the indigestible components.

Deep bacteria may be lithotrophes, using hydrogen, and carbon dioxide as a carbon source.

In the oceans and other waters there is much dissolved organic materials. These are several thousand years old on average, and are called gelbstoff (yellow substance) particularly in fresh waters. Much of this is tannins. The nitrogen containing materials here appear to be amides, perhaps from peptidoglycans from bacteria. Microorganisms have trouble consuming the high molecular weight dissolved substances, but quickly consume small molecules.

From terrestrial sources black carbon produced by charring is an important component. Fungi are important decomposers in soil.

Macromolecules
Proteins are normally hydrolysed slowly even without enzymes or bacteria, with a half life of 460 years, but can be preserved if they are desiccated, pickled or frozen. Being enclosed in bone also helps preservation. Over time the amino acids tend to racemize, and those with more functional groups are lost earlier. Protein still will degrade on the timescale of a million years. DNA degrades rapidly, lasting only about four years in water. Cellulose and chitin have a half life in water at 25° of about 4.7 million years. Enzymes can accelerate this by a factor of 1017. About 1011 tons of chiting are produced each year, but it is almost all degraded.

Lignin is only efficiently degraded by fungi, white rot, or brown rot. These require oxygen.

Lipids are hydrolysed to fatty acids over long time periods. Plant cuticle waxes are very difficult to degrade, and may survive over geological time periods.

Preservation
More organic matter is preserved in sediments if there is high primary production, or the sediment is fine-grained. The lack of oxygen helps preservation greatly, and that also is caused by a large supply of organic matter. Soil does not usually preserve organic matter, it would need to be acidified or water logged, as in the bog. Rapid burial ensures the material gets to an oxygen free depth, but also dilutes the organic matter. A low energy environment ensures the sediment is not stirred up and oxygenated. Salt marshes and mangroves meet some of these requirements, but unless the sea level is rising will not have a chance to accumulate much. Coral reefs are very productive, but are well oxygenated, and recycle everything before it is buried.

Sphagnum bog
In dead Sphagnum, sphagnan a polysaccharide with D-lyxo-5-hexosulouronic acid is a major remaining substance. It makes the bog very acidic, so that bacteria cannot grow. Not only that, the plant ensures there is no available nitrogen. Holocellulose also absorbs any digestive enzymes around. Together this leads to major accumulation of peat under sphagnum bogs.

Mantle
Earth's mantle is a significant reservoir of carbon. The mantle contains more carbon than the crust, oceans, biosphere, and atmosphere put together. The figure is estimated to be very roughly 1022 kg. Carbon concentration in the mantle is very variable, varying by more than a factor of 100 between different parts.

The form carbon takes depends on its oxidation state, which depends on the oxygen fugacity of the environment. Carbon dioxide and carbonate are found where the oxygen fugacity is high. Lower oxygen fugacity results in diamond formation, first in eclogite, then peridotite, and lastly in fluid water mixtures. At even lower oxygen fugacity, methane is stable in contact with water, and even lower, metallic iron and nickel form along with carbides. Iron carbides include Fe3C and Fe7C3.

Minerals that contain carbon include calcite and its higher density polymorphs. Other significant carbon minerals include magnesium and iron carbonates. Dolomite is stable above 100 km depth. Below 100 km, dolomite reacts with orthopyroxine (found in peridotite) to yield magnesite (an iron magnesium carbonate). Below 200 km deep, carbon dioxide is reduced by ferrous iron (Fe2+), forming diamond, and ferric iron (Fe3+). Even deeper pressure induced disproportionation of iron minerals produces more ferric iron, and metallic iron. The metallic iron combines with carbon to form the mineral cohenite with formula Fe3C. Cohenite also contains some nickel substituting for iron. This form or carbon is called "carbide". Diamond forms in the mantle below 150 km deep, but because it is so durable, it can survive in eruptions to the surface in kimberlites, lamproites, or ultramafic lamprophyres.

Xenoliths can come from the mantle, and different compositions come from different depths. Above 90 km (3.2 GPa) spinel peridotite occurs, below this garnet peridotite is found.

Inclusions trapped in diamond can reveal the material and conditions much deeper in the mantle. Large gem diamonds are usually formed in the transition zone part of the mantle, (410 to 660 km deep) and crystallise from a molten iron-nickel-carbon solution, that also contains sulfur and trace amounts of hydrogen, chromium, phosphorus and oxygen. Carbon atoms constitute about 12% of the melt (about 3% by mass). Inclusions of the crystallised metallic melt are sometimes included in diamonds. Diamond can be caused to precipitate from the liquid metal, by increasing pressure, or by adding sulfur.

Fluid inclusions in crystals from the mantle have contents that most often are liquid carbon dioxide, but which also include carbon oxysulfide, methane and carbon monoxide

Material is added by subduction from the crust. This includes the major carbon containing sediments such as limestone, or coal. Each year 2×1011 kg of CO2 is transferred from the crust to the mantle by subduction. (1700 tons of carbon per second).

Upwelling mantle material can add to the crust at mid oceanic ridges. Fluids can extract carbon from the mantle and erupt in volcanoes. At 330 km deep a liquid consisting of carbon dioxide and water can form. It is highly corrosive, and dissolves incompatible elements from the solid mantle. These elements include uranium, thorium, potassium, helium and argon. The fluids can then go on to cause metasomatism or extend to the surface in carbonatite eruptions. The total mid oceanic ridge, and hot spot volcanic emissions of carbon dioxide match the loss due to subduction: 2×1011 kg of CO2 per year.

In slowly convecting mantle rocks, diamond that slowly rises above 150 km will slowly turn into graphite or be oxidised to carbon dioxide or carbonate minerals.

Core
Earth's core is believed to be mostly an alloy of iron and nickel. The density indicates that it also contains a significant amount of lighter elements. Elements such as hydrogen would be stable in the Earth's core, however the conditions at the formation of the core would not be suitable for its inclusion. Carbon is a very likely constituent of the core. Preferential partitioning of the carbon isotope12C into the metallic core, during its formation, may explain why there seems to be more 13C on the surface and mantle of the Earth compared to other solar system bodies (−5‰ compared to -20‰). The difference can also help to predict the value of the carbon proportion of the core.

The outer core has a density around 11 cm−3, and a mass of 1.3×1024kg. It contains roughly 1022 kg of carbon.
Carbon dissolved in liquid iron affect the solution of other elements. Dissolved carbon changes lead from a siderophile to a lithophile. It has the opposite effect on tungsten and molybdenum, causing more tungsten or molybdenum to dissolve in the metallic phase. The measured amounts of these elements in the rocks compared to the Solar System can be explained by a 0.6% carbon composition of the core.

The inner core is about 1221 km in radius. It has a density of 13 g cm−3, and a total mass of 9×1022 kg and a surface area of 18,000,000 square kilometers. Experiments with mixtures under pressure and temperature attempt to reproduce the known properties of the inner and outer core. Carbides are among the first to precipitate from a molten metal mix, and so the inner core may be mostly iron carbides, Fe7C3 or Fe3C. At atmospheric pressure (100 kPa) the iron-Fe3C eutectic point is at 4.1% carbon. This percentage decreases as pressure increases to around 50 GPa. Above that pressure the percentage of carbon at the eutectic increases. The pressure on the inner core ranges from 330 GPa to 360 GPa at the centre of the Earth. The temperature at the inner core surface is about 6000 K. The material of the inner core must be stable at the pressure and temperature found there, and more dense than that of the outer core liquid. Extrapolations show that either Fe3C or Fe7C3 match the requirements. Fe7C3 is 8.4% carbon, and Fe3C is 6.7% carbon. The inner core is growing by about 1 mm per year, or adding about 18 cubic kilometres per year. This is about 18×1012kg of carbon added to the inner core every year. It contains about 8×1021 kg of carbon.

High pressure experimentation
In order to determine the fate of natural carbon containing substances deep in the Earth, experiments have been conducted to see what happens when high pressure, and or temperatures are applied. Such substances include carbon dioxide, carbon monoxide, graphite, methane, and other hydrocarbons such as benzene, carbon dioxide water mixtures and carbonate minerals such as calcite, magnesium carbonate, or ferrous carbonate. Under super high pressures carbon may take on a higher coordination number than the four found in sp3 compounds like diamond, or the three found in carbonates. Perhaps carbon can substitute into silicates, or form a silicon oxycarbide. Carbides may be possible.

Carbon
At 15 GPa graphite changes to a hard transparent form, that is not diamond. Diamond is very resistant to pressure, but at about 1 TPa (1000 GPa) transforms to a BC-8 form.

Carbides
Carbides are predicted to be more likely lower in the mantle as experiments have shown a much lower oxygen fugacity for high pressure iron silicates. Cohenite remains stable to over 187 GPa, but is predicted to have a denser orthorhombic Cmcm form in the inner core.

Carbon dioxide
Under 0.3 GPa pressure, carbon dioxide is stable at room temperature in the same form as dry ice. Over 0.5 GPa carbon dioxide forms a number of different solid forms containing molecules. At pressures over 40 GPa and high temperatures, carbon dioxide forms a covalent solid that contains CO4 tetrahedra, and has the same structure as β-cristobalite. This is called phase V or CO2-V. When CO2-V is subjected to high temperatures, or higher pressures, experiments show it breaks down to form diamond and oxygen. In the mantle the geotherm would mean that carbon dioxide would be a liquid till a pressure of 33 GPa, then it would adopt the solid CO2-V form till 43 GPa, and deeper than that would make diamond and fluid oxygen.

Carbonyls
High pressure carbon monoxide forms the high energy polycarbonyl covalent solid, however it is not expected to be present inside the Earth.

Hydrocarbons
Under 1.59 GPa pressure at 25 °C, methane converts to a cubic solid. The molecules are rotationally disordered. But over 5.25 GPa the molecules become locked into position and cannot spin. Other hydrocarbons under high pressure have hardly been studied.

Carbonates
Calcite changes to calcite-II and calcite-III at pressures of 1.5, and 2.2 GPa. Siderite undergoes a chemical change at 10 GPa at 1800K to form Fe4O5. Dolomite decomposes 7GPa and below 1000 °C to yield aragonite and magnesite. However, there are forms of iron containing dolomite stable at higher pressures and temperatures. Over 130 GPa aragonite undergoes a transformation to a SP3 tetrahedrally connected carbon, in a covalent network in a C2221 structure. Magnesite can survive 80 GPa, but with more than 100 GPa (as at a depth of 1800 km it changes to forms with three-member rings of CO4 tetrahedra (C3O96−). If iron is present in this mineral, at these pressures it will convert to magnetite and diamond. Melted carbonates with SP3 carbon are predicted to be very viscous.

Some minerals that contain both silicate and carbonate exist, spurrite and tilleyite. But high-pressure forms have not been studied. There have been attempts to make silicon carbonate. Six coordinated silicates mixed with carbonate should not exist on Earth, but may exist on more massive planets.

References

Extra reading

Geochemistry
Carbon


Even with many competitors within an industry, it is in the interest of all industry participants to have a core culture of functionality that is interoperable. With this philosophy in mind, The Business Case for Interoperability and Health Information Exchange sets the transformational stage for healthcare reform with a strong connection between health information exchange and interoperable exchange of patient health data.
The newer model of sustainability would be supported by a realignment of financial and policy incentives to support HIE, according to the white paper. This approach shifts away from the current system of provider incentives to purchase and implement EHRs and toward rewarding those vendors and stakeholders within the health marketplace who actively design for interoperability and demonstrably prove its value in practice.
"The imperative of health information exchange is now, but in the drive to move from EHRs to information exchange, several tasks still lay ahead.
"HIMSS envisions a world where we move from static data to a liquid interoperable future, but to advance interoperability toward this goal, there are still challenging tasks ahead. Many of these tasks will require consensus building within the healthcare industry and the development of new policies, laws and ideas that have not yet been conceived or imagined.
"This report serves as a primer on our country's growing national focus on health IT, prompted by President Bush's 2004 executive order declaring EMR availability by 2014. It provides a history from where we've come and identifies the challenges ahead for HIE, healthcare integration and interoperability," said HIE Community member Charlie Rogers, CEO, CoreHealth Technologies Inc.
"While it is too early to say, initial indicators see interoperability and health information exchange bringing value to healthcare in terms of outcomes, quality, patient engagement and other factors that indicate the investment is paying off," said Keith Salzman, MD, IBM, and member of HIMSS Clinical and Business Intelligence community.
"The connection between health information exchange and interoperability continues as a primary focus for HIMSS through the Interoperability Showcase™ - held around the world each year - as well as our tools and resources on health IT standards and interoperability. This new white paper extends our vision of better health through IT and demonstrates support for the Office of the National Coordinator's current 10-year vision of establishing interoperable health IT networks," says Joyce Sensmeier MS, RN-BC, CPHIMS, FHIMSS, FAAN, Vice President, Informatics, HIMSS North America.
• Download the white paper on the HIMSS' website.
• Watch a video on the HIMSS YouTube channel featuring John Loonsk, MD, FACMI, HIMSS Interoperability Maturity Model committee member, discussing the importance of adoption of interoperability and health IT.


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Environmental law at three Nordic universities
Joint Nordic Master Programme in Environmental Law
The Joint Nordic Master Programme in Environmental Law (NOMPEL) gives you a competitive degree in environmental law. The programme provides knowledge in environmental law at three levels: internationally, within the EU and in Nordic countries.
The goal is to provide first class learning for students who want to gain expertise in environmental law, nationally or internationally, as well as those who want to pursue a PhD in environmental law.
The Masters is the result of a cooperation between three leading Nordic universities: the University of Uppsala University (Uppsala, Sweden), the University of Eastern Finland (Joensuu, Finland) and the Arctic University of Norway (Tromsø, Norway). Students will spend a semester in each institution.
This combination of expertise will give you a unique international learning and living experience.
The programme will equip you with theoretical and methodological skills in environmental law. You will furthermore acquire specialistic knowledge and legal expertise on the management of natural resources, the protection of biodiversity, climate change and the energy transition.
Level of degree: Master's degree
Programme duration: 2 years / 120 ECTS credits
Language of instruction: English
Programme start: Autumn 2023
Tuition fee: EU/EEA nationals no tuition fee; non-EU/EEA nationals: Uppsala University: SEK 50 000/autumn semester 2023. UEF: EUR 2000/spring semester 2024 (incl. tuition fee waiver). UiT: no tuition fee.
Study campus: Uppsala (Sweden), Joensuu (Finland) and Tromsø (Norway)
The Master's degree programme is administrated by the Uppsala University. All the information concerning the admission process can be found on the NOMPEL webpage managed by Uppsala university.
This is a unique Master's programme in environmental law, featuring internationally renowned instructors who provide students with first hand insights into themes of great actuality and urgency. Throughout your studies, you will learn of best practices in the Nordic region, as well as of outstanding challenges to resolving global environmental problems.
Annalisa Savaresi
Associate Professor of International Environmental Law
Four semesters
NOMPEL is an advanced full-time study programme of 120 ECTS credits, with a nominal study length of two years.
First semester: Uppsala University (UU)
The first semester of the programme, comprising 30 ECTS, is spent in Uppsala. During this semester two themes are addressed. The first is a general introduction to the role of law in the formulation and implementation of environmental policies. This comprises the functions and potentials of different environmental legal instruments and principles, as well as how legislation and legal principles can counteract implementation of environmental objectives and green growth. Students will also learn how international and EU environmental law interact with national law, using Nordic countries as examples, as well as the basic structures and challenges of environmental law making and implementation.
The second theme of the first semester is more substantive and relates to the effective management of natural resources, including the protection of biodiversity. The objective is to analyse the relation between the management of natural resources (forest, water, wind etc.) and the interest of conserving biodiversity, as stipulated in international law, EU law and also the law of the Nordic states. This part of the first semester also constitutes the introduction to natural resource management and biodiversity protection, various subfields of which are subject to in depth discussions during subsequent semesters.
Second semester: University of Eastern Finland (UEF)
The second semester of the programme is spent at the School of Law of the University of Eastern Finland (UEF), Joensuu. The university is home to the Centre for Climate Change, Energy and Environmental Law (CCEEL), which brings together around 80 senior and junior scholars specialised in climate change, energy, natural resources and environmental law. At UEF, NOMPEL students take courses, for a total of 30 ECTS, comprising the following themes: climate change law and policy; international environmental law; green transitions; international forest law; international water law; environmental and social impact assessment. All NOMPEL courses at UEF are taught by international experts, providing unique insights into developments in international, European, and national environmental law. At UEF, NOMPEL students also have access to a host of extracurricular activities organised for all CCEEL Masters students.
Third semester: UiT the Arctic University of Norway (UiT)
The third semester is spent at UiT the Arctic University of Norway, Tromsø. At UiT you find one of the worlds' largest research centres for the law of the Sea (Norwegian Centre for the Law of the Sea, NCLOS), devoted to teaching and research on the law of the sea and marine environmental law. The studies at UiT add to and broadens the student's in-depth knowledge on marine resource management and biodiversity protection and energy and climate change Law. The courses in Tromsø are taught subsequently and gives a total of 30 ECTS.
The first course focuses on marine environmental law and sustainable use of living marine resources and includes studies on the protection of biodiversity in marine harvesting, in areas within and beyond national jurisdiction, and offers case studies on regional implementation.
The second course provides students with advanced knowledge of the interdependence between climate and energy, including the implications of climate change law for the energy sector, renewable energy, emissions trading and carbon capture and storage. The course will also offer case studies from the Arctic.
Fourth semester: The master's thesis
The fourth semester is administered by UiT, where the students must register, though students are not required to stay in Tromsø throughout the entire semester. Students will produce an individual master's thesis on a topic related to the subjects taught in the programme. The topic must be approved by UiT, which will also appoint an academic supervisor.
All students are required to attend a mandatory course training students in legal methodology, thesis structuring and writing skills. Each thesis is evaluated and graded by two examiners appointed by UiT. To be accepted to this fourth semester, students must have completed 75 credits of the programme courses.
Students who have successfully completed the programme will be awarded a joint degree (120 credits), named:
Master of Legal Science (Uppsala University)
Master of International and Comparative Law (University of Eastern Finland)
Master of Laws (UiT The Arctic University of Norway)
In Finland, the MICL degree does not qualify the graduate for positions in the judiciary or to practice law (e.g. as a judge or a lawyer). These positions require a Finnish Master of Laws degree (oikeustieteen maisteri, OTM).
Students holding a Finnish Bachelor of Laws (oikeusnotaari, ON) degree from a Finnish university can be awarded the degree Master of Laws (OTM).
The Programme degree requires the completion of all Programme courses (see below).
Language of the programme
The language of the programme is English. Students are required to complete all the courses in English.
Structure of studies
NOMPEL is in brief structured as follows:
First semester: Uppsala University
Introduction - The Role of Law in Environmental Policies (15 ECTS)
Law on Management of Natural Resources and Protection of Biodiversity (15 ECTS)
Second semester: University of Eastern Finland
Climate Change Law and Policy (5 ECTS)
International Economic Law and Green Transitions (5 ECTS)
International Environmental Law II (5 ECTS)
International Law and Forests (5 ECTS)
Environmental and Social Impact Assessment (5 ECTS)
International Water Law (5 ECTS)
Third semester: UiT The Arctic University of Norway
Energy and Climate Change Law (15 ECTS)
Protection of the Marine Environment with Focus on Marine Living Resources Law (15 ECTS)
Fourth semester: No obligation for students to stay in Uppsala, Tromsø or Joensuu
Master thesis in Environmental Law (30 ECTS)
Students will follow the regulations and procedures of the university at which they attend courses and sit for examinations, in a given semester. They will be provided with the same academic resources and support services that are available to all students at the university.
General instructions concerning studies at the UEF Law School can be found in Moodle (requires logging in with your UEF account) and Smart Start Guide.
Contact and General Enquiries
Lee Holmström
lawmaster@jur.uu.se
For admissions-related or general information, please contact the applicant support team: masterprogrammes@uu.se
University of Eastern Finland
Leader of the programme
Annalisa Savaresi, Associate Professor of International Environmental Law
email: annalisa.savaresi@uef.fi
Study coordinator
Moritz Petersmann
email: nompel@uef.fi
Course-specific information
In questions pertaining to a particular course, please contact the teacher of the course.
The Master's degree programme is administrated through the Uppsala University. All the important information related to the admission can be found at the website of the Uppsala university.
A Bachelor of Law corresponding to at least three years of full-time study (180 credits). Alternatively, a university degree of at least 180 credits, comprising or in combination with at least 90 credits in legal science.
Proficiency in English equivalent to the Swedish upper secondary course English 6. This requirement can be met either by achieving the required score on an internationally recognised test, or by previous upper secondary or university studies in some countries. Detailed instructions on how to provide evidence of your English proficiency are available at universityadmissions.se.
The Master's degree programme is administrated through the Uppsala University. All the important information related to the admission can be found at the website of the Uppsala university. NOTE that the application to the programme is submitted to Uppsala University only.
Student selection
Students are selected based on:
an overall appraisal of previous university studies; and
a statement of purpose including information on previous education, work and other experience.
Students are admitted to the NOMPEL programme at Uppsala University. The students are also registered at the University of Eastern Finland and UiT The Arctic University of Norway in order to gain study rights as a degree student and to gain access to student services.
Tuition fees and waivers
If you are not a citizen of a European Union (EU) or European Economic Area (EEA) member state or Switzerland, you are required to pay fees, as follows:
To apply for the programme, there is an application fee of SEK 900.
Tuition fee for the first semester at Uppsala University is currently SEK 50 000.
University of Eastern Finland (UEF)
The tuition fee to study one semester at UEF is EUR 2000. This figure includes the 50% tuition fee waivers UEF has granted to all fee-paying NOMPEL students for academic year 2022-2023.
The tuition fee covers the UEF courses included in the NOMPEL degree and all study-related supporting services at UEF.
In addition, at UEF students must pay a healthcare fee (EUR 35.80) and the membership fee to join the Student Union (EUR 36).
At UiT The Arctic University of Norway, there are no tuition fees. Students only need to pay a semester fee, currently NOK 625.
Essential information for a new student can be found in the Kamu student handbook.
Smart Start Guide
Programme specific materials for new students are compiled in Smart Starts.
Learn more about life in Finland and our campus cities.
Latest news and greetings from our study programme.
Lee Holmström, lawmaster@jur.uu.se
Moritz Petersmann, nompel@uef.fi
Lene Emilie Øye, lene.e.oye@uit.no


Address: Sammy Marks Sq, Vermeulen St, Gauteng Central, Gauteng, 0002, South Africa, Pretoria. See full address and map.
Address: 534 Rembrandt Ave, Faerie Glen, Gauteng, 0081, South Africa, Pretoria. See full address and map.
Address: Prinsloo St, Gauteng Central, Gauteng, 0002, South Africa, Pretoria. See full address and map.
Address: 518 Jacqueline Dve, Garsfontein, Gauteng, 0081, South Africa, Pretoria. See full address and map.
Address: 681 Honoria St, Garsfontein, Gauteng, 0081, South Africa, Pretoria. See full address and map.
Address: 1 Bank Forum Bldg, Fehrsen St, New Muckleneuk, Gauteng, 0181, South Africa, Pretoria. See full address and map.
Address: 26 Rose St, Heatherdale A H, Gauteng, 0002, South Africa, Pretoria. See full address and map.
Address: 3 Gr Van Erkom Arc, 222 Schoeman St, Gauteng Central, Gauteng, 0002, South Africa, Pretoria. See full address and map.
Address: 107 Haymeadow Cres, Faerie Glen, Gauteng, 0081, South Africa, Pretoria. See full address and map.
Address: 95 Hadeda St, Montanapark Exts, Gauteng, 0159, South Africa, Pretoria. See full address and map.
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Address: 50 Veronica Rd, Montana A H, Gauteng, South Africa, Pretoria. See full address and map.
Address: 4 Flaming Rock Cres, Mooikloof, Gauteng, 0018, South Africa, Pretoria. See full address and map.
Address: 371 Farenden St, Arcadia, Gauteng, 0083, South Africa, Pretoria. See full address and map.
Address: 741 Sout St, Wingate Park, Gauteng, 0153, South Africa, Pretoria. See full address and map.


text:
Home > Business > Anti-Corruption Day
Anti-Corruption Day
by Martin Banks 2 years ago Dec 09, 2020 0 Comments
On International Anti-Corruption Day (9 December), 101 leading transparency, anti-corruption and open data organisations along with investigative journalists from across Europe have called on the European Commission and national governments to act to ensure that company registers, including ownership and corporate structure data, are freely accessible and published in open data format.
In an open letter sent today to Thierry Breton, Internal Market Commissioner, and Vera Jourová, Vice President for Values and Transparency, the organisations respond to threats to reduce access to company registers to only very basic data, without the names of owners, when the EU agrees on the details of implementation of the 2019 Open Data Directive. The letter states that the commitment to open company registers, including ownership and corporate structure data, is the most critical transparency and anti-corruption measure that the EU will adopt in 2020.
"More than $11 trillion has already been spent by governments all over the world urgently responding to the COVID-19 pandemic, and reliable information on who controls anonymous companies is central for identifying where this money goes and for preventing financial mismanagement, fraud and corruption," said Laure Brillaud, Senior Policy Officer, Transparency International EU.
Addressing the importance of the open company data for investigative journalists, Drew Sullivan, Editor and Publisher of the Organized Crime and Corruption Reporting Project said: "The EUs plan to water down the Open Data Directive is a gift to organized crime and corrupt actors. Half-hearted transparency leaves loopholes which invite dark money into your system, undermining democracy, and ultimately promotes plutocracy. As a European directive, you need a rock hard standard that can serve as a bedrock for democracy."
"High-quality and readily-accessible company ownership information is essential to carry out proper due diligence on potential fraudulent or false companies, and therefore is essential for both governments and other businesses operating in the European space," said Robin Hodess, Director of Governance & Transparency at The B Team.
Emily Wigens, EU Director of The ONE Campaign, added: "Developing countries lose more than $1 trillion each year as a result of secrecy and shady deals. The public, including journalists and civil society organizations, plays a critical role in exposing corruption and bad deals, so must have full access to open company ownership data for the EU's company registers to be effective."
"We see that most big cases of fraud, corruption and tax evasion are uncovered by journalists and civil society. Unrestricted access to these data is essential for these organizations to play their part" stated Serv Wiemers, Director Open State Foundation.
Partial progress has already been made towards this goal, according to Jesse Renema Senior Project Lead of the Open State foundation: "We are halfway there as the European Union's 5th Anti Money Laundering Directive (AMLD5), already requires open registers of beneficial owners of companies. To complete the anti-corruption package, it is essential to commit to fully open company registers."
Addressing privacy concerns, Helen Darbishire, Executive Director of Access Info Europe explained: "When legislators determine – as they have done with the Open Data Directive – that certain data needs to be made public, including the names of company owners, to combat corruption, this has a legal basis and is proportionate and entirely consistent with data protection rules. There cannot be backtracking now because of lobbying by businesses not ready to be open."
Addressing the concern that opening up company data will have an associated cost for national company registers, Thom Townsend, Executive Director, Open Ownership, stated: "It is evident that the cost of publishing this essential information is minimal compared to the significant economic savings and invaluable societal benefits that accrue from avoiding fraud and corruption."
Chris Taggart, of the business Open Corporates, added: "This data is essential for entrepreneurs across Europe, such as the business that I run. If the EU is serious about supporting open data for entrepreneurship, they should start with pivotal data sets such as company registers. In a financial crisis and risks of increasing unemployment, the way ahead is to act on the EU's digital strategy promises and keep this data open."
Tagged #Breton #Brillaud #Hodess #Jourová #Renema #Sullivan #Taggart #Townsend #Wigens
NGOs Unite in call for China Russia and Iran to Release Religious Prisoners
Stop Arming Turkey
Greens Call for Windfall Profits Tax on Oil Companies
Parliament Takes Commission to Court for Inaction on Rule of Law
Importance of a Diversified Banking System for Europe


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2001 PG-13 1h 37m DVD
Jane has it made: She's the talent booker for a popular talk show and has started dating the show's studly producer. But when she gets summarily dumped, the now-bitter Jane is prompted write a tell-all advice column about why men do what they do.
Ashley Judd, Greg Kinnear, Hugh Jackman, Marisa Tomei, Ellen Barkin, Catherine Dent, Peter Friedman, Laura Regan, Donna Hanover, Matthew Coyle, Colleen Camp
Comedy, Romantic Comedies
English, Spanish (Neutral)
English: Dolby Digital 5.1, English: Dolby Digital 2.0 Surround, French: Dolby Digital 2.0 Surround
PG-13 - Some material may be inappropriate for children under 13. Parents are urged to be cautious. Some material may be inappropriate for pre-teenagers.
Parents need to know that the movie features sexual references and situations and some very strong language for a PG-13. Characters drink and smoke, and there are scenes in a bar. Drinking is shown as a solace for pain. Boxes of condoms and a diaphragm that has not been used for a while are shown for comic effect.
Sexual references and situations, including birth control humor.
Some emotional tension.
Strong language for PG-13.
Characters drink and smoke, including use of alcohol to numb feelings.


Najnovším letným/jesenným trendom je hybrid vesty a saka. Podobá sa na vestu, ale strihom a dĺžkou je to viac sako alebo kabát, len bez rukávov. Môžete ich nájsť v rôznych podobách, ako hrubší a častejší variant z kože alebo z látky či ľahká vesta z jemného materiálu na leto. Takisto možností na ich nosenie je veľmi veľa. Napríklad na šaty alebo sukňu prepásané opaskom či jednoduchší look so slim nohavicami. Je to len na vás.
The newest summer/autumn trend is a hybrid of vest and jacket. It looks like a vest, but with a cut and lenght, it´s more like a jacket or blazer without sleeves. You can find it in different variants, like thick and more common choice made from leather or fabric, or a light-weighted vest from light material for summer. There are also many possibilities how to wear it. For example, on dress or skirt belted with a belt or more simple look with slim pants. It´s all up to you.
Love this! I have so many vests like this so I'm super stoked it is in fashion!!
Lovely compilation of high fashion pictures !
Fantastic post! Love leather vests. Have a great day.
I love this trend.... amazing selection Lia!!!!
Love these retro long vest back on trend once again:). I remembers back in the day when my Mom and Aunts were wearing these trendy when I was a child:) and I, myself have some in my closet, hopefully :). I can wear sometimes soon:). Thanks so much for the update trendy sweetie:).
Wishing you a peaceful night over your place:).
Sending you a kiss darling! (PS. I'm the once who late today).
Yes I've been seeing a lot of these vest type jackets and they look so cute! I like them belted the most!
I love the casualness yet the elegance these long vests bring! thanks for sharing!
Great selection! I really love Rachel Zoe's version.
Love that trend! I need one right now!
You're totally inspiring me to get a long vest with all these great looks!
Sending you more kisses and hugs sunshine:). Wish your day is going smooth:).
Tnx for your lovely comment!!!
Dear Lia, I have to admit that you inspired me with this trend so much that now I must immediately find such a vest :) Thanks a lot for the wonderful inspiration, I think such a vest is really versatile and can be combined with so many outfits that the buy is for sure worth!
Good morning honey. Great selection Lia. I already have quite a lot of those vest/cardigans in my closet, so fall can come.
Very chic trend dear! Love this.
Amazing post! Love the sleeveless blazers- fabric ones!
O yes yes! Totally digging these looks. I have been eyeing a few myself.
So jackets are getting longer again, as in the '80s... Welcome back!
Super!!! moc se mi líbí ta bílá na první fotce!
Tento trend mě docela začíná bavit :-).
Looks like a pretty great trend to get into.
a lot of ways to wear this cloth!
Have a lovely night sweetie! Sending you kisses and love:). (Just got home).
Che bella selezione di outfit, mi piace un sacco.
Anche la scelta delle foto è unica e bellissima.
I love long coats too! Arent these fab!
I've really been loving these long vests, they are so chic. I need to get one!
Great picks, the vest is such a great look!
I love this trend... I think the one from topshop is perfect!
Love them and love your selection!
Wow! Thanks for posting these great inspirations. I actually own a long vest but never wore it because I didn't know how. Now I'm inspired!


text: Source: Photo: Lieblingsfilm / Fabian Rösler I am delighted to announce today that I have completed an agreement with Lieblingsfilm Film Production company in Munich to supply my full size FA CUP Replica Trophy to them for their upcoming movie 'Trautmann'. The film is a biopic of legendary German goalkeeper Bert Trautmann, the former Nazi paratrooper who became a goalkeeping legend at Manchester City, making 545 appearances and famously playing in the FA Cup final with a


text:
Friesland Bank was a Dutch retail bank originally focusing on the northern provinces of the Netherlands, Friesland, Groningen, Drenthe, Overijssel, and North Holland. On 2 April 2012 Friesland Bank announced that it would become a 100% daughter of Rabobank Nederland after a merger plan with NIBC was blocked by De Nederlandse Bank.

History
Founded in 1913 as  the Coöperatieve Zuivelbank (Co-operative Dairy bank), it affiliated with "Raiffeisenbank". However, as  Raiffeisenbank merged with the Boerenleenbank to form Rabobank, the Coöperatieve Zuivelbank was once again fully independent. In 1970, the company changed its name to Friesland Bank. Originally operating only in Friesland itself, Friesland Bank started opening branches in the northern Netherlands in the 1990s.

In 2011, the bank was in dire straits, suffering a loss of € 350 million, partly as a result of an extra write-down on the interest in Van Lanschot and loan losses. Van Lanschot's planned sales plans were not realised. The solvency ratios fell below the established standards. The BIS ratio fell to 6.1%, which is far below the standard of 8% and the Tier1 ratio more than halved to 4.2%.

References

External links

Friesland Bank website

Banks of the Netherlands
Banks established in 1913
Companies based in Friesland
Leeuwarden
Dutch companies established in 1913


Midland Health is one of the nation's leading providers of on site wellness screenings, health coaching and flu shot programs.
Midland Health is a woman-owned business and is proud to be certified by the WBENC and Department of Transportation DBE. View our certification details.


HstWB Installer is a set of powershell scripts, image templates, configuration files, AmigaDOS scripts and binaries used to easily build Amiga HDF or directory images with automated installation of Workbench, Kickstarts roms and packages with additional content for Classic Amiga. It's currently being developed and maintained by Henrik Nørfjand Stengaard. Setting up a blank Amiga HDF image with e.g. PFS3, Workbench, Kickstarts roms, WHDLoad games and demos installed properly can be a cumbersome task unless you spend a lot of time figuring out how this is done step by step. This is where HstWB Installer come to aid and can help to automate such installations using WinUAE and should be possible for almost anyone to do with very little knowledge about Amiga. The packages included are BetterWB, HstWB, EAB WHDLoad games and demos menus for both AGA and OCS. Menu packages has screenshots and details for EAB games and demos WHDLoad packs configured for Arcade Game Selector 2 and iGame. These packages can be added to an image configuration and will be installed during HstWB Installer installation process. In general HstWB Installer is build as a minimalistic as possible using BetterWB and HstWB to support A500 as a minimum. HstWB is mainly targeted A500, A600, A1200. The minimalistic approach allows users to customize it further with their own preferences like installing eg. MagicWB or Scalos.


The 2018 Paint Branch Marching Panthers kicked off their competition season by hosting their first competition in the Paint Branch Stadium on October 13th.
The event, which included 19 other bands from all over the DMV, New York, and New Jersey, was an exciting event that included some very talented performers. The Paint Branch Marching Band, as is customary, was the final band to participate in the competition. Each band performed their selected show; ranging from 10-12 minutes and the adjudicated based on music, visual, and overall effect. The bands were divided into 5 groups, IA, IIA, IIIA, IVA, and Open class.
Additionally, as hosts, their performance was an exhibition, which meant that they could not place in the event. However, they were still critiqued by the judges and received a score of 78.575 that would have put them at second place in their division.
One of the biggest pluses for such an event is that it not only brings awareness to the marching band program at PB and other music programs in Montgomery County, but allows the community to see the amount of effort and dedication it takes to put on a ten minute show. These complex shows transform a football field into something more than a place where a traditional American sport is played.
Components of music, drill, and choreography come together in harmony to help a story come to life.