WrLd Fed Saiz Ohmz Vrs (Haoh=#)1: WorLd Fed Sizomes In Simp Lang Yeeng Voiss Sownd Chahrz

WrLd Fed Vrs (Haoh=#)1: World FederaTion In Simp Lang Yeeng Voiss Sownd Chahrz

Earth in Funetik Inglish iz Rth uv Gaia Earth Science Sizomes

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Structure of the Atmosphere

Earth's atmosphere Lower 4 layers of the atmosphere in 3 dimensions as seen diagonally from above the exobase. Layers drawn to scale, objects within the layers are not to scale. Aurorae shown here at the bottom of the thermosphere can actually form at any altitude in this atmospheric layer.

Principal layers

In general, air pressure and density decrease with altitude in the atmosphere. However, temperature has a more complicated profile with altitude, and may remain relatively constant or even increase with altitude in some regions (see the temperature section, below). Because the general pattern of the temperature/altitude profile is constant and measurable by means of instrumented balloon soundings, the temperature behavior provides a useful metric to distinguish atmospheric layers. In this way, Earth's atmosphere can be divided (called atmospheric stratification) into five main layers. Excluding the exosphere, the atmosphere has four primary layers, which are the troposphere, stratosphere, mesosphere, and thermosphere.[10] From highest to lowest, the five main layers are:

Exosphere: 700 to 10,000 km (440 to 6,200 miles)
Thermosphere: 80 to 700 km (50 to 440 miles)[11]
Mesosphere: 50 to 80 km (31 to 50 miles)
Stratosphere: 12 to 50 km (7 to 31 miles)
Troposphere: 0 to 12 km (0 to 7 miles)[12]
Exosphere
Main article: Exosphere
The exosphere is the outermost layer of Earth's atmosphere (i.e. the upper limit of the atmosphere). It extends from the exobase, which is located at the top of the thermosphere at an altitude of about 700 km above sea level, to about 10,000 km (6,200 mi; 33,000,000 ft) where it merges into the solar wind.

This layer is mainly composed of extremely low densities of hydrogen, helium and several heavier molecules including nitrogen, oxygen and carbon dioxide closer to the exobase. The atoms and molecules are so far apart that they can travel hundreds of kilometers without colliding with one another. Thus, the exosphere no longer behaves like a gas, and the particles constantly escape into space. These free-moving particles follow ballistic trajectories and may migrate in and out of the magnetosphere or the solar wind.

The exosphere is located too far above Earth for any meteorological phenomena to be possible. However, the aurora borealis and aurora australis sometimes occur in the lower part of the exosphere, where they overlap into the thermosphere. The exosphere contains most of the satellites orbiting Earth.

Thermosphere
Main article: Thermosphere
The thermosphere is the second-highest layer of Earth's atmosphere. It extends from the mesopause (which separates it from the mesosphere) at an altitude of about 80 km (50 mi; 260,000 ft) up to the thermopause at an altitude range of 500–1000 km (310–620 mi; 1,600,000–3,300,000 ft). The height of the thermopause varies considerably due to changes in solar activity.[11] Because the thermopause lies at the lower boundary of the exosphere, it is also referred to as the exobase. The lower part of the thermosphere, from 80 to 550 kilometres (50 to 342 mi) above Earth's surface, contains the ionosphere.

The temperature of the thermosphere gradually increases with height. Unlike the stratosphere beneath it, wherein a temperature inversion is due to the absorption of radiation by ozone, the inversion in the thermosphere occurs due to the extremely low density of its molecules. The temperature of this layer can rise as high as 1500 °C (2700 °F), though the gas molecules are so far apart that its temperature in the usual sense is not very meaningful. The air is so rarefied that an individual molecule (of oxygen, for example) travels an average of 1 kilometre (0.62 mi; 3300 ft) between collisions with other molecules.[13] Although the thermosphere has a high proportion of molecules with high energy, it would not feel hot to a human in direct contact, because its density is too low to conduct a significant amount of energy to or from the skin.

This layer is completely cloudless and free of water vapor. However, non-hydrometeorological phenomena such as the aurora borealis and aurora australis are occasionally seen in the thermosphere. The International Space Station orbits in this layer, between 350 and 420 km (220 and 260 mi).

Mesosphere
Main article: Mesosphere
The mesosphere is the third highest layer of Earth's atmosphere, occupying the region above the stratosphere and below the thermosphere. It extends from the stratopause at an altitude of about 50 km (31 mi; 160,000 ft) to the mesopause at 80–85 km (50–53 mi; 260,000–280,000 ft) above sea level.

Temperatures drop with increasing altitude to the mesopause that marks the top of this middle layer of the atmosphere. It is the coldest place on Earth and has an average temperature around −85 °C (−120 °F; 190 K).[14][15]

Just below the mesopause, the air is so cold that even the very scarce water vapor at this altitude can be sublimated into polar-mesospheric noctilucent clouds. These are the highest clouds in the atmosphere and may be visible to the naked eye if sunlight reflects off them about an hour or two after sunset or a similar length of time before sunrise. They are most readily visible when the Sun is around 4 to 16 degrees below the horizon. Lightning-induced discharges known as transient luminous events (TLEs) occasionally form in the mesosphere above tropospheric thunderclouds. The mesosphere is also the layer where most meteors burn up upon atmospheric entrance. It is too high above Earth to be accessible to jet-powered aircraft and balloons, and too low to permit orbital spacecraft. The mesosphere is mainly accessed by sounding rockets and rocket-powered aircraft.

Stratosphere
Main article: Stratosphere
The stratosphere is the second-lowest layer of Earth's atmosphere. It lies above the troposphere and is separated from it by the tropopause. This layer extends from the top of the troposphere at roughly 12 km (7.5 mi; 39,000 ft) above Earth's surface to the stratopause at an altitude of about 50 to 55 km (31 to 34 mi; 164,000 to 180,000 ft).

The atmospheric pressure at the top of the stratosphere is roughly 1/1000 the pressure at sea level. It contains the ozone layer, which is the part of Earth's atmosphere that contains relatively high concentrations of that gas. The stratosphere defines a layer in which temperatures rise with increasing altitude. This rise in temperature is caused by the absorption of ultraviolet radiation (UV) radiation from the Sun by the ozone layer, which restricts turbulence and mixing. Although the temperature may be −60 °C (−76 °F; 210 K) at the tropopause, the top of the stratosphere is much warmer, and may be near 0 °C.[16]

The stratospheric temperature profile creates very stable atmospheric conditions, so the stratosphere lacks the weather-producing air turbulence that is so prevalent in the troposphere. Consequently, the stratosphere is almost completely free of clouds and other forms of weather. However, polar stratospheric or nacreous clouds are occasionally seen in the lower part of this layer of the atmosphere where the air is coldest. The stratosphere is the highest layer that can be accessed by jet-powered aircraft.

Troposphere
Main article: Troposphere
The troposphere is the lowest layer of Earth's atmosphere. It extends from Earth's surface to an average height of about 12 km, although this altitude actually varies from about 9 km (30,000 ft) at the poles to 17 km (56,000 ft) at the equator,[12] with some variation due to weather. The troposphere is bounded above by the tropopause, a boundary marked in most places by a temperature inversion (i.e. a layer of relatively warm air above a colder one), and in others by a zone which is isothermal with height.[17][18]

Although variations do occur, the temperature usually declines with increasing altitude in the troposphere because the troposphere is mostly heated through energy transfer from the surface. Thus, the lowest part of the troposphere (i.e. Earth's surface) is typically the warmest section of the troposphere. This promotes vertical mixing (hence the origin of its name in the Greek word τρόπος, tropos, meaning "turn"). The troposphere contains roughly 80% of the mass of Earth's atmosphere.[19] The troposphere is denser than all its overlying atmospheric layers because a larger atmospheric weight sits on top of the troposphere and causes it to be most severely compressed. Fifty percent of the total mass of the atmosphere is located in the lower 5.6 km (18,000 ft) of the troposphere.

Nearly all atmospheric water vapor or moisture is found in the troposphere, so it is the layer where most of Earth's weather takes place. It has basically all the weather-associated cloud genus types generated by active wind circulation, although very tall cumulonimbus thunder clouds can penetrate the tropopause from below and rise into the lower part of the stratosphere. Most conventional aviation activity takes place in the troposphere, and it is the only layer that can be accessed by propeller-driven aircraft.

Space Shuttle Endeavour orbiting in the thermosphere. Because of the angle of the photo, it appears to straddle the stratosphere and mesosphere that actually lie more than 250 km below. The orange layer is the troposphere, which gives way to the whitish stratosphere and then the blue mesosphere.

Other layers

Within the five principal layers that are largely determined by temperature, several secondary layers may be distinguished by other properties:

The ozone layer is contained within the stratosphere. In this layer ozone concentrations are about 2 to 8 parts per million, which is much higher than in the lower atmosphere but still very small compared to the main components of the atmosphere. It is mainly located in the lower portion of the stratosphere from about 15–35 km (9.3–21.7 mi; 49,000–115,000 ft), though the thickness varies seasonally and geographically. About 90% of the ozone in Earth's atmosphere is contained in the stratosphere.
The ionosphere is a region of the atmosphere that is ionized by solar radiation. It is responsible for auroras. During daytime hours, it stretches from 50 to 1,000 km (31 to 621 mi; 160,000 to 3,280,000 ft) and includes the mesosphere, thermosphere, and parts of the exosphere. However, ionization in the mesosphere largely ceases during the night, so auroras are normally seen only in the thermosphere and lower exosphere. The ionosphere forms the inner edge of the magnetosphere. It has practical importance because it influences, for example, radio propagation on Earth.
The homosphere and heterosphere are defined by whether the atmospheric gases are well mixed. The surface-based homosphere includes the troposphere, stratosphere, mesosphere, and the lowest part of the thermosphere, where the chemical composition of the atmosphere does not depend on molecular weight because the gases are mixed by turbulence.[21] This relatively homogeneous layer ends at the turbopause found at about 100 km (62 mi; 330,000 ft), the very edge of space itself as accepted by the FAI, which places it about 20 km (12 mi; 66,000 ft) above the mesopause.
Above this altitude lies the heterosphere, which includes the exosphere and most of the thermosphere. Here, the chemical composition varies with altitude. This is because the distance that particles can move without colliding with one another is large compared with the size of motions that cause mixing. This allows the gases to stratify by molecular weight, with the heavier ones, such as oxygen and nitrogen, present only near the bottom of the heterosphere. The upper part of the heterosphere is composed almost completely of hydrogen, the lightest element.
The planetary boundary layer is the part of the troposphere that is closest to Earth's surface and is directly affected by it, mainly through turbulent diffusion. During the day the planetary boundary layer usually is well-mixed, whereas at night it becomes stably stratified with weak or intermittent mixing. The depth of the planetary boundary layer ranges from as little as about 100 metres (330 ft) on clear, calm nights to 3,000 m (9,800 ft) or more during the afternoon in dry regions.

See also:

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Simp Lang World Law In FuhnehTik IngLish Yeeng Voiss Sownd Chahrz

See also: https://en.wikipedia.org/wiki/Category:International_law

WorLd Fed Law Sizomes In Yeeng Voiss Sownd Chahrz
Iz Wrld Fed Lah Saiz Ohmz Uv Lah Saiz Ohmz
Uv Thuh AhL Spundj STeiT Saiz Ohmz Uv Thuh AhL STeiT Saiz Ohmz Peidj LisT.

WP%20header%20med.jpg

Provisional WorLd Fed Laws In Simp Lang Yeeng Voiss Sownd Chahrz

Earth Constitution Article 19 - Provisional World Government

Sec. A - Actions to be Taken by the World Constituent Assembly

Upon adoption of the World Constitution by the World Constituent Assembly, the Assembly and such continuing agency or agencies as it shall designate shall do the following, without being limited thereto:

Issue a Call to all Nations, communities and people of Earth to ratify this World Constitution for World Government.

Establish the following preparatory commissions:
Ratification Commission.
World Elections Commission.
World Development Commission.
World Disarmament Commission.
World Problems Commission.
Nominating Commission.
Finance Commission.
Peace Research and Education Commission.
Special commissions on each of several of the most urgent world problems.
Such other commissions as may be deemed desirable in order to proceed with the Provisional World Government.

Convene Sessions of a Provisional World Parliament when feasible under the following conditions:
Seek the commitment of 500 or more delegates to attend, representing people in 20 countries from five continents, and having credentials defined by Article 19, Section C (Provisional World Parliament);
The minimum funds necessary to organize the sessions of the Provisional World Parliament are either on hand or firmly pledged.
Suitable locations are confirmed at least nine months in advance, unless emergency conditions justify shorter advance notice.

Earth Constitution

Image4.gif

The Provisional World Parliament shall be composed of the following members:

All those who were accredited as delegates to the 1977 and 1991 Sessions of the World Constituent Assembly, as well as to any previous Session of the Provisional World Parliament, and who re-confirm their support for the Constitution for the Federation of Earth], as amended.

Persons who obtain the required number of signatures on election petitions, or who are designated by Non-Governmental Organizations which adopt approved resolutions for this purpose, or who are otherwise accredited according to terms specified in Calls which may be issued to convene particular sessions of the Provisional World Parliament.

Members of the World Parliament to the House of Peoples who are elected from World Electoral and Administrative Districts up to the time of convening the Provisional World Parliament. Members of the World Parliament elected to the House of Peoples may continue to be added to the Provisional World Parliament until the first operative stage of World Government is reached.

Members of the World Parliament to the House of Nations who are elected by national legislatures or appointed by national governments up to the time of convening the [Provisional World Parliament. Members of the World Parliament to the House of Nations may continue to be added to the Provisional World Parliament until the first operative stage of World Government is reached.

Those universities and colleges which have ratified the World Constitution may nominate persons to serve as Members of the World Parliament to the House of Counsellors. The House of Peoples and House of Nations together may then elect from such nominees up to fifty Members of the World Parliament to serve in the House of Counsellors of the Provisional World Government.
Members of the Provisional World Parliament in categories (a) and (b) as defined above, shall serve only until the first operative stage of World Government is declared, but may be duly elected to continue as Members of the World Parliament during the first operative stage.

WORLD LEGISLATIVE ACTS Uv In Fohrss Proh WrLd Fed Lahz Uv WrLd Fed Lah Saiz Ohmz

WORLD LEGISLATIVE ACTS Hohm Peydj

World Legislative Act #1 World Disarmament Agency

See related material:

Summary WLA #1 WMD Prohibition Act
WLA#13 - World Peace Act
WLA#33 - Fissile Materials Production Ban
WLA#34 - Elimination Protocol Protocol
Enforcement System Diagram
ICJ Advisory Opinion (1996)
World Legislative Act #2 World Economic Development Organization

Summary WLA #2 Economic Development
Hour money website
World Legislative Act #3 Ownership, Administration and Development of the Oceans and Seabeds of Earth

Summary WLA #3 Oceans and Seabeds
Referred and disapproved Law of the Sea Convention, subject to further review by Provisional World Parliament
World Legislative Act #4 Graduate School of World Problems

Summary WLA #4 World University System
World Legislative Act #5 World Courts

Summary WLA #5 District World Courts
World Legislative Act #6 Emergency Earth Rescue Administration

Summary WLA #6 Earth Rescue
World Legislative Act #7 World Government Funding Corporation

Summary WLA #7 Funding Corporation
Hour money website
Funding Corporation Diagram
CONVENTION ON THE LAW APPLICABLE TO CERTAIN RIGHTS IN RESPECT OF SECURITIES HELD WITH AN INTERMEDIARY (This links to the 2006 Hague Convention full text. The convention serves as a guideline, but as a convention does not and cannot supercede the principles and terms of the overall world law with respect to illegal securites.)
World Legislative Act #8 World Commission on Terrorism

Summary WLA #8 Terrorism Commission
World Legislative Act #9 Global Ministry of Environment

Summary WLA #9 Environment Ministry
Referred International Conventions Basel - Biodiversity - Climate Change - International Trade in Endangered Species - London Dumping - Migratory Species - Montreal Protocol - Ramsar Wetlands - World Conservation Union
World Legislative Act #10 World Hydrogen Energy System Authority

Summary WLA #10 Hydrogen System
Low Energy Nuclear Reaction
Cold Fusion
World Legislative Act #11 Earth Financial Credit Corporation

Summary WLA #11 Credit Corporation
Hour money website
World Legislative Act #12 Manifesto 1996 & 2000

Summary WLA #12 Manifesto 1996 & 2000
World Legislative Act #13 World Peace Act

Summary WLA #13 World Peace Act
World Legislative Act #14 World Security Act

Summary WLA #14 World Security Act
Enforcement System Diagram
World Legislative Act #15 Human Rights Court

Summary WLA #15 Human Rights Court
Office of the High Commissioner for Human Rights
World Judicial Commission
Statute of the World Court of Human Rights 1974
World Service Authority
World Legislative Act #16 Hydrocarbon Resources

Summary WLA #16 Hydrocarbon Resources
World Legislative Act #17 Commission for Legislative Review

Arizona Legislative Council Bill Drafting Manual
Oregon Form and Style Manual for Legislative Measures
World Legislative Act #18 World Revenue and Rules of Procedure for World Constituent Assembly

Summary WLA #18 World Revenue
Funding Corporation Diagram
Hour money website
Rules of Procedure for World Constituent Assembly (as provisional parliamentary deliberation & adoption was directed by the 4th Session of World Constituent Assembly, Troia, Portugal, 1991. Article 18.5 of Earth Constitution.)
World Legislative Act #19 World Criminal Code Penalty Classification (World Penal Code)

Summary WLA #19 World Penal Code
The Assembly of States Parties Version Elements of Crimes
World Legislative Act #20 World Criminal Case Bench

Summary WLA #20 Criminal Case Court
World Legislative Act #21 Department of World Patents and Intellectual Property Rights

Summary WLA #21 World Patents
World Legislative Act #22 World Equity Act

Summary WLA #22 Economic Equity Act
Hour money website
World Legislative Act #23 Global Accounting & Auditing System

Summary WLA #23 Account Standards Act
World Legislative Act #24 Procedure & Evidence for the World Bench on Criminal Cases

Summary WLA #24 Procedure and Evidence
Assembly of States Parties Version
World Legislative Act #25 Records Preservation

Summary WLA #25 Records Act
World Legislative Act #26 Education Act

Summary WLA #26 Education Act
World Legislative Act #27 Child Rights

Summary WLA #27 Child Rights
World Legislative Act #28 World Bench on Juvenile Cases

Summary WLA #28 World Juvenile Court
Hague Conventions on International Protection of Children, Family and Property Relations
World Legislative Act #29 World Elections Act

Summary WLA #29 Elections Act
World Legislative Act #30 Water Act

Summary WLA #30 Water Act
World Legislative Act #31 World Ombudsmus Act

Summary WLA #31 Ombudsmus Act
Office of the High Commissioner for Human Rights
World Legislative Act #32 Conflict Resolution

Summary WLA #32 Conflict Resolution
World Legislative Act #33 Fissile Production Ban

Summary WLA #33 Fissile Materials Ban
Enforcement System Diagram
World Legislative Act #34 Nuclear Weapons Dismantling Procedure

Summary WLA #34
World Legislative Act #35 Nuclear Contamination Act

Summary WLA #35 Nuclear Contamination
(Reference annulled letter)
World Legislative Act #36 Quit Guantanamo Directive

Summary WLA #36 Guantanamo Bay Directive
Guantanamo Bay City Map
Guantanamo Province Map
World Legislative Act #37 Agreement on World Federal Privilege of Immunities

Summary WLA #37 Privileges and Immunities
Assembly of States Parties Version
List of States Parties to the ASP version
World Legislative Act #38 Public Utilities

Summary WLA #38 Public Utilities
World Legislative Act #39 Prohibition of Unauthorized Destruction of Illegal Financial Instruments

Summary WLA #39 Stock Record Destruction Ban
CONVENTION ON THE LAW APPLICABLE TO CERTAIN RIGHTS IN RESPECT OF SECURITIES HELD WITH AN INTERMEDIARY (This links to the 2006 Hague Convention full text. The convention serves as a guideline, but as a convention does not and cannot supercede the principles and terms of the overall world law with respect to illegal securites.)
World Legislative Act #40 Indemnity Bonds

Summary WLA #40 Indemnity Bonds
Hour money website
CONVENTION ON THE LAW APPLICABLE TO CERTAIN RIGHTS IN RESPECT OF SECURITIES HELD WITH AN INTERMEDIARY (This links to the 2006 Hague Convention full text. The convention serves as a guideline, but as a convention does not and cannot supercede the principles and terms of the overall world law with respect to illegal securites.)
World Legislative Act #41 Posting the Stock Law

Summary WLA #41 Posting the Stock Law
World Legislative Act #42 Universal Guaranteed Annual Income

Summary WLA #42 Guaranteed Annual Income
World Legislative Act #43 On Human Trafficking

Summary WLA #43 On Human Trafficking
World Legislative Act #44 Non-Violent Civil Disobedience Act

Summary WLA #44 Non-Violent Civil Disobedience Act
World Legislative Act #45 Bureaucratic Efficiency Act

Summary WLA #45 Bureaucratic Efficiency Act
World Legislative Act #46 Clandestine Operations Prohibition Act

Summary WLA #46 Clandestine Operations Prohibition Act
World Legislative Act #47 International Integration Act

Summary WLA #47 International Integration
12th Session of Provisional World Parliament convened December 2010 as scheduled at the Rabindranath Tagore Auditorium, Bangla Academy and Sri Aurobindo Bhavan in Calcutta, West Bengal, India. Again, five new world legislative acts were deliberated and adopted, as well as resolutions, and for the first time ever, a regular budget in terms of the monetary system of the Parliament.

World Legislative Act #48 Collegium of World Judges

World Legislative Act #49 Shipbreaking Code

World Legislative Act #50 Nuclear Power Plant Decommission Fund

World Legislative Act #51 Economic Prosperity Act

World Legislative Act #52 Corporation Act

First Regular Budget of the Provisional Earth Federation, for annual appropriations in Earth Hours for years 2011 to 2016.

First Re-apportionment Decisions of the Provisional Earth Federation, based on World Federal Distinction (2010), subject to refinement, debate, plebiscites and world parliament confirmations.

World Federal Distinction
About World Federal Distinction
USA Map 2010
China Table 2010

World Legislative Decisions Uv In Fohrss Proh WrLd Fed Lahz Uv WrLd Fed Lah Saiz Ohmz

World Legislative Decisions Hohm Peydj

World Legislative Decision

Resolution on the Recognition of the Rights of Animals
Peace of the Brave: Resolution for Palestinian Statehood
Declaration of the Independence of the Earth Constitution and World Legislation
Rules of Procedure for the World Constituent Assembly as per Earth Constitution, Article 18.5.
Resolution on the Spirit of Global Government
Memorial to the Assembly of States Parties
Pledge of Allegiance to the Federation of Earth
Declaration of the Rights of the People of the Earth to create and ratify a World Constitution and hold sessions of the Provisional World Parliament
Recommended tax policy statement
Memorial to General Assembly President Jean Ping, to convene the United Nations General Review Conference for the United Nations to consider and adopt the Earth Constitution
Promotion of Esperanto as world auxiliary language of the Earth Federation
Resolution on Prior Acts of Genocide, Crimes against Humanity and War Crimes
Rules of Procedure for Founding Ratification Convention (to be posted later, as per stipulation decision of the provisional World Parliament)
(Founding Ratification Convention Rules Summary to be posted later, as per stipulation decision of the provisional World Parliament)
World Federal Distinction (About Distinction)
Model of Earth Federation
Declaration of Government and Citizen Responsibilities under the Earth Constitition
**

Attested:

Eugenia Almand, JD, Secretary

Provisional World Parliament

Simp Lang PLanned WorLd Fed Laws In Yeeng Voiss Sownd Chahrz
Iz PLand WrLd Fed Lahz Uv WrLd Fed Lah Saiz Ohmz Uv Lah Saiz Ohmz
Uv Thuh AhL Spundj STeiT Saiz Ohmz Uv Thuh AhL STeiT Saiz Ohmz Peidj LisT.

Earth Constitution in Funetik Inglish iz Rth Konstitwshun uv Wrld Lah uv uv Lahz uv Omneeoh thuh Ahl Spunj Kuntree.

Official Brief History of the Earth Constitution

The relation of the Earth Constitution to the United Nations (by Eugenia Almand)

The Authority and Legitimacy of the Earth Constitution: Response to Basic Questions (by Eugenia Almand)

Constitution for the Federation of Earth - 'The Earth Constitution'

PREAMBLE
Realizing that Humanity today has come to a turning point in history and that we are on the threshold of a new world order which promises to usher in an era of peace, prosperity, justice and harmony;
Aware of the interdependence of people, nations and all life;
Aware that man's abuse of science and technology has brought Humanity to the brink of disaster through the production of horrendous weaponry of mass destruction and to the brink of ecological and social catastrophe;
Aware that the traditional concept of security through military defense is a total illusion both for the present and for the future;
Aware of the misery and conflicts caused by ever increasing disparity between rich and poor;
Conscious of our obligation to posterity to save Humanity from imminent and total annihilation;
Conscious that Humanity is One despite the existence of diverse nations, races, creeds, ideologies and cultures and that the principle of unity in diversity is the basis for a new age when war shall be outlawed and peace prevail; when the earth's total resources shall be equitably used for human welfare; and when basic human rights and responsibilities shall be shared by all without discrimination;
Conscious of the inescapable reality that the greatest hope for the survival of life on earth is the establishment of a democratic world government;
We, citizens of the world, hereby resolve to establish a world federation] to be governed in accordance with this constitution for the Federation of Earth.

Article 1 ‑ Broad Functions of the World Government: Wrld Guvrnment Fungshunz
Article 2 ‑ Basic Structure of World Federation and World Government:
Wrld Fed Guvernment Strukt
Article 3 ‑ Organs of the World Government: Wrld Guvrnment Ohrganz
Article 4 ‑ Grant of Specific Powers to the World Government: Wrld Guvrnment Powrz
Article 5 ‑ World Parliament
Article 6 ‑ The World Executive
Article 7 ‑ The World Administration
Article 8 ‑ The Integrative Complex
Article 9 ‑ The World Judiciary
Article 10 ‑ The Enforcement System
Article 11 ‑ The World Ombudsmus
Article 12 ‑ Bill of Rights for the Citizens of Earth: Rth Sitizen Ryts
Article 13 ‑ Directive Principles for the World Government: Wrld Guvernment Dyrekshun
Article 14 ‑ Safeguards and Reservations
Article 15 ‑ World Federal Zones and the World Capitals: Federal Zones and Capitals
Article 16 ‑ World Territories and Exterior Relations
Article 17 ‑ Ratification and Implementation
Article 18 ‑ Amendments
Article 19 ‑ Provisional World Government
End of the Constitution

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The Constitution for the Federation of Earth was originally ratified at the second session of the World Constituent Assembly held at Innsbruck, Austria in June, 1977; and was amended and ratified at the fourth session of the World Constituent Assembly held at Troia, Portugal in May 1991. The Amended Constitution is being personally ratified by outstanding personalities throughout the world as the campaign for ratification by the people and governments of the world continues.

The World Constitution and Parliament Association keeps files of thousands of persons who have become personal ratifiers of the Constitution in addition to the original signers. The personal ratification campaign continues alongside the campaign for ratification of the peoples and nations of Earth.

CALL to the GLOBAL RATIFICATION and ELECTIONS CAMPAIGN

In the course of history, particularly during the past several hundred years, the technique of a Constituent Assembly has been developed and used under various circumstances as a means to devise the constitutions for democratic governments, either to create new governments where none existed before or to replace old or crumbling governments under both peaceful and revolutionary situations.
Sometimes such assemblies have been appointed by existing governments. At other times, under the most favorable circumstances, such assemblies have been elected by vote of established electorates. But at other times such assemblies have been composed and convened under circumstances where only a limited number of people of the country or areas involved actually took part in the selection of delegates. Only a small minority of any electorate might actually participate during the time when a new democratic government is emerging under conditions of revolution from tyranny or of external image arrow-10x10.png turmoil or urgent crises; or in the absence of any organized political system which was willing or able to supervise a vote of the total potential electorate for such an assembly or newly emerging democratic government.
It is under the later kind of circumstances that the move has gone forward during the years since World War II for the external image arrow-10x10.png of a World Constituent Assembly to devise the constitution for a democratic form of federal world government. No previous world government or competent world authority has existed to organize or supervise elections to such a World Constituent Assembly. No universally approved electoral lists exist for the conduct of such elections. Existing national governments heretofore have proved unwilling or uninterested or hostile or otherwise unable to assist in either the appointment or election of working delegates to such a World Constituent Assembly, despite numerous appeals ‑‑ although these appeals are continuing.
This Constitution has been translated into twenty-two languages and distributed world-wide for study, debates, and organizing by the citizens of Earth.
Under Article XIX of the Constitution Provisional World Parliaments are being held in various locations around the world to begin the process of elaboration of world law as a model and an incentive for the people of the Earth to assert their sovereignty and begin an official World Parliament upon ratification of this Constitution. These have been organized by the World Constitution and Parliament Association and The Institute on World Problems.

See Also:

The relation of the Earth Constitution to the United Nations (by Eugenia Almand)