the-french-artist/wikipedia_20220301.simple_sentence_split huggingface dataset:
Late on August 4, the system dissipated near the Kii Peninsula.
Tropical Depression (13W)
Late on August 8, the JMA upgraded a low pressure area to a tropical depression west of Guam, and the JTWC issued a TCFA.
The system gradually drifted north and early on August 10, the JTWC started monitoring the system as a tropical depression and designated it with 13W. Initially, the JMA predicted the system to strengthen into a tropical storm, but on August 11, as it moved further north into cool waters and experienced unfavourable conditions, the JMA issued their final advisory.
Later, the JTWC too issued their final warning on the system, reporting that it has moved into a subtropical ridge and was expected to dissipate into a remnant low.
However, the JMA continued to track the remants as a weak tropical depression over the next few days until the system dissipated on August 15.
Late on August 8, the JMA upgraded an area of low pressure to a tropical depression, to the northwest of Minamitorishima.
The system gradually moved to the northeast.
On August 10, the system was caught in a moderate vertical wind shear and due to cold sea surface temperature, the system dissipated into a remnant low.
On August 19, a low pressure area developed east-northeast of Guam.
Early on August 20, the system developed a broad area of low level circulation center and a good divergence aloft becoming more well defined.
Later that day, the JMA upgraded the system to a tropical depression southeast of the Bonin Islands.
On August 22, the system started interacting with an anticyclone and was exposed to a strong vertical wind shear, prompting the JMA to stop monitoring the system as a tropical depression, as the system dissipated to a remnant low.
However, at midnight, the same day, the remnants regenerated, and the JMA started tracking the system as a tropical depression again, until it last appeared near Okinawa, Japan on August 25, as the system dissipated completely.
Typhoon Nanmadol (Mina)
Late on August 19, an area of low pressure developed north of Palau.
Early on August 20, the system became more better organized and developed a low-level circulation center.
The system then turned north and continued to drift north until on August 21, when the JMA upgraded the low pressure area to a tropical depression east of Philippines.
The JTWC also issued a Tropical Cyclone Formation Alert (TCFA) on the system reporting that the system was becoming more well organized.
Later that day, the PAGASA started monitoring the system as a tropical depression and named it Mina.
Late on August 22, the system became more well organized prompting the JTWC to initiate advisories on the system, designating it with 14W. On August 23, the JMA upgraded 14W to a tropical storm, naming it Nanmadol.
Overnight, the system continued to intensify and early on August 24, the JMA upgraded Nanmadol to a severe tropical storm.
Later that day, convective banding improved and Nanmadol developed an eye-like feature.
As a result, Nanmadol continued to intensify rapidly and became a typhoon, by midnight, that day.
Nanmadol continued to drift northeast and made landfall over Gonzaga, Cagayan, Philippines with strong winds of over .
Nanmadol weakened significantly after interacting with land and early on August 28, the JMA downgraded Nanmadol to a severe tropical storm.
Late on August 28, Nanmadol made its second landfall over Taimali in the Taitung County of Taiwan and started weakening.
Landfall weakened the system rapidly prompting the JMA to downgrade Nanmadol to a tropical storm with winds of under .
Soon it started experiencing strong wind shear and continued weakening.
The shear pushed convection about  south of the LLCC.
The system also accelerated towards China at  and weakened to a minimal tropical storm.
After its third landfall over Fujian, China, Nanmadol weakened rapidly prompting both the JTWC and the JMA to issue their final warnings on the system.
On August 27, five people died after Nanmadol caused landslides.
At least two Filipino fishermen were reported to be missing after Nanmadol's strong winds whipped up large waves.
Typhoon Talas
Late on August 22, an area of low pressure developed to the west of Guam.
At midnight that day, the system became sufficiently well organized that the JMA started tracking it as a tropical depression.
On August 23, the system moved into an environment of low wind shear and warm sea surface temperatures prompting the JTWC to issued a TCFA on it.
By August 25, the system grew strong enough that the JMA upgraded it to a tropical storm, naming it Talas.
Later that day, the JTWC followed suit and initiated advisories on Talas.
Talas continued to strengthen and by midnight that day, it became a severe tropical storm.
Over the next few days, Talas continued to drift north very slowly until late on August 29, when the JMA upgraded Talas to a typhoon.
Soon, a subtropical ridge to the west of the storm weakened and the subtropical ridge to the east of the system pushed Talas to the west.
As a result, Talas accelerated towards the west maintaining strength and outflow.
An upper-level cyclone over the system suppressed the convection and kept it from reaching the center.
Therefore, Talas remained weak and did not strengthen further.
Convection never managed to consolidate the center and convective banding remained well away from the fully exposed low-level circulation center.
The convective banding continued to expand more and more with the outer rainbands already brushing parts of Japan.
Coastal areas in the nation have already reported gale-force winds several hours before landfall, while the Omega block continued to drive Talas towards the nation.
Land interaction weakened Talas, prompting the JMA to downgrade Talas from a typhoon to a severe tropical storm with winds of under .
Early on September 3, Talas made landfall over Aki, Japan.
After landfall, Talas accelerated north at over  and its central convection became significantly eroded and was displaced to the northeast as Talas was exposed to a very strong wind shear of over  that made the LLCC very distorted and difficult to pin-point.
Talas was embedded in a baroclinic zone and the JTWC anticipated an extratropical transition, which prompted them to issue their final warning on the system.
On September 5, the JMA issued their final warning on the system, reporting that Talas has become extratropical on the Sea of Japan.
Tropical Storm Noru
On September 1, a low pressure area formed to the northeast of Guam.
On the next day, the JMA started monitoring the low pressure area as a tropical depression.
Soon, the system developed a well-defined but partially exposed low-level circulation center (LLCC), prompting the JTWC to issue a tropical cyclone formation alert.
On September 3, the central convection around the LLCC deepened with favorable equatoward outflow prompting the JTWC to initiate advisories on the system, designating it with 16W. Soon, 16W accelerated north at over  with its LLCC being being consolidated by convection.
Also, data from an ASCAT scatterometer pass revealed that the LLCC was tightly wrapped with  winds prompting the JTWC to upgrade 16W to a tropical storm.
An Aqua microwave imagery depicted that the LLCC remained partially exposed though consolidated with deep central convection.
Albeit in an area of moderate vertical wind shear, an anticyclone enhanced northeastward outflow while a tropical upper tropospheric trough (TUTT cell) suppressed the outflow towards the west.
As 16W continued to accelerate north at a staggering , convective banding became fragmented and detached behind the main area of central convection.
However, the outflow to the southeast of the storm remained favorable and 16W continued to strengthen, prompting the JMA upgraded the system to a tropical storm, naming it Noru.
Late on September 4, Noru's LLCC that remained partially exposed since formation unexpectedly became elongated and started weakening.
However, data from an ASCAT scatterometer pass depicted that the LLCC had an expansive area of strong tropical storm force winds along the eastern and northern peripheries.
A TUTT cell wrapped the east and northeastern sides of Noru suppressing its outflow.
Soon, the convective banding, which was already fragmented started becoming disorganized causing Noru to start weakening.
A new TUTT cell developed over the system and started restraining outflow.
As a result, the LLCC became fully exposed and virtually lacked convection.
The TUTT cell moved over Noru snuffing outflow in all directions and sheared the remnant central convection, prompting the JTWC to downgrade Noru to a tropical depression.
However, data from an scatterometer pass depicted that Noru had winds of over  near the center, prompting the JTWC to reupgrade the system to a tropical storm.
On September 5, Noru started to appear like a hybrid system, primarily showing subtropical characteristics.
The JTWC added that Noru was undergoing an extratropical transition and would become an extratropical cyclone within 24 hours.
Noru continued to transition into an extratropical cyclone with a broadening LLCC and weaker winds at the core, being embedded in an upper-level trough that suppressed the formation of convection within the LLCC.
With the extratropical transition well underway, Noru drifted into an area of low sea surface temperatures and started weakening, prompting the JTWC to downgrade Noru to a tropical depression.
On September 6, Noru finished the extratropical transition becoming an extratropical cyclone east-southeast of Hokkaido, Japan, prompting the JMA and the JTWC to issue their final warning on the system.
Tropical Storm Kulap (Nonoy)
Late on September 4, an area of low pressure developed to the southeast of Okinawa, Japan.
Over the next two days, the system drifted north and developed a well defined LLCC with organized convective banding, prompting the JMA to upgrade the low pressure area to a tropical depression.
On September 7, convection consolidated the low-level circulation center very well with tightly curved banding wrapped into it.
Also, high sea-surface temperatures and very low wind shear caused the system to undergo rapid deepening, prior to which, the JMA upgraded the system to a tropical storm and named it Kulap.
However, the system stopped strengthening soon after as the LLCC became partially exposed and the convection was displaced to the south.
Kulap remained small in size and dry air entering from the western periphery kept it from strengthening further.
Wind shear increased, pushing convection about  south of the LLCC.
Also, Kulap was beneath a tropical upper tropospheric trough (TUTT cell) that caused subsidence.
A mid-level subtropical steering ridge cuased Kulap to track in a northwestward direction.
On September 8, Kulap moved into the east-northeast periphery of the Philippine Area of Responsibility (PAR) prompting the PAGASA to start issuing advisories on the system, naming it Nonoy.
However, Kulap quickly accelerated north and exited the PAR on the same evening, prompting the PAGASA to issued their final advisory on the system.
After increasing wind shear caused further weakening, the JTWC downgraded Kulap to a tropical depression late on September 8.
Early on September 10, the JMA too downgraded Kulap to a tropical depression, and continued to track Kulap's remnants as a tropical depression until it finally dissipated early on September 11.
Typhoon Roke (Onyok)
Early on September 8, a cluster of thunderstorms came together as a low pressure area with imporoving outflow and a developing low-level circulation center (LLCC).
Later that day, the JMA upgraded the low pressure area to a tropical depression north-northeast of the Northern Mariana Islands.
Over the next two days, the system gradually drifted west and intensified slightly, prompting the JTWC to issue a Tropical Cyclone Formation Alert (TCFA) on it.
Convection gradually consolidated the LLCC and the JTWC initiated advisories on the system on September 11, designating it with 18W. The next day, the depression drifted into the Philippine Area of Responsibility (PAR) and the PAGASA initiated advisories on the depression, naming it Onyok.
However, just as similar to Kulap, Onyok also exited the PAR in 6 hours from entering the region.
In an advisory, the JTWC reported that there were at-least two more vortices associated with the system, that caused an abrupt, erratic movement.
However, being in an area of warm sea surface temperatures and low vertical wind shear, the depression continued to strengthen and on September 13, the JMA upgraded the depression to a tropical storm and named it Roke.
On September 17, Roke developed a small, deep convective eye promoting the JMA to upgrade Roke to a severe tropical storm with winds of over .
Between September 19 and 20, Roke underwent Explosive intensification, a more extreme case of rapid deepening that involves a tropical cyclone deepening at a rate of at least 2.5 mbar per hour for a minimum of 12 hours.
Also, they added that Roke developed a  eye and a good poleward outflow channel.
On September 21, Typhoon Roke made landfall over Hamamatsu, Japan at about 5:00 UTC (14:00 JST).
Soon Roke started weakening as cloud tops started getting warmed up and eye diameter started to decrease.
However, the system still maintained a near radial outflow and the convective structure continued to remain organized that kept Roke from dissipating rapidly.
Although Roke entered a de-intensification phase, it still had plenty of strength that posed a great threat to regions of Japan.
Being about  southwest of Yokosuka, Kanagawa, the typhoon accelerated north-northwestward at about  with winds of over  (1-min sustained) being a Category 3 typhoon on the SSHS.
Being embedded in the baroclinic zone, Roke started its extratropical transition.
Also, land interaction severely weakened the storm to a minimal Category 1 typhoon with winds of under  (1-min sustained).
Only six hours later, the storm further weakened and accelerated northeastward at about  with rapidly dissipating deep convection completely sheared to the northeast of the LLCC.
As a result, the JTWC ceased advisories on the storm, as it became fully extratropical.
Typhoon Sonca
Early on September 13, a low pressure area formed northeast of the Northern Mariana Islands.
The system gradually drifted north and steadily intensified until the next day when the JMA upgraded the system to a tropical depression.
Later on September 14, the JTWC issued a Tropical Cyclone Formation Alert (TCFA) on the system reporting that the system could intensify into a tropical storm within 24 hours from then.
Convection rapidly consolidated the center with persistent, deep convection around the northeastern periphery, prompting the JTWC to initiate advisories on the system, designating it with 19W. Soon, the JMA also initiated advisories on the system, upgrading it to Tropical Storm Sonca.
In the begging, Sonca seemed to have intensified rapidly since formation, however, soon the storm weakened back to a minimal tropical storm because of dry air entering the LLCC that caused it to elongate and weaken.
However, that was not for too long as vigorous convection persisted over the well defined LLCC with tightly curved banding wrapped in, Sonca continued to strengthen gradually and the JTWC reported winds of at-least  near the center.
As Sonca continued to strengthen, and the JMA upgraded it to a severe tropical storm on September 17.
Later that day, Sonca developed a large  ragged eye with deep convective banding tightly wrapped into it.
As a result, Sonca strengthened more rapidly and by early the next day, it became a typhoon.
On September 18, Sonca reached a peak intensity of  (1-min mean) and  (10-min mean) and soon the convection around the northern periphery started weakening.
Being embedded in a baroclinic zone with low sea surface temperatures, Sonca started its extratropical transition late on September 19.
The transition took place relatively fast because of a frontal boundary and the JTWC reported that Sonca became extratropical early on September 20, while the JMA did the same later in the evening.
Early on September 14, the JMA started monitoring a cluster of thunderstorms to the southeast of Taiwan as a tropical depression.
But because of the land interaction, the system could not be empowered and the JMA stopped tracking the depression late on September 15, as the system dissipated.
Typhoon Nesat (Pedring)
In the evening of September 21, a low pressure area developed to the east-southeast of Palau.
The low gradually drifted west and became more well organized prompting the JTWC to issue a Tropical Cyclone Formation Alert (TCFA) on it.
Later, the LLCC became well organized with flaring deep convection developing around it, so the JMA started monitoring the low as a tropical depression.
Later on September 23, the JTWC also initiated advisories on the system designating it with 20W. Early on September 24, the JMA further upgraded 20W to a tropical storm and named it Nesat.
Nesat continued to drift west with expanding deep convection around the entire system and consolidating convection around the LLCC.
The mid-level warm anomaly near the system continued to intensify and convective banding near the LLCC became more and more tighter.
As a result, the JMA upgraded Nesat to a severe tropical storm on September 25.
Late on the same day, the JMA further upgraded Nesat to a typhoon.
Tropical Storm Haitang
On the evening of September 21, at almost the same time when Nesat was first seen, another low pressure area persisted far south of Hong Kong.
The low slowly drifted north and strengthened slowly until on September 24, when the JMA upgraded the system to a tropical depression east of Vietnam.
Later that day, the JTWC issued a Tropical Cyclone Formation Alert stating that the low could develop into a tropical cyclone.
Early on September 25, the JMA upgraded the system to a tropical storm and named it Haitang.
Typhoon Nalgae (Quiel)
On September 26, the Japan Meteorological Agency (JMA) started to monitor a weak tropical depression.
It had developed about  to the northwest of Manila in the Philippines.
The next day the JTWC issued a tropical cyclone formation alert on the system.
However less than 3 hours later, the JTWC designated it as Tropical Depression 22W. JMA reported that the depression had become a tropical storm and named it Nalgae.
The storm slowly drifted to the west.
It got stronger slowyl.
Nalgae developed a microwave eye like feature and well defined convective banding in all the quadrants.
The system had a tiny radius of winds.
It was still strengthening significantly and was very well defined.
On the evening of September 28, the JMA reported that Nalgae continued to intensify.
They upgraded it to a severe tropical storm with winds of over .
On that night, the PAGASA began advisories on Nalgae.
They gave it the local name Quiel as it entered the Philippine Area of Responsibility (PAR).
Late on September 29, the JMA upgraded Nalgae to a typhoon.
Nalgae quickly intensified on September 30, and became a category 4 super typhoon early on October 1.
This was just before making landfall over Luzon.
Due to land interaction and colder sea surface temperature in the South China Sea, the JMA downgraded Nalgae to a severe tropical storm on October 2.
Then a tropical storm late on October 3.
The JTWC downgraded Nalgae to a tropical depression on October 4.
The JMA also did it on the next day.
Later on October 5, the last low of Nalgae dissipated.
Hitting the Philippines just days after Typhoon Nesat, Nalgae caused further damage across Luzon.
It was first feared that Nalgae would cause much more damage to Luzon.
But damage from the storm was lighter than Typhoon Nesat.
Nearly 2,900 homes were destroyed and about another 15,400 took damage.
At least 18 people were killed by the storm and another 7 were reported as missing as of October 11.
A total of 1,113,763 people were affected by the storm.
Total losses in the country reached just over 115 million PHP (US$2.62 million).
Tropical Storm Banyan (Ramon)
On October 7, the JTWC started monitoring a tropical disturbance about 750 km (465 mi) to the south of Hagåtña, Guam.
Over the next couple of days the system gradually developed further while moving towards the west.
The JMA reported on October 9, that the disturbance had become a tropical depression.
Early on October 10, the JTWC upgraded the system to a tropical depression called 23W. The PAGASA also upgraded it to a tropical depression and named it Ramon.
On October 11, the JMA and the JTWC upgraded the system to a tropical storm and named it Banyan.
Early on October 12, Banyan made landfall over Leyte, Philippines.
The JTWC downgraded it to a tropical depression.
A half day later, the JMA also downgraded Banyan to a tropical depression.
The system dissipated in the South China Sea on October 16.
While going through the Philippines, Banyan had heavy rains across much of the country.
This led to widespread flooding.
A total of 75,632 people were affected by the storm.
Severe Tropical Storm Washi (Sendong)
On December 11, a disturbance formed and stayed near Chuuk.
On December 13, the low pressure area quickly got stronger.
On the same day, the JTWC upgraded the low pressure to a tropical depression.
They named it 27W. The JMA also upgraded it to a tropical depression.
The JTWC upgraded the system to a tropical storm on December 14.
They then downgraded it to a tropical depression early on December 15.
The PAGASA called it Sendong as it entered the Philippine Area of Responsibility.
After passing Palau on December 15, both the JTWC and the JMA upgraded the system to a tropical storm.
They named it Washi.
On December 16, Washi made landfall over Surigao del Sur, a province of the Philippines.
Several hours later, Washi arrived at the Sulu Sea and regained its strength quickly.
Late on December 17, Washi crossed Palawan, and arrived at the South China Sea.
On December 19, Washi weakened into a tropical depression and dissipated.
Storm Names
Within the Northwestern Pacific Ocean, there are two separate agencies who assign names to tropical cyclones which often results in a cyclone having two names.
The Japan Meteorological Agency names tropical cyclones should they be judged to have 10-minute sustained windspeeds of 65 km/h, (40 mph), to the north of the equator between the 180° and 100°E. Whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility between 135°E and 115°E and between 5°N-25°N even if the cyclone has had a name assigned to it by the Japan Meteorological Agency.
International names
Tropical Cyclones are named from the following lists by the Regional Specialized Meteorological Centre in Tokyo, Japan, once they reach tropical storm strength.
Names are contributed by members of the ESCAP/WMO Typhoon Committee.
Each of the 14 nations or territories submitted 10 names, which are used in alphabetical order, by the English name of the country.
The next 24 names on the naming list are listed here.
The Philippine Atmospheric, Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility.
PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility.
Should the list of names for a given year prove to be insufficient, names are taken from an auxiliary list, the first 10 of which are published each year before the season starts.
During their 2012 annual session the ESCAP/WMO Typhoon Committee said that the name Washi would be retired from its naming lists.
The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) said that the names Bebeng, Juaning, Mina, Pedring were retired from PAGASA's list of local names after they each caused over 1 billion PHP in damages to the Philippines during 2011.
The name Sendong was also retired from the list after it caused over 300 deaths, when it made landfall on the Philippines during December 2011.
This table lists all the storms that developed in the western Pacific Ocean to the west of the International Date Line during the 2011 season.
It includes their intensity, duration, name, landfalls, deaths, and damages.
All damage figures are in 2011 USD.
Damages and deaths from a storm include when the storm was a precursor wave or extratropical low.
Broadly speaking, the ACE is a measure of the power of a typhoon multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong typhoons, have high ACEs.
ACE is calculated for only full advisories on specifically tropical systems reaching or exceeding wind speeds of 34 knots (63 km/h, 39 mph), or tropical storm strength.
Accordingly, tropical depressions are not included here.
The ACE also does not include subtropical storms.
Later the JMA reexamines the data, and produces a final report on each storm, which can lead to the ACE for a storm being revised either upward or downward.
Until the final reports are issued, ACEs are, therefore, provisional.
2011 Pacific hurricane season
2011 North Indian Ocean cyclone season
Southwest Indian Ocean cyclone seasons: 2010-11, 2011-12
Australian region cyclone seasons: 2010-11, 2011-12
South Pacific cyclone seasons: 2010-11, 2011-12
"The Saga Begins" is a song by "Weird Al" Yankovic.
It is a parody of "American Pie" by Don McLean
"It's All About the Pentiums" is a song by "Weird Al" Yankovic.
It is a parody of "It's All about the Benjamins (Rock Remix)" by Sean "Puff Daddy" Combs .
It is about a man who is obsessed with computers.
"Pretty Fly for a Rabbi" (also called "Pretty Fly (For a Rabbi)" in Australia) is a song by "Weird Al" Yankovic.
It is a parody of "Pretty Fly (For a White Guy)" by The Offspring.
"You're Pitiful" is a parody of "You're Beautiful" by James Blunt by parody musician "Weird Al" Yankovic.
It was released only online in June 2006.
Blunt's record label did not want Yankovic to release the song, so he put it on his website for a free download.
A stage or age in geology is a period of time measured in millions of years.
It is less than an epoch, and more than a chron or chronozone.
Technically, a stage is a succession of rock strata laid down in a single age on the geologic timescale, which usually represents millions of years of sedimentation or deposition.
An example of a stage in the Geologic time scale is the Kimmeridgian.
The term red beds usually refers to strata of reddish-colored sedimentary rocks such as sandstone, siltstone or shale that were deposited in hot climates under oxidizing conditions.
They are usually formed in terrestrial situations: on land, and in rivers and lakes.
The red color comes from iron oxide in their mineral structure.
Although they have been deposited throughout the Phanerozoic, they are most commonly associated with rocks deposited during the Devonian, Permian and Triassic periods.
The Old Red Sandstone is one of the most famous rock formations.
The formation of red beds has been much discussed.
The basic chemical change which produces them is oxidation.
At first it was thought they indicated desert conditions.
Some do, and this can be proved if the strata show signs of dune formations.
"In modern times red beds are often found in low-latitude tropical climates, and they are always associated with oxidising conditions... the redbeds may be associated with rain forests or places where the rainfall is high but confined to monsoonal periods... A good model for red bed-producing conditions today is the Amazon basin.
Torridonian sandstone
Wesel is a city in the German state of North Rhine-Westphalia.
Wesel is near to Duisburg and belongs to the Ruhr area.
Titanosaurus  was a genus of sauropod dinosaur, first described by Lydekker in 1877 from fragments, but not confirmed by later research.
Titanosaurus was 9-12 metres (30-40 ft) long and weighed about 13 tons.
Titanosaurus has traditionally been treated as a "wastebasket taxon" for poorly preserved sauropod remains.
The most well-known species of Titanosaurus, "Titanosaurus" colberti, has been renamed Isisaurus.
The remains were from the Upper Cretaceous of India.
The First Minister and the deputy First Minister (Irish: Céad-Aire agus an leas-Chéad-Aire, Ulster Scots: Heid Männystèr an tha Heid Männystèr depute), (FM/dFM for short), are jobs in the Northern Ireland Government.
The First Minister is not more important than the deputy First Minister.
The two positions are a diarchy, meaning they have equal power; both are nominated and appointed by members of the Northern Ireland Assembly.
Currently, the position is held by Sir Jeffrey Donaldson (DUP) and Michelle O’Neill (Sinn Fein).
Before however, the incumbents were Peter Robinson of the Democratic Unionist Party as First Minister and Martin McGuinness of Sinn Féin as deputy First Minister.
The First Minister and the deputy First Minister are elected on a joint ticket.
Under the St Andrews Agreement, the Leader of the largest party nominates the First Minister, and the leader of the next largest party that is in the other group nominates the deputy First Minister.
Their joint nomination has to obtain an overall majority in the Assembly along with a majority of both designated Nationalist MLAs and designated Unionist MLAs.
Designated Other MLAs also vote.
"Deputy" becomes "deputy"
It was neither Mr McGuinness nor his advisers who asked for the change.
The Speaker of the Northern Ireland Assembly, William Hay, ordered the change and the capital D was dropped from Hansard references.
The Office of the First and deputy First Minister still uses both versions of Mr McGuinness' title on their website, and their archive of press releases has been changed, but the capital D still appears in some places, and a spokesman confirmed on 20 March 2008 that the office has "no plans" to change the OFMDFM logo.
However, the Assembly committee that looks at their work is now listed as the "Committee for the Office of the First Minister and deputy First Minister".
It was decided that Mr McGuinness should be the deputy First Minister, unless all the other letters in the title are in capitals.
Confusion is not completely resolved however; if Mr McGuinness writes to the Assembly committee, his note will have a letterhead that comes from the Office of the First Minister and Deputy First Minister, but he'll get a reply back from the Committee for the Office of the First Minister and deputy First Minister.
OFMDFM
Outlook is a town in west central Saskatchewan.
It is about 80 kilometres south-southwest of Saskatoon.
About 2,000 people live in Outlook.
It has the longest pedestrian bridge in Canada, the Skytrail.
The Skytrail Bridge is a bridge in Outlook, Saskatchewan that crosses the South Saskatchewan River.
Today, it is a pedestrian bridge, but it was a railway until 1987.
It is now the longest pedestrian bridge in Canada.
Scrophulariaceae, the figwort family, is a family of flowering plants, with around 3000 species in around 200 genera, mainly found in the northern temperate regions of the world.
The family name is based on the name of the included genus Scrophularia.
A cold seep (sometimes called a cold vent) is an area of the ocean floor where hydrogen sulfide, methane and other hydrocarbon-rich liquids leak out of the Earth's crust, often in the form of a brine pool.
Cold seeps form a biome supporting several native species.
Cold seeps change the shape of the ocean floor over time, where reactions between methane and seawater create carbonate rock formations and reefs.
These reactions may change when bacteria are present.
Cold seeps at different depths have different names.
Other kinds of cold seeps are:
oil/gas seeps
gas seeps: methane seeps
gas hydrate seeps
brine seeps are forming brine pools
pockmarks
mud volcanos
Formation and ecological succession
Cold seeps occur over cracks in the seafloor caused by the movement of the Earth's crust.
Oil and methane "seep" out of those cracks, get dissolved by tiny bits of rock, and emerge over an area several hundred meters wide.
Methane () is the main part of what we commonly refer to as natural gas.
But in addition to being an important energy source for humans, methane also forms the basis of a cold seep ecosystem.
Calamba City is a city in the province of Laguna, Philippines.
It is the regional center of Calabarzon, after Lucena City, Calamba is a component city in the placed,
first is San Pablo City, The City of Calamba, is one of the fastest growth city in region 4A, and it growth population, which divided into barangays, because of its economic some, commercials, entertainment, factory companies and others, are served in city, Calamba City is  south of Manila.
Calamba City is a popular tourist destination.
It has several hot spring resorts.
Most of these are in Barangay Pansol.
There are 651 resorts and hot springs in the city.
The Canlubang Golf and Country Club has been the host of many  Philippine Opens.
Calamba is also an important modern industrial center in the CALABARZON region.
This is shown by the large number of industrial parks and business estates in the city.
454,486 people live in the city (2015).
There are in 58,466 households.
Calamba City is  the most populated city in Laguna province.
San Pedro, Santa Rosa City, Biñan City, and San Pablo City follow it as the top 5 municipalities and cities by number of people in the province.
Calamba City is the birthplace of José Rizal.
He is a national hero in the Philippines.
The name of the city comes from a legend.
The legend says that during the early time of the Spanish period in the country, two "guardias civil" or Spanish soldiers were lost.
As they moved through the area that is now Calamba, they met a young woman.
She came from a river carrying a jar of water and a wooden stove.
The soldiers asked the lady what the name of the place was.
They asked this in Spanish and used an angry tone to hide the fact that they were lost.
She did not speak Spanish and thought she was being questioned about what she was carrying.
She answered "kalan-banga", meaning "clay stove" (kalan) and "water jar" (banga).
Because they could not pronounce it correctly, the city has been called Calamba since then.
This legend is immortalized with a large concrete water jar built in the city plaza with the names of the city's barangays written on it.
It is said to be the World's Biggest "Claypot".
This same jar is also in the city's seal.
The idea to build the plaza came from Dr. Agapito Alzona.
He was a town councilor at the time.
It was built on an unused area that was at one time the old town market.
The plaza was built in 1939.
Before it became a separate city, Calamba was a part of Tabuco.
Tabuco is now known as  Cabuyao, Laguna.
Calamba became an independent pueblo on August 28, 1742.
While the area was under the control of the Japanese in World War II, the city was the site of a massacre.
The Imperial Japanese Army killed at least 2,000 civilians.
With the passage of  Republic Acts of the Philippines-Republic Act,No.
9024 on April 7, 2001 and the approval of the people on April 21, Calamba went from being a  municipality into being Laguna's second component city.
San Pablo City was the other component city at the time.
Calamba is seen as a major growth center.
Calamba has been the home to five national heroes:  Dr. Jose Rizal, General Paciano Rizal, Teodora Alonzo, General Vicente Lim, and Lt.
Geronimo Aclan.
The main church in Calamba City is the St. John the Baptist Church.
It was built in 1859.
The church was burned by the Japanese during World War II.
It was rebuilt by Fr.
Eliseo Dimaculangan.
It was the christening site of Jose Rizal.
The original baptismal font has been is still there.
Calamba City Website
Calamba, Laguna Website
Laguna is a landlocked province in the Philippines.
It is about 30 kilometres south of Manila.
Laguna is named after "La Laguna" which means the lake, meaning Laguna de Bay.
This is the largest lake in the Philippines, and is on the north edge of the province.
Laguna province has six cities: Biñan, Cabuyao, Calamba, San Pablo, San Pedro, and Santa Rosa.
There are two international schools, IB World Schools, to be specific, located in Biñan: Brent International School Manila, and The Beacon Academy.
Deposed Queen Lady Yun or Waste Queen Lady Yun (, hanja:廢妃 尹氏, 1445? -
August 16, 1482) was Queen of Joseon Dynasty, King of Joseon Dynasty Seongjong's Second Wife, Mother of King Yeonsan.
first cousin once removed to Shin Suk-ju.
http://people.aks.ac.kr/front/tabCon/ppl/pplView.aks?pplId=PPL_6JOa_A1445_2_0019315
http://100.naver.com/100.nhn?docid=181894
http://www.ohmynews.com/NWS_Web/view/at_pg.aspx?CNTN_CD=A0000839977
1482 deaths
The Institute of Welsh Affairs is an independent, think-tank based in the capital of Wales, Cardiff.
It focuses its research on politics, culture, economy, education, environment, science and technology in Wales, with the aim of developing plans for "policy innovation and improvement" and promoting new thinking on Welsh issues.
The IWA publishes numerous reports on the research it carries out, and organises public seminars and conferences to encourage discussion and debate.
It is highly regarded for the quality of its work and its commitment to informed public discussion.
2010 saw the begin of ClickonWales.org, the IWA’s online news-analysis magazine.
ClickonWales is designed to bring users a new level of regular commentary and analysis on Welsh affairs, and opportunities for debate.
Expert contributors and commentators from across the political spectrum will be commissioned daily.
The site also features the ‘Wales factfile’ and the ‘Lecture Library’.
Wales factfile is a handy one-stop shop for information and data about many aspects of Wales and its economic, social, cultural and political life.
The ‘Lecture Library’ is a place where organisations will be able to post
Foundation of the IWA
The Institute is governed by a Board of Trustees.
Its first chairman was Henry Kroch, then chairman of AB Electronics.
Since 1992, the chairman has been Geraint Talfan Davies, and since 1996 the director of the organisation has been former journalist and television producer, John Osmond.
The IWA has five area branches – for north Wales, for west Wales, Swansea Bay, Gwent, and Cardiff and the Valleys.
A sixth 'virtual' branch - IWA Women - has been formed to raise the profile of women's concerns in Wales and to increase the engagement of women with the IWA and civil society in Wales more generally.
The IWA publishes a journal three times a year (in spring, summer and winter), called Agenda.
First published in 1994, Agenda contains numerous articles on current issues in Wales, written by experts in their field, including academics, politicians and business people, and a wide range of participants from Welsh civil society.
It now publishes a regular bulletin on developments in the Assembly, Assembly Bwletin Cynulliad, published in association with Grayling Wales.
These can be downloaded from clickonwales.org .
In addition,  the IWA has published a multitude of research reports, discussion papers and books.
One of the IWA’s central activities is holding events which are designed to disseminate information to the public on a host of public policy issues.
The events range from the smaller ‘coffee shop’ debates to full-scale conferences.
Typically, an IWA event will focus on a contested issue in Welsh politics.
It will bring in an expert (or number of experts) who have detailed knowledge and understanding of the issue, to clearly present both side’s arguments clearly.
This is inline with the first part of its mission, which to help raise the level of public debate on issues affecting Wales, by placing quality information in the public domain.
In 2010 the IWA began the Inspire Wales Awards, in association with the Western Mail .
The Awards aim to raise the profile of Welsh men and women who are making a contribution to our society, to encourage active citizenship and create role models for others.
Categories for the awards include the environment, business, education, sport, and arts, media and the creative industries.
2011 sees the IWA/Western Mail Business Awards, celebrating business achievement in Wales.
In November 2006 the IWA published a report entitled Time to Deliver: The Third Term and Beyond.
This looked at policy options for the Assembly’s third term, and was the result of work by eight study groups in individual policy areas.
In 2010 the IWA's director, John Osmond was asked by the Older People's Commissioner to carry out a study exploring Welsh policy responses to our rapidly ageing society, in particular the Welsh Government’s policy which has been developing in a number of innovative ways since 2003.
The findings were published in the bilingual report, 'Adding Life to Years / Ychwanegu Bywyd at a y Blynyddoedd'.
The IWA's most recent publication, entitled 'Engaging Wales' disengaged youth', explores the issue of so-called 'NEETS' - Children Not in Education, Employment of Training.
It contains contributions from experts in the fields of youth policy, education, employment, and youth-centred charities.
A full list of the IWA's research outputs is available on its website .
Public record filed at Companies House, (Company No: 02151006), October 2007.
Public record filed at Charity Commission, (Charity No: 1078435), October 2007.
Welsh Baccalaureate Qualification Internal Evaluation, University of Bath.
A 'Quarter-Way House' , John Osmond, November 2006.
IWA Website
ClickonWales - News analysis from and about Wales
Table Mountain is a flat-topped mountain overlooking the city of Cape Town in South Africa.
It is 1084.6 meters (3,563-feet) tall, of sandstone and granite.
With nearby mountains and Table Bay, it surrounds the central part of Cape Town.
It is a significant tourist attraction, featured in the flag of Cape Town and other local government insignia.
Many visitors use the Table Mountain Aerial Cableway or hike to the top.
The mountain forms part of the Table Mountain National Park.
The upper part of the mountain mesa (table) consists Silurian/Ordovician quartzitic sandstone, commonly referred to as Table Mountain Sandstone (TMS).
It is highly resistant to weathering and forms steep grey crags.
Below the sandstone is a layer of micaceous shale, which weathers quite readily.
The basement of folded metamorphic shales intruded by the Cape Granite are of late Precambrian age.
A drawing of Table Mountain from the 1600's.
Fingal's Cave is a sea cave on the uninhabited island of Staffa, in the Inner Hebrides of Scotland, part of a National Nature Reserve owned by the National Trust for Scotland.
It is formed entirely from hexagonally jointed basalt columns.
These are part of the same ancient lava flow as the Giant's Causeway in Northern Ireland and those of nearby Ulva.
In both cases, the cooling surface of the mass of hot lava cracked in a hexagonal pattern in a similar way to drying mud cracking as it shrinks.
These cracks slowly extended down into the mass of lava as it cooled and shrank to form the columns, which were later exposed by erosion.
The size of the cave, and its naturally arched roof, and the eerie sounds produced by the echoes of waves, give it the atmosphere of a natural cathedral.
The cave's Gaelic name, Uamh-Binn, means "cave of melody."
In art and literature
Romantic composer Felix Mendelssohn visited in 1829 and wrote Die Hebriden (in English, Hebrides Overture Opus 26, commonly known as Fingal's Cave overture), inspired by the weird echoes in the cave.
Other famous 19th-century visitors included author Jules Verne; poets William Wordsworth, John Keats, and Alfred, Lord Tennyson; and Romantic artist J.M.W. Turner, who painted "Staffa, Fingal's Cave" in 1832.
Queen Victoria also made the trip.
Deadpool (Finn Anderson the ranga), better known as Flanders not Randerz, is a comic book character in the Marvel Universe published by Marvel Comics.
The character was created by Rob Leifeld in 1991.
Deadpool began as a villain but is currently being used as an anti-hero and in his own comic book series he ended as a good guy.
He is currently one of the most popular Marvel characters.
He has had many of his own book series as well as been in most of Marvel's other titles.
He is often seen in several of the X-Men series of books and is a regular character in the series "Uncanny X-Force".
His clothing is colored red and black, and he has two guns and short katanas as well as many other weapons.
Deadpool's special power is regeneration.
His body can repair itself from any injury.
He has formed a relationship with the personification of Death but because his healing power is so strong, he cannot die.
This is a common theme in his stories.
Deadpool is well known for "breaking the fourth wall".
He knows he is a comic book character.
Deadpool will often talk to the readers or refer to a specific issue when talking about something that happened in the past.
He also can transport to the other alternative universes.
His fighting skills are also very known.
In the comic book universe, Deadpool was mostly considered neutral and sometimes even evil, but near the end of the series he was proved to be a good person.
He tried really hard to fight his own psychotic mind behaviour and stop killing people.
He got married with a person that cared for him and had a daughter.
He made friends with an agent of S.H.I.E.L.D. and by himself destroyed a whole evil army that was trying to kill his family.
In the end, on a vacation with his family and friends, Deadpool hugged his daughter as a second earth came crashing down from the sky, presumably killing him and his family and friends, along with many lives on earth, joining up the story with Secret Wars.
He has been portrayed by Ryan Reynolds in X-Men Origins: Wolverine before having a more faithful take starting with Deadpool.
Fictional Canadian people
Fictional characters with slowed ageing
A villain is a bad person in fiction.
The word comes from a Latin word meaning a feudal farm worker or peasant.
Villains, or antagonists, are usually found in fiction, such as books and movies.
The audience do not usually like the villain and they support the hero or heroine.
However, in some cases the villain is more praised by the public than the hero, as the example of Joker in the Batman franchise.
In some movies and books (such as the movie Ocean's Eleven), the villain is a good person and the hero/heroine is bad (such as a robber).
When used in comic books, they are depicted as supervillains.
Supervillains usually hold some kind of unnatural force.
The Giant's Causeway  is an area of about 40,000 interlocking basalt columns.
The formation is a result of an ancient volcanic eruption.
It is in County Antrim on the northeast coast of Northern Ireland.
It is a World Heritage Site by UNESCO.
It was named a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland.
In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom.
The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea.
Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides.
The tallest are about 12 metres (36 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
The Giant's Causeway is today owned and managed by the National Trust.
It is the most popular tourist attraction in Northern Ireland.
The Giant's Causeway and Fingal's Cave are part of the same volcanic eruption.
They were separated by the plate tectonics movements which happened when the supercontinent Pangaea broke up.
During the Palaeogene period, some 50 to 60 million years ago, Antrim was subject to intense volcanic activity.
Highly fluid molten basalt intruded through chalk beds to form a large scale lava plateau.
As the lava cooled rapidly, contraction occurred.
The size of the columns is mostly determined by the speed at which lava from a volcanic eruption cools.
The extensive fracture network produced the distinctive columns seen today.
The basalts were originally part of a great volcanic plateau called the Thulean Plateau which formed during the Paleogene period.
Parts of this plateau can be found in the Faroe Islands, Iceland, and Norway, as well as at Fingal's Cave.