OpenLLM-France/wikimedia huggingface dataset:
# Wii Sports

Wii Sports is a collection of simplified sports games that employs the Wii Remote to mimic an action in real life, such as swinging a golf club. The sports available in the Wii Sports package include baseball, tennis, bowling, boxing, and golf.
As you play the different sports, you will be awarded Skill Points which add or subtract from your cumulative Skill Level. Once you reach 1000 Skill points, you will receive a special tag that says "Pro".
Information in this book is currently quite sparse, but you're invited to add more details and gameplay tips!

## Table of Contents

* Tennis
* Baseball
* Golf
* Boxing
* Bowling
* Training
# The Geology of Indonesia/Preface

Indonesia is the largest archipelagic state in the world comprising five major islands and about 300 smaller island groups. Altogether there are 13,667 islands and islets of which about 6,000 inhabited. The archipelago is situated on a crossroad between two oceans, the Pacific and Indian oceans, and bridges two continents, the Asian and Australian. Indonesia has a total area of 9,8 million sq km, of which more than 7,9 million sq km are under water. Physiographically, the islands of Sumatra, Java and Kalimantan are attached to the Sunda Shelf of the Asian continent. On this landmass the water depth does not exceed 200 meters. To the east, Irian Jaya and the Aru islands lie on the Sahul Shelf, which are parts of the Australian continent. Located between these two shelves is the island group of Nusa Tenggara, Sulawesi, Maluku and Halmahera. These islands are encircled by deep seas which in many places reach 5,000 meters.
About 60 Tertiary sedimentary basins, spread out from Sumatra in the west to Irian Jaya in the east, are identified in Indonesia. So far only 38 basins have been explored and drilled for petroleum and 14 of the are now producing oil and gas. Seventy three percent of these basins are located offshore, about one third of them in the deeper sea, with water depth exceeding 200 m.
Background
In 1949, R. W van Bemmelen published a compilation of reports and data on the Geology of Indonesia. The book was reprinted in 1970 with no additional data. This book has documented a lot of data and geological understanding before the second world war and only covered onshore geology of Indonesia. W. Hamilton published a book titled Tectonics of the Indonesian Region in 1979 which include offshore seismic data and remote sensing. The Indonesian geologist celebrated the 50th anniversary of R. W. van Bemmelen's book in a conference titled "Tectonics and Sedimentation of Indonesian" in 1999 and published "An Outline of the Geology of Indonesia" the following year (2000). The data and the knowledge on the geology of Indonesia are so much and make it so difficult to compile them in a single book. In 2007 the Wikibook of the Geology of Indonesia was started by converting Än Outline of the Geoloyg of Indonesia"to a digital version. The idea is to include as many geoscientists as possible to keep the information on the geology of Indonesia as good as possible. This online version of the Geology of Indonesia will also give a chance to renew or update the information stored at anytime.
# The Geology of Indonesia/Plate Tectonic

Indonesia is a meeting point of several tectonic plates. Indo-Australian Plate is moving northward, Eurasia Plate moves southeast direction. Both Filipino and Pacific plate move westward. The Indo-Australian plate was moved northward and partly subducted under the Eurasian plate. The subduction zone can be traced from northern tip of Sumatra until the Lesser Islands, that creates deep submarine trench. Most of the earthquake also concentrate in this subduction zone. This subduction also triggers the formation of volcanic range from Sumatra, Java to Lesser Islands.
The center part of Indonesia also experienced another subduction of Pacific plate that move southwesterly under the Eurasian plate. This subduction create the formation of volcanoes in the North Sulawesi, Sangihe and Halmahera.
The Australian and Pacific plate collides in the eastern part of Indonesia and formed the mountain range in central Papua, with Puncak Jaya / Carstenz Pyramide as the highest peak.
Below is a regional cross section of Indonesia from west to east showing the relationship of the tectonic components of Indonesia, their depth, and structural features.
# The Geology of Indonesia/Sedimentary Basins
## Introduction

The basic premise to explore the petroleum is the existence of sedimentary basin. Sedimentary basin is a depression on the earth surface the can accumulated the sedimentation material through time. Since most of the sediment transporting agent are water, the sedimentary basin usually the place where the water finally accumulate. It can be in the form of sea, lake, delta, or river.
Indonesia is a large country with various type of sedimentary basins. Most of the sedimentary basin in the western Indonesia are already explored since the end of 19th century. The recent years also saws the exploration on the frontier basins, especially in the eastern Indonesia. Unfortunately, the interest of the major oil companies lost their appetite to conduct explorational activities in Indonesia probably due to the unfavorable fiscal regime. As a result, the oil and gas production is keep declining in Indonesia without any substantial reserve replacement.
The sediment which comprise of clay, sand, boulder or carbonate are being deposited in the sedimentary basin over a geologic time (million years). Due to the weight of the sedimentary deposit, the sedimentary basin experience subsidence to allow more sedimentation. This sedimentary process may accumulate sediment with cumulative thickness of several thousand meters.

## Characteristics

About 60 Tertiary sedimentary basins, spread out from Sumatra in the west to Irian Jaya in the east, are identified in Indonesia. So far only 38 basins have been explored and drilled for petroleum and 14 of the are now producing oil and gas. Seventy three percent of these basins are located offshore, about one third of them in the deeper sea, with water depth exceeding 200 m.

## Back-arc Basin

The most prolific sedimentary basin in Indonesia are belong to back-arc basin, whichis located on the 'back' of the volcanic-arc. Most of the back-arc basin located in the northeastern coast of Sumatra, northern Java, and continue to northern Lesser Island. Almost all of the back-arc basin are currently producing oil and gas, therefore categorized as proven petroleum province.

## Fore-arc Basin

The fore-arc basin located to the 'front' of the volcanic arc, which is located along southwestern coast of Sumatra, southern coast of Java and Lesser Island. The fore-arc basin is mainly considered as a frontier basin and no commercial hydrocarbon found yet. However, there is strong indication of working petroleum system in the fore-arc basin, such as gas discoveries in the Nias area. Oil shows also reported to be found in offshore Bengkulu (Southern Sumatra). On the interesting note, the fore-arc basin in the southern part of Papua New Guinea already found commercial gas accummulation in the Pandorra Gas Field.
# The Geology of Indonesia/Petroleum Issues
## Fiscal Regime

Fiscal regime for the petroleum exploration in Indonesia is considered un-competitive compared to other countries. It reflected on the minimal interest from the major oil companies to invest their money for the petroleum exploration activities in Indonesia.

## Technical Brain Drain

The problem on the petroleum industry in Indonesia is the technical brain drain. Large proportion of the highly skilled technical people with good experience in the oil industry are left to working overseas to gain international experience and higher salary. It is not a secret that oil industry in Indonesia is unfairly renumerate their workers. The renumeration for expatriate personnel is about 5-10 times higher than the local employee with similar technical skills and level of experiences.
# The Geology of Indonesia/Stratigraphy/Introduction

The stratigraphical knowledge of the Indonesian Archipelago will be summarized in this chapter. A synopsis of the stratigraphy of the Netherlands East Indies has been published by BROUWER (1925) and L. M. R. RUTTEN (1927). In 1938 UMBGROVE gave a comprehensive review of the geological history of the East Indies. A number of important contributions to the stratigraphy which appeared in 1937-1938, not available to UMBGROVE, were summarized by SMIT SIBINGA (1940). L. M. R. RUTTEN (1948) and DE BEAUFORT (1948) reviewed the paleontological work carried out in the Netherlands for the Dutch Overseas Territories during the period 1918-1943.
Other important reviews on the stratigraphy of the Indian Archipelago are to be found in: The "MARTIN-Volume" of the "Leidsche Geologische Mededeelingen" (1931), in which a number of authors gives a review of the paleontological and stratigraphical data up to the year 1930; UMBGROVE (1934 b) on theNeogene, and(1935)on thePre-Tertiary; BADINGS (1936) on the Paleogene; STAUFFER (1945) on the stratigraphy of Indonesia; SMITH (1924, 1925) on the stratigraphy of the Philippines; MONTGOMERY, OSBORN and GLAESSNER on the stratigraphy of Eastern New Guinea 1); CHHIBBER (1934) on the stratigraphy of the Andamans and Nicobars.
In 1950, P. Marks, published Stratigraphic Lexicon of Indonesia, which is a compilation of formation names in Indonesia. The formation names are sorted in alphabetical order with their description, rough map of the localities, and summarized them in stratigraphic charts.
The first Indonesian Stratigraphic Nomenclature guide (Sandi Stratigraphy Indonesia) was published in 1973 by Soejono Martodjojo and Djuhaeni. This book was updated in 1996 and published electronically by the Indonesian Geologist Association. The file is available online in SSI-1996. Many publications related to sequence stratigraphy and seismic stratigraphy in Indonesia were published by the Indonesian Petroleum Assocation (IPA), the Indonesian Geological Association (IAGI)and other professional organizations. A compilation of updated article on biostratigraphy of SE Asia is currently being prepared by the Indonesian Sedimentologists Forum (FOSI), which aim to issue it in 2014. Another key source on the stratigraphy of Indonesia is the Geological Research and Development Centre of Indonesia (GRDC)
For the sake of brevity, in this chapter only some notes will be given on recent advances in our knowledge of the pre-tertiary stratigraphy. For the rest the reader is referred to the regional descriptions.
The tertiary and quaternary formations have a much wider distribution than the pre-tertiary rocks. Their stratigraphy is most important in the unraveling of the evolution of the younger mountain systems in this area. Therefore, the stratigraphy of the Tertiary and the Quaternary will be treated at some length in this chapter.
# Walking Rugby/History

Walking Rugby (WR) was started at Reading RFC in late October 2015, in response to enquiries locally to the rugby club regarding the possibility of a game similar to Walking Football which seems to have taken off nationally with some success.
Reading WR started with a group of about 8 to 12 people, initially at the Reading Rugby Club on grass, but soon moved indoors to a local sports hall. The group consisted mainly of retired members of the Rugby Club plus others with the flexibility to manage their own working hours. The version of the game that was started was very soon modified, adapted, and has evolved into the current version which we have tried to make identifiably a version of the game of Rugby Football Union.

## References

* ↑ https://www.rugbytoolbox.co.nz/the-game/other-rugby-formats/walking-rugby
# Wampanoag/Clothing

|Paúskesu.| `Naked.' |Pauskesìtchick| `Naked men and women.' |Nippóskiss.| `I am naked.'
They have a two-fold nakednesse:
First ordinary and constant, when although they have a Beasts skin, or an English mantle on, yet that covers ordinarily but their hinder parts and all the foreparts from top to toe, (excep their secret parts, covered with a little Apron, after the patterne of their and our first Parents) I say all else open and naked.
Their male children goe starke naked, and have no Apron untill they come to ten or twelve yeeres of age; their Female they, in a modest blush cover with a little Apron of an hand breadth from their very birth.
Their second nakednesse is when their men often abroad, and both men and women within doores, leave off their beasts skin, or English cloth and so (excepting their little Apron) are wholly naked; yet but few of the women but will keepe their skin or cloth (though
loose) <111/r.119> <Of {their nakedn[.]sse} and {clothing}.>
# WP:AWB/T

Wikipedia:AutoWikiBrowser/Typos This page is a soft redirect.
# Walking Rugby

Walking Rugby is a much gentler version of the physically demanding game of Rugby. It is played on half of a normal pitch, participants must be walking at all times, and there is no tackling involved, instead a touch of two hands below the armpit or above the waist is used.
In some ways, it can be seen as similar in concept to Walking football or Walking netball where for whatever reason people cannot play the normal high-speed full-contact version of the game they are based on, in this case Rugby union
It is a good cardiovascular workout and can also help to improve speed, agility, and strength. Plus, it’s an opportunity to meet new people without the risk of getting tackled to the floor, if you don't what to play the outdoors, walking sports like this can be played inside all year round

## Contents

* Introduction
* Rules
* Guidelines

## References

* ↑ https://www.justgetactive.co.uk/get-involved/walking-sports/walking-touch-rugby/
* 1 2 https://www.englandrugby.com/participation/playing/ways-to-play/walking-rugby
# Wampanoag/Blood and marriage

|Nnín-nnìnnuog, `Man_men' {&} |keétomp-aúog| |Squàws-suck.| `Woman-women.' |Kichize,| {&} `An old man,' |Kichîzuck| `Old men.' |Hômes,| {&} `An old man,' |Hômesuck| `Old men.' |Kutchìnnu| `A middle-aged-man.' |Kutchìnnuwock.| `Middle-aged-men.' |Wuskeène| `A youth,' |Wuskeeneésuck.| `Youths.' |Wénise| {&} `An old woman,' |Wenîsuck| `Old women.' |Mattaúntum| `Very old and decrepit.'
Wásick <28> < Of {their} relations {of} consanguinity. >
|Wâsick| `An Husband.' |Weéwo,| {&} `A Wife.' |Mittúmmus,| {&} |Wullógana| |Nowée o,| `My Wife.' |Nummittamus,| {&c.} |Osh.| `A Father.' |Nosh| `My father.' |Còsh| `Your father.' |Cuttòso?| `Have you a father?' |Okásu,| {&} `A mother.' |Wìtchwhaw| |Nókace|, |nìtchwhaw| `My mother.' |Wússese| `An Unckle.' |Nissesè| `My Unckle.' |Papoòs,| `A childe.' |Nippápoos,| {&} `My childe.' |Nummúckiese| |Nummúckquáchucks| `My sonne.' |Nittaúnis| `My daughter.' |Nonânese| `A sucking child.' |Muckquachuckquêmese|- `A little boy.' |Squ sese| `A little girle.' |Weémat.| `A brother.'
They hold the band of brother-hood so deare, that when one had committed a murther and fled, they executed his brother; and <29> <Of {their} relations.> `tis common for a brother to pay the debt of a brother deceased.
|Neémat| `My brother.' |Wéticks,| {&} `A sister.' |Weésummis| |Wematìttuock| `They are brothers.' |Cutchashematìtin?| `How many brothers have you?' |Natòncks| `My cousin.' |Kattòncks| `Your cousin.' |Watòncks| `A cousin.' |Nullóquaso| `My ward or pupill.' |Wattonksìttuock| `They are cousins.' |Kìhtuckquaw| `A virgin marriageable.'
Their Virgins are distinguished by a bashfull falling downe of their haire over their eyes.
|Towiúwock| `orphan.'
There are no beggars amongst them, nor orphans unprovided for.
|Tackqìuwock| `Twins.'
Their {affections}, especially to their children, are very strong; so that I have knowne a {Father} take so grievously the losse of his {childe}, that hee hath cut and stabd himselfe with {griefe} and {rage}.
This extreme {affection}, together with want of {learning}, makes their children sawcie, bold, and undutifull.
# Trainz: A Comprehensive Guide
### A Brief Overview of Trainz
## Driver Mode in Trainz

Explore the Driver mode in Trainz, where you can operate virtual trains on various routes.

## Surveyor Mode in Trainz

Surveyor mode allows you to create and customize virtual railroads.

## Asset Management in Trainz

Learn how to effectively manage your Trainz assets, a crucial aspect as your collection grows.
    Main Asset Management TOC: Trainz/AM&C
Explore detailed asset management topics including downloading, organizing, and fixing assets.

## Creating Assets in Trainz

Delve into the creative side of Trainz by learning how to develop your own assets.
* Upcoming reorganization into multiple divisions...
* Soon, in-depth content on intermediate and advanced Trainz topics will be available in the new division: Trainz Asset Management & Creation. Other materials will be moved to references, and older content will be kept in the Appendices.
Discover the rewarding process of creating content for Trainz, using tools like 3D modeling software.

## Scripting in Trainz

Scripting adds flexibility and interactivity to Trainz assets, using the TrainzScript language.

## Navigation and Categories

← Overview of Trainz releases · Introduction →
# 3DS Max Keyboard Shortcuts

Back to the Top
* Trainz Content Creation—Intermediate to Advanced Topics
* TOC | Beginnings | Fun | AM&C | Creation | InBook Refs | ORP Refs:  • Index • Containers • Kinds • Tags | Appendixes  • Vers
Glossary :
HKeys-CM :
HKeys-DVR :
HKeys-SUR :
HKeys-WIN :
Mouse use :
Notations :
    This page renamed from: Hints and Tips for 3D Modelling Software
* Editor's note: Getting to know the keyboard shortcuts in any program can speed up your efficiency and productivity. 3DS Max is no exception.
* Many of the following will apply to GMAX too.
| Hot Key | Effect or action |
| F1 | Opens 3DS Max Help |
| F2 | Shade Selected Faces (on/off) |
| F3 | Toggle Between Wireframe and Smooth + Highlights |
| F4 | View Edged Faces |
| F9 | Render Particular Viewport |
| F10 | Render Scene Dialogue |
| E | Select and Rotate Tool |
| H | Select by Name Dialogue |
| J | Selection Brackets (on/off) |
| Q | Select Tool |
| R | Select and Scale Tool |
| W | Select and Move Tool |
| B | Switch to the Bottom viewport |
| C | Switch to a Camera viewport |
| F | Switch to the Front viewport |
| L | Switch to the Left viewport |
| P | Switch to the Perspective viewport |
| R | Switch to the Right viewport |
| T | Switch to the Top viewport |
| D | Disable Viewport |
| G | Main Grid (onn/off) |
| V | Open View Shortcut Menu |
| M | Material Editor Dialogue |
| O | Adaptive Degradation (on/off) |
| X | Transform Gizmo (on/off) |
| Z | Zooms in on the Current Selection |
| CTRL+A | Select All |
| CTRL+D | Deselect all |
| CTRL+C | Create Camera From Current Viewport |
| CTRL+V | Clone Object |
| CTRL+X | Expert Mode (on/off) |
| ALT+C | Cut |
| ALT+L | Select Edge Loop |
| ALT+Q | Hide Unselected Objects |
| ALT+X | Display As See-Through (on/off) |
| ⇧ Shift+E | Extrude Polygon |
| ⇧ Shift+Q | Quick Render Selected Viewport |
| ⇧ Shift+Y | Redo Last Viewport Operation |
| ⇧ Shift+Z | Undo Last Viewport Operation |
| SPACE | Selection Lock (on/off) |
| 1 | Vertex Sub-Object Level |
| 2 | Edge Sub-Object Level |
| 3 | Border Sub-Object Level |
| 4 | Polygon Sub-Object Level |
| 5 | Element Sub-Object Level |
| 7 | Polygon Counter (on/off) |
| 8 | Environment and Effects Dialog |
| + | Increase Gizmo Size |
| - | Decrease Gizmo Size |
There are also many more. The hotkeys are customizable under the 'Customize User Interface' menu option.
Back to the Top
# Wu Chinese/Lesson 1

Here are a few greetings and phrases in the Wu language, specifically the Shanghai dialect, that may be of use to you.
侬好 (nóng hō) - Hello
大家好 (dâka hō) - Hello everyone
侬好伐 (nóng hō va) or 侬过得还好伐 (nóng kûle e-hô va?) - How are you?
我蛮好，谢谢 (wú mehō, yáyà) - I'm ok
蛮好。侬呢？ (mehō. nóng nak) - I'm pretty good. What about you?
我蛮好, 侬 (wú mehō, nóng) - I'm good.
请问尊姓大名？(chînmen tzenxin-dâmin) or 请问侬信啥？(chînmen nóng xin sa?) - What is your name?
# Wu Chinese/Pronunciation
## Wu sounds
### Syllables

The number of syllables in the Wu language are much less than English. The syllables are also easily described with the concepts of initials and finals. A syllable begins with a single consonant. This is called the initial. The rest of the syllable is called the final. A final can have a single vowel or a diphthong (two vowels that glide from one to the other).
The pronunciation guide below is based on American English except where otherwise noted. Not all sounds can be described with English words and some are just approximations at best. Be sure to listen to actual speakers to ensure that your pronunciation is correct.

### Initials

| Ghou'nyu Phin'in | Pronunciation |
| t | t in "stop" |
| th | t as in "top" |
| d | d as in "dog" |
| n | n as in "no" |
| l | l in "let" |
| p | p as in "spa" |
| ph | p as in "pop" |
| b | b as in "bad" |
| f | f in "fat" |
| v | v as in "very" |
| m | m as in "mom" |
| ts | No equivalent in English. s as in "beds", but a lot lighter and clearer. |
| tsh | ts as in "cats" |
| dz | ds as in "beds" |
| s | s as in "sun" |
| z | z as in "zero" |
| c | No equivalent in English. j as in "BeiJing" in Mandarin. |
| ch | ch as in "chocolate" |
| j | j as in "jack" |
| sh | sh as in "shack" |
| zh | s as in "usual" |
| ny | ni as in "onion" |
| k | ch as in "school" |
| kh | c as in "cat" |
| g | g as in "good" |
| h | h as in "good" |
| gh | No equivalent in English or Mandarin. It's a more pronounced "h". |
| ng | ng as in "singer", as if the "ng" sound is carried onto the "er" instead of being cut off before the "er". |
# X-COM: Apocalypse Strategy Guide/OpenApoc
## What is OpenApoc

OpenApoc is a reimplementation of the X-COM: Apocalypse game engine which offers a number of improvements. Most importantly, this engine offers support for contemporary operating systems. This engines does not ship with game assets, so an official game disk is still required to use this engine.
# X-COM: Apocalypse Strategy Guide/Equipment
## Initial Equipment
### Personnel Weapons
#### Megapol LawPistol

Quite decent in the first week, after that it's obsolete and should be avoided. As a single-handed weapon, it allows the use of a second item (grenade, medikit, a second gun) in the other hand without lowering accuracy.

#### Megapol Plasma Gun

Much better than it's predecessor. This gun never really becomes obsolete but it's not really not that effective. As a single-handed weapon, it allows the use of a second item (grenade, medikit, a second gun) in the other hand without lowering accuracy.

#### Marsec M4000 Machine Gun

The same thing can be said about this weapon as about the basic pistol, except on the higher difficulties where it's obsolete before the game starts.

#### Megapol Laser Sniper Gun

An excellent long range weapon. While it's damage capabilities leaves a lot of room for improvement just remember that if you miss damage will be exactly 0, so hitting is better than missing. While using this gun agents will progress relatively rapidly in their accuracy skills, making it a good weapon for training.