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[ | |
{ | |
"number": 1, | |
"kanji": "北海道", | |
"kana": "ほっかいどう", | |
"roman": "hokkaido" | |
}, | |
{ | |
"number": 2, | |
"kanji": "青森県", |
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{ | |
"0": { | |
"id": 0, | |
"key": [ | |
"", | |
"" | |
], | |
"code": "" | |
}, | |
"1": { |
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class Sounder{ | |
constructor(url){ | |
this.url=url; | |
} | |
make(){ | |
return new (class{ | |
constructor(url){ | |
this.elem=document.createElement("audio"); | |
this.elem.src=url; | |
} |
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{ | |
"h1": 26, | |
"h2": 19, | |
"h3": 15, | |
"h4": 13, | |
"h5": 10, | |
"h6": 8 | |
} |
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{ | |
"title": "理科", | |
"data": [ | |
{ | |
"type": "text", | |
"src": ".use md\n# 力の世界\n- 力を加えると、物体の((形))を変えることができる。\n- 力を加えると、物体を((支え))たり、((持っ))たりすることができる。\n- 力を加えると、物体の((運動))の様子を変えることができる。\n- 100gの物体に働く重力の大きさは、地球上では約1((N))[読み:((ニュートン))]。\n- 物体に働くいくつかの力を一つにまとめることを、((力の合成))という。\n- それにより、まとめた力のことを、((合力))という。\n- 1つの力をいくつかの力に分けることを、((力の分解))という。\n- 分解した力のことを、((分力))という。\n# 地震\n- 観測地点の揺れの大きさのことを、((震度))という。\n- 地震そのもののエネルギーの大きさを、((マグニチュード))という。\n- たて波のことを、((P波))といい(α)、よこ波のことを、((S波))という(β)。\n- ((たて波))の方が早く進む。\n- αによる揺れのことを、((初期微動))といい、βによる揺れのことを、((主要動))という。\n- αによる揺れが始まってからβによる揺れが始まるまでの時間を、((初期微動継続時間))という。\n# 火山\n| 情報 | 出っぱっている火山 | 層になっている火山 | 平らな火山 |\n| ---- | ---- | ---- | ---- |\n| 名前 | ((鐘状火山)) | ((成層火山)) | ((たて状火山)) |\n| 粘り気 | ((強い)) | ((ふつう)) | ((よわい)) |\n| 噴火の勢い | ((激しい)) | ((ふつう)) | ((ゆるやか)) |\n| 色 | ((白っぽい)) | ((←中間→)) | ((黒っぽい)) |\n| 温度 | ((低い)) | ((ふつう)) | ((高い)) |\n- 火山の形は、((溶岩の性質))によって決まる。\n- プレートとの摩擦で溶けたものを、((マグマ))といい、高温である。それが地上に出たものを、((溶岩))と呼ぶ。\n- ((マグマ))の熱でその周辺の((水))などが蒸発し、そのエネルギーで((岩石))を吹き飛ばし、((噴火) |
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{ | |
"title": "Xearfiy Notebookのヘルプ", | |
"data": [ | |
{ | |
"type": "img", | |
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