Discover Top Posts Tagged with #plate movement

沈恩綺 @台灣7Crash 品牌創始人

今年榮幸受邀參加『2016 Fashion In Taipei臺北好時尚』在台北魅力展中的設計師品牌聯合動態秀，此次秀場舉辦在台北松菸四號倉庫，由於我們的品牌7CRASH剛參加完上海時裝周及北京的中國國際時裝週展會，因此今年觀摩許多才華洋溢的海內外設計師作品，發現台灣設計一直有著多元層次融合的魅力，也似乎相呼應於今年「武動時尚」的主題，歷史複雜的紋理交織傳承於今，而藉由設計的力量，設計師用自己的方式訴說著文化傳承亦或是嶄新的一面。

今年大賞金獎得主田明彬（MING STUDIO）的作品，透過不同材質輪廓組合、拼貼，創造和諧與矛盾並存而的獨特美感，服裝輔料上運用如繫帶、金屬環等將時裝元素融合街頭運動風，也是近幾年設計師特別喜愛在秀場運用的元素。

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XIWI-設計師張洊瑋

過長的袖子、OVERSIZE的著裝，針織梭織面料的互相匹配，今年在潮流圈吹起一陣炫風！具有獨特中性魅力的設計作品，在看似複雜的細節與搭配中呈現最有態度的年輕風範。

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within #nude – 設計師黃紀堯

#nude本身已經是一個非常純熟的品牌，平時也積極參與各大時裝展會，極簡素雅的清新風格已經有一群喜愛#nude的追隨者，雖然是極簡的風範但在面料上的選用也特別的細心，非常具有市場的潛力。本次特別與黃紀堯設計師合作推出系列作品，期待#nude接下來與更多台灣設計師合作激發出更多創意火花！

Plate Movement – 設計師李昱昌

透過服裝在版型、圖騰、印花等表現技法，將文化融合表現於服裝上，特殊的大面積立體刺繡相當有視覺效果，強調「愛是平等的，無論何種身份」的主題發想也讓人印象深刻。

BOB Jian – 設計師簡國彥

主題「彩虹」採用單套單色系的方式展示，以俐落的服裝結構詮釋每種顏色在設計師心裡的形象，從簡國修的系列裡我看見柔軟卻又帶有堅毅性個的女性魅力。

設計師與模特合照

精彩的大秀結束後來跟大家分享當天的秀場秀外的潮人穿搭！

帥氣女孩一身黑色穿搭

適當利用配件單品如寬腰帶展現女性魅力

(左圖1) 這位帥氣女孩一身黑色穿搭，透過不同廓形與材質創造層次感，也更加凸顯其白金色的個性髮色。

(右圖1) 同樣是全身黑色系，適當利用配件單品如寬腰帶、頸鍊等搭配紅唇，也能展現黑色獨有的女性魅力，特別的是混搭充滿民俗風的肩背包，讓整體又增添一點神秘異國風情。

簡單俐落的黑白灰和現在最流行的oversize韓系穿搭，最好的呈現方式就是靠完美的身材比例！

日系復古風完美展現其清新的氣質，恰到好處的配件和色彩搭配，展現輕鬆不經意又讓人忍不住回過頭的穿搭技巧。

在時尚圈掀起一陣潮流的KENZO X H&M系列單穿就已經充滿潮範。

黑白波點的搭配是經典中的經典。

李昱昌設計師，設計師本身就是最好的model展示！

歌手隋玲的私著以一襲黑色連身褲搭配綠色襯衫讓膚色更顯白皙。

已經舉辦四屆的Fashion In Taipei臺北好時尚，是個很好的平台讓台灣的新銳設計師有舞台能夠展現作品，更進一步到國際市場發展。身為台灣設計師，期望將來台灣除了設計大賞也能夠有自己的時裝周，以及其配套的商業平台。當來自全球的買手們逐漸將主辦的時裝周作為一年兩季常規的採購據點，那麼年輕的設計師品牌勢必能獲得更多被看見與發光發熱的機會。西方時裝界發展了這麼多年後，時代的風向標已經越來越偏向崛起的東方，然而我們原創設計師應該做的，不是追隨舊世界的腳步，也不用急於跟進市場的各類潮流，而是要看清楚自己最本質的優勢，然後做強做大。能夠在百家爭鳴的品牌競爭中找到自己市場的，必定是那些走出模仿怪圈，找到自己語言的設計。期待台灣更多優秀的設計師一起在國際上發光發熱！

文/沈恩綺責任編輯/Coco

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2016 Fashion in Taipei臺北好時尚 : 從台灣武動設計看見世界沈恩綺 @台灣7Crash 品牌創始人今年榮幸受邀參加『2016 Fashion In Taipei臺北好時尚』在台北魅力展中的設計師品牌聯合動態秀，此次秀場舉辦在台北松菸四號倉庫，由於我們的品牌7CRASH剛參加完上海時裝周及北京的中國國際時裝週展會，因此今年觀摩許多才華洋溢的海內外設計師作品，發現台灣設計一直有著多元層次融合的魅力，也似乎相呼應於今年「武動時尚」的主題，歷史複雜的紋理交織傳承於今，而藉由設計的力量，設計師用自己的方式訴說著文化傳承亦或是嶄新的一面。

#BOB Jian #Plate Movement #within nude #台北魅力展 #張洊瑋XIWI #李昱昌 #武動設計 #田明彬 MING STUDIO #簡國彥 #黃紀堯

Plate tectonics

#pangaea #earth #plate movement #tectonics #TED-ed #youtube knowledge

Hotspots - Yellowstone

Yellowstone is another example of volcanic activity created by a hotspot underneath a moving plate, but unlike the Hawaiian hotspot the Yellowstone hot spot is underneath continental crust, and has created a series of supervolcano calderas.

#plate movement #hotspots #yellowstone #caldera

1. Plate Movement - Hotspots

(I really don't know why Hotspots are under Plate movement in the specification, and not under Vulcanicity.)

Vulcanicity is usually associated with plate margins, but there are a few anomalous places of volcanic activity which are no where near a plate boundary.

It is believed that a Plume of magma within the mantle that is hotter than the surrounding magma rises and burns through the plate above it like a blow torch. Where lava breaks through to the surface, volcanoes occur over the hotspot.

Probably the most famous example is the Hawaiian islands, which are part of a chain of islands and seamounts extending some 1,500 miles across the Pacific ocean.

The Hawaiian archipelago is believed to have been (and is being) created by a localised hot spot in the Pacific plate. the hot spot is stationary, so as the pacific plate moves over it a chain of volcanoes form. Once an island is moved by the pacific plate so that it is no longer over the hot spot, the volcanoes' lava source is cut off and the volcanoes become extinct.

Currently, the islands of Maui and Hawaii have active volcanoes, and there is another underwater volcano SE of Hawaii that will eventually form a new island.

The ages of the Hawaiian islands also corresponds with their proximity to the hotspot, clearly showin that the pacific plate is movingin a NW direction approximately 10cm/year. This also adds support to Wegener's theory.

The hawaiian Volcanoes are the typical Shield type volcanoes, with very runny/ non viscous basaltic lava (due to low sillica content) and eruptions are effusive (gentle/non explosive lava eruptions) and frequent.

Mauna Loa is one of the five volcanoes that make up Hawaii, and is the largest volcano on earth in terms of volume.

(It's neighbour Mauna Kea, if measured from the base of the volcano on the seabed to it's peak is the tallest mountain on Earth at 10,200m, dwarfing Mt. Everest's 8,848m elevation from seabed to peak)

#Plate movement #hotspots #hawaii #mauna loa #mauna kea #effusive eruptions #wegener's theory

1. Plate Movement - Convergent margins (pt.2) - collision

Collision plate boundaries occur where two plates of continental crust converge.

Since the plates forming continental crust have a much lower density than the underlying layers of lithosphere, there is not much subduction where they converge. Instead, the edges of the plates and the sediments on top are forced to fold and buckle to form Fold Mountains as the plates converge.

^this picture really clearly shows folded and deformed rock sediments!

Vulcanicity Is not commonly found at collision margins, as not much subduction occurs.

Seismicity Is frequent and capable of producing large magnitude earthquakes due to the friction build up and land mass settling as the plates collide.

Example:

The Himalayas are an example of fold mountains that are still growing, where the Indian plate is colliding with the Eurasian plate.

The Himalayas are currently the tallest mountain chain on earth, but eventually erosion may reduce the himalayas to the height of the Alps and other, older mountain chains that are relics of past tectonic activity.

#plate movement #plate boundaries #convergent boundaries #collision boundaries #fold mountains

1. Plate Movement - Constructive margins

Also called Divergent margins.

Occur where two plates are diverging (moving apart). the space between the diverging plates is filled with basaltic lava upwelling from below. New crust is constantly being created at constrictive margins, and are therefore some of the youngest parts of the earth's surface.

Features:

Mid-oceanic ridges are created when a constrictive boundary occurs in an oceanic area - for example the mid-Atlantic ridge

Rift valleys are created when a constructive boundary occurs in continental crust - for example the East African rift valley, and the rift valley visible at Thingvellir national park, Iceland