“如果你熬到一个人喝茶,一个人散步,一个人旅行，一个人看书，没有电话，没有邀约，没有聚会，没有一些所谓的社交。早睡早起，善待自己,无欲无求,云淡风轻。不在乎别人评价,只要随心而活，知足常乐，顺其自然。那么恭喜你,你己达到人生最高境界。”
"If you stay up until you drink tea alone, walk alone, travel alone, read alone, no phone calls, no invitations, no parties, no some so-called socializing." Go to bed early, get up early, treat yourself, have no desires, the clouds are light and the wind is light. Don't care about other people's evaluation, as long as you live, content, let nature take its course. Then congratulations, you have reached the highest level of life."
"If you stay up until you drink tea alone, walk alone, travel alone, read alone, no phone calls, no invitations, no parties, no some so-called socializing." Go to bed early, get up early, treat yourself, have no desires, the clouds are light and the wind is light. Don't care about other people's evaluation, as long as you live, content, let nature take its course. Then congratulations, you have reached the highest level of life."
根据片治肯特遗址壁画还原的粟特国王形象 #Archaeology# #archaeohistories#
Late 7th - early 8th century #Sogdian# king based on wall paintings from #Panjakent# (Tajikistan).
Reconstructed with the advice of @eranudturan (the dagger and sword have been designed by Nadeem Ahmad based on the murals) https://t.cn/A6YdnfbJ
Late 7th - early 8th century #Sogdian# king based on wall paintings from #Panjakent# (Tajikistan).
Reconstructed with the advice of @eranudturan (the dagger and sword have been designed by Nadeem Ahmad based on the murals) https://t.cn/A6YdnfbJ
【珠穆朗玛峰的顶峰曾经被水淹没过吗？】
珠穆朗玛峰的山顶是由海洋石灰岩构成的，这意味着地球上的最高点曾经是在海底！
珠穆朗玛峰的山顶实际上是4.7亿年前的海底！ 没错，构成“顶峰金字塔”或珠穆朗玛峰最上部的岩石是灰色石灰岩，是在古生代奥陶纪早期到中期沉积在印度北部北部大陆架上的，早在印度开始北上之前 通往欧亚大陆的旅程以及最终导致喜马拉雅山和青藏高原抬升的构造板块的碰撞。 被地质学家称为“珠穆朗玛峰石灰岩”的山顶岩石是层理良好的石灰岩（粒岩），其中含有常见的奥陶纪海洋无脊椎动物贝壳的碎片，如三叶虫、腕足类、介形类和海百合等。 珠穆朗玛峰石灰岩经过热量、压力和流体的作用，改变了原来的石灰岩，所以现在它是一种低品位的变质岩。 印度和欧亚大陆的碰撞（至今仍在继续）、大喜马拉雅山的深度侵蚀以及沿藏南滑脱的断层位移导致这些岩石不断抬升，这些岩石已被带到了世界屋脊。 山顶岩石位于下面较高品位的变质岩之上。
【Was the summit of Mount Everest Ever Underwater?】
The summit of Mt. Everest is made of marine limestone which means the highest point on earth was once at the bottom of the sea！
The summit of Mount Everest was actually the seafloor 470 million years ago! That's right, the rock that comprises the "summit pyramid" or uppermost part of Mount Everest is gray limestone that was deposited on the northern continental shelf of northern India during the early to middle Ordovician Period of the Paleozoic Era, long before India began its northward journey towards Eurasia and the eventual collision of tectonic plates that uplifted the Himalaya and Tibetan Plateau. Called the "Qomolangma Limestone" by geologists, the summit rocks are well-bedded limestone (grainstone) with fragments of common Ordovician marine invertebrate shells, such as trilobites, brachiopods, ostracods and crinoids. The Qomolangma Limestone has been altered by heat, pressure and fluids that have altered the original limestone, so it is now a low-grade metamorphic rock. These rocks have been brought to the roof of the world through continual uplift caused by the collision of India and Eurasia (still on-going today), deep erosion of the Greater Himalaya, and fault displacement along the South Tibetan detachment that has tectonically placed the summit rocks over higher-grade metamorphic rocks below.
Read more: https://t.cn/A6YdWZxF#
珠穆朗玛峰的山顶是由海洋石灰岩构成的，这意味着地球上的最高点曾经是在海底！
珠穆朗玛峰的山顶实际上是4.7亿年前的海底！ 没错，构成“顶峰金字塔”或珠穆朗玛峰最上部的岩石是灰色石灰岩，是在古生代奥陶纪早期到中期沉积在印度北部北部大陆架上的，早在印度开始北上之前 通往欧亚大陆的旅程以及最终导致喜马拉雅山和青藏高原抬升的构造板块的碰撞。 被地质学家称为“珠穆朗玛峰石灰岩”的山顶岩石是层理良好的石灰岩（粒岩），其中含有常见的奥陶纪海洋无脊椎动物贝壳的碎片，如三叶虫、腕足类、介形类和海百合等。 珠穆朗玛峰石灰岩经过热量、压力和流体的作用，改变了原来的石灰岩，所以现在它是一种低品位的变质岩。 印度和欧亚大陆的碰撞（至今仍在继续）、大喜马拉雅山的深度侵蚀以及沿藏南滑脱的断层位移导致这些岩石不断抬升，这些岩石已被带到了世界屋脊。 山顶岩石位于下面较高品位的变质岩之上。
【Was the summit of Mount Everest Ever Underwater?】
The summit of Mt. Everest is made of marine limestone which means the highest point on earth was once at the bottom of the sea！
The summit of Mount Everest was actually the seafloor 470 million years ago! That's right, the rock that comprises the "summit pyramid" or uppermost part of Mount Everest is gray limestone that was deposited on the northern continental shelf of northern India during the early to middle Ordovician Period of the Paleozoic Era, long before India began its northward journey towards Eurasia and the eventual collision of tectonic plates that uplifted the Himalaya and Tibetan Plateau. Called the "Qomolangma Limestone" by geologists, the summit rocks are well-bedded limestone (grainstone) with fragments of common Ordovician marine invertebrate shells, such as trilobites, brachiopods, ostracods and crinoids. The Qomolangma Limestone has been altered by heat, pressure and fluids that have altered the original limestone, so it is now a low-grade metamorphic rock. These rocks have been brought to the roof of the world through continual uplift caused by the collision of India and Eurasia (still on-going today), deep erosion of the Greater Himalaya, and fault displacement along the South Tibetan detachment that has tectonically placed the summit rocks over higher-grade metamorphic rocks below.
Read more: https://t.cn/A6YdWZxF#
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