These ripples are preserved in this sandstone rock and are now lining a dry creek bed in Australian outback. But, it was around 2 billion years ago when motion of water formed these sand ripples on the bottom of a shallow sea. Note that orientation of ripples is different between sedimentary layers which indicates changes to water current direction.
Everest Range, 𝗡𝗲𝗽𝗮𝗹 and 𝗧𝗶𝗯𝗲𝘁, 𝗖𝗵𝗶𝗻a
27°59'17"N / 086°55'30"E
𝙂𝙚𝙤𝙡𝙤𝙜𝙞𝙘𝙖𝙡 𝙋𝙚𝙧𝙞𝙤𝙙:
Middle 𝗢𝗿𝗱𝗼𝘃𝗶𝗰𝗶𝗮𝗻 (𝗗𝗮𝗿𝗿𝗶𝘄𝗶𝗹𝗶𝗮𝗻)
𝘿𝙚𝙨𝙘𝙧𝙞𝙥𝙩𝙞𝙤𝙣:
Mount Everest is 𝗘𝗮𝗿𝘁𝗵'𝘀 𝗵𝗶𝗴𝗵𝗲𝘀𝘁 𝗺𝗼𝘂𝗻𝘁𝗮𝗶𝗻 above sea level, located in the Mahalangur Himal sub-range of the Himalayas. The China–Nepal border runs across its summit point. Its elevation of 𝟴,𝟴𝟰𝟴.𝟴𝟲 𝗺 was most recently established in 2020 by the Chinese and Nepali authorities.
𝗚𝗲𝗼𝗹𝗼𝗴𝗶𝗰𝗮𝗹 𝗗𝗲𝘀𝗰𝗿𝗶𝗽𝘁𝗶𝗼𝗻:
The 𝘀𝘂𝗺𝗺𝗶𝘁 of Mount Everest, the 𝗵𝗶𝗴𝗵𝗲𝘀𝘁 𝗽𝗼𝗶𝗻𝘁 on Earth, was a 𝘀𝗲𝗮 𝗳𝗹𝗼𝗼𝗿 once. 𝗜𝘀𝗻'𝘁 𝘄𝗼𝗻𝗱𝗲𝗿𝗳𝘂𝗹?. The highest rock on Earth, marking the summit of Mount Everest, are 𝗢𝗿𝗱𝗼𝘃𝗶𝗰𝗶𝗮𝗻 𝗟𝗶𝗺𝗲𝘀𝘁𝗼𝗻𝗲𝘀, deposited in a warm, shallow water sea some 𝟰𝟱𝟬 𝗠𝗮 𝗮𝗴𝗼.
These rocks deposited in an 𝗮𝗻𝗰𝗶𝗲𝗻𝘁 𝗧𝗲𝘁𝗵𝘆𝗮𝗻 𝗢𝗰𝗲𝗮𝗻 were thrust and 𝘂𝗽𝗹𝗶𝗳𝘁𝗲𝗱 into their present commanding position when 𝗜𝗻𝗱𝗶𝗮𝗻 𝗽𝗹𝗮𝘁𝗲 𝗰𝗼𝗹𝗹𝗶𝗱𝗲𝗱 with the 𝗔𝘀𝗶𝗮𝗻 𝗰𝗼𝗻𝘁𝗶𝗻𝗲𝗻𝘁 some 𝟱𝟱 𝗺𝗶𝗹𝗹𝗶𝗼𝗻 𝘆𝗲𝗮𝗿𝘀 𝗮𝗴𝗼.
��𝗙: 𝗤𝗼𝗺𝗼𝗹𝗮𝗻𝗴𝗺𝗮 𝗙𝗼𝗿𝗺𝗮𝘁𝗶𝗼𝗻 (𝗘𝘃𝗲𝗿𝗲𝘀𝘁 𝗹𝗶𝗺𝗲𝘀𝘁𝗼𝗻𝗲𝘀):
It is the un-metamorphosed layer of limestone here called ‘QF’ for 𝗤𝗼𝗺𝗼𝗹𝗮𝗻𝗴𝗺𝗮 𝗙𝗼𝗿𝗺𝗮𝘁𝗶𝗼𝗻, which forms the 𝘀𝘂𝗺𝗺𝗶𝘁 of Everest. It is separated from the underlying Yellow Band layer by a low angle detachment fault.
𝗬𝗕:𝗬𝗲𝗹𝗹𝗼𝘄 𝗕𝗮𝗻𝗱:
This is the layered bedding. It is a limestone, formed from a shallow marine sediment, heated to become a 𝗺𝗮𝗿𝗯𝗹𝗲.
𝗘𝗦: 𝗘𝘃𝗲𝗿𝗲𝘀𝘁 𝗦𝗲𝗿𝗶𝗲𝘀:
It consists of 𝘀𝗲𝗱𝗶𝗺𝗲𝗻𝘁𝗮𝗿𝘆 rock which has been metamorphosed at reasonably high temperatures. It is separated from the underlying layer by a low angle almost horizontal fault.
𝗥𝗙: 𝗥𝘂𝗻𝗴𝗯𝗼𝗸 𝗳𝗼𝗿𝗺𝗮𝘁𝗶𝗼𝗻:
The Rungbok Formation consists of ‘LG’ Leuco- granite and gneiss.RF is a gneiss: rock partly melted and metamorphosed under high temperatures.
𝙁𝙤𝙨𝙨𝙞𝙡𝙨:
These rocks still contain the fossils of marine animals such as 𝗕𝗿𝗮𝗰𝗵𝗶𝗼𝗽𝗼𝗱𝘀, 𝗖𝗼𝗻𝗼𝗱𝗼𝗻𝘁𝘀 and 𝗖𝗿𝗶𝗻𝗼𝗶𝗱𝘀 that occupied tropical habitats during one of the most 𝗶𝗺𝗽𝗼𝗿𝘁𝗮𝗻𝘁 𝗶𝗻𝘁𝗲𝗿𝘃𝗮𝗹𝘀𝗹𝘀 in 𝗘𝗮𝗿𝘁𝗵'𝘀 history, the 𝗚𝗿𝗲𝗮𝘁 𝗢𝗿𝗱𝗼𝘃𝗶𝗰𝗶𝗮𝗻 𝗕𝗶𝗼𝗱𝗶𝘃𝗲𝗿𝘀𝗶𝗳𝗶𝗰𝗮𝘁𝗶𝗼𝗻 𝗘𝘃𝗲𝗻𝘁 (𝗚𝗢𝗕𝗘).
Who on this planet would ever design a second year sedimentology course where ALL of the depositional environments and events are only explained and described in full at the END?!
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Marine sedimentary rocks are the most common along southern New South Wales coast of Australia. These contain many marine shell fossils in sandstones and siltstones that represent a shallow to deep sea environments from around 250 million years ago.
These creatures would have fed on the organic-rich debris found within the sediment that now surrounds them, and which after many millions of years have turned into a hard rock.
به نام خدا معرفی مجلات علمی و پژوهشی، علمی و ترویجی و ISI رشته زمین شناسی: ✓ Sedimentology √ پیشرو بین المللی در زمینه خود، رسوب شناسی تحقیقات پیشگامانهای را از طیف وسیعی منتشر میکند. رسوب شناسی، زمین شناسی رسوبی و رسوبی ژئوشیمی مناطق تحت پوشش عبارتند از: انتقال تجربی و نظری دانه شارهای رسوبی محیط های رسوبی مدرن و قدیمی چینه نگاری توالی تعامل رسوب و ارگانیسم خاکهای دیرینه دیاژنز ژئوشیمی ایزوتوپ پایدار رسوب شناسی محیطی گروه آموزشی و پژوهشی زمین آزمون #Sedimentology #Geology #ZaminAzmoonGroup #zaminazmoon #Dr_Samadi #Dr_Ramin_Samadi #Geologist #geology_journal #فصلنامه_علمی_پژوهشی #مجله #ژورنال #نشریه #فصلنامه #لیست_مجلات_علمی_رشته_زمین_شناسی #وزارت_علوم #فهرست_نشریات_مجلات_علمی_معتبر_زمین_شناسی #مقالات_علمی_پژوهشی_ژورنال_های_داخلی_رشته_زمین_شناسی #معرفی_مجلات_علمی_پژوهشی_زمین_شناسی #معرفی_مجلات_علمی_ترویجی_زمین_شناسی #معرفی_مجلات_ISI_زمین_شناسی #دکتر_رامین_صمدی #دکتر_صمدی #ایران #زمین_آزمون #زمین_شناسی #زمین_شناس #گروه_آموزشی_و_پژوهشی_زمین_آزمون https://www.instagram.com/p/Cembof3Jat5/?igshid=NGJjMDIxMWI=
spent like altogether 1.5 hours preparing for my sedimentary facies analysis exam today and i got 80% on the first part and an objectively middling, but compared to the rest of the results Very Good score in the second part so actually i think i'm invincible and nothing bad will ever happen to me
The Yukon River exports sixty megatons of sediment per year away into the Bering Sea, the majority of it silt and clay derived from the glaciers carving stone at its headwaters. We call this measurement, movement quantified over time, a flux.
I kissed them the night before they left the hemisphere on an exploration geology contract, a two year visa. They study ores, hard rock, mapping what has sat solid in earth for an age, waiting. Their hands were callused already from the heft of samples.
They study ores, and I study fluxes -- water, sediment, salt, ice. My hands are finicky, shaky things, carved for the precision of catching a change in the act. You cannot hold a flux, only bear witness.
I kissed them in a liminal bedroom, half-boxed, walls bared. I took off my binder and we laughed -- oh, fluxes -- at how when they return, we will be changed, both, irrevocably and unavoidably, sure as every river I've known rises each spring and reworks the geometry of its own banks.
To live is to be in flux. It is my honour and joy, queer geologist I am, to bear witness.
We kiss, forehead to forehead, eyes open. Their hand presses into mine, chipped nail polish, calluses blooming. Sixty megatons of sediment, passing through my spread fingers --