The Malwa constituting the Deccan Trap volcanic province (Upper Cretaceous –Eocene). The Malwa region occupies a plateau in Western M.P and South-Eastern Rajasthan (between 21010’ N and 73045 E ) with Gujarat in the West . The region include the M.P district of Agar, Dewas, Dhar, Indore, Jhabua, Mandsaur, Neemuch, Rajgarh, Ratlam, Shajapur, Ujjain parts of Guna and Sehore and the Rajasthan district of Jhalawar and parts of Banswara and Pratapgarh. It is covered an area of 81,767 sq. km. and elevation of 500m.Ujjain region constituting the Malwa region. Ujjain District is situated in Madhya Pradesh and lies between longitude 750 45’ to 750 50’ and latitude 230 15’ to 230 5’ and area lies the toposheet No. 45M/16 and 46M/12.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
The Malwa constituting the Deccan Trap volcanic province (Upper Cretaceous –Eocene). The Malwa region occupies a plateau in Western M.P and South-Eastern Rajasthan (between 21010’ N and 73045 E ) with Gujarat in the West . The region include the M.P district of Agar, Dewas, Dhar, Indore, Jhabua, Mandsaur, Neemuch, Rajgarh, Ratlam, Shajapur, Ujjain parts of Guna and Sehore and the Rajasthan district of Jhalawar and parts of Banswara and Pratapgarh. It is covered an area of 81,767 sq. km. and elevation of 500m.Ujjain region constituting the Malwa region. Ujjain District is situated in Madhya Pradesh and lies between longitude 750 45’ to 750 50’ and latitude 230 15’ to 230 5’ and area lies the toposheet No. 45M/16 and 46M/12.
The term "trap" has been used in geology since 1785–95 for rock formations. It is derived from the Swedish word for stairs (trapp , trappa) and refers to the step-like hills forming the landscape of the region.
The plateau: also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A plateau is an elevated land. It is a flat-topped table standing above the surrounding area. A plateau may have one or more sides with steep slopes.
LIP – Large Igneous provinces. (Province = Area / Region)
DVP - The Deccan Volcanic Province is one of the Earth’s giant continental flood basalts and has a total exposed area of about half a million square kilometers in Maharashtra, Madhya Pradesh, Gujrat and some part of Andhra Pradesh. Deccan trap has maximum thickness 3400m in western ghat and its thickness goes decrease toward east side. At Amrakantat on east its thickness is just 160m. Geographical distribution is between latitudes 16° - 24° N and longitudes 70° - 77° E.
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
chinji zone:
by these slides you will know about the chinji zone location in siwalik hills
fossil fuels of the chinji zone
how chinji zone formation occurs
FEldspar etc...
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
chinji zone:
by these slides you will know about the chinji zone location in siwalik hills
fossil fuels of the chinji zone
how chinji zone formation occurs
FEldspar etc...
This time the slide rock mainly contains what Huangshan has seen and heard, as well as the resolution of stone sampling and the final understanding of the law.
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archaeocyathid
o
Cambrian - sessile, reef-building marine organisms of warm tropical and subtropical waters that lived during the early (lower) Cambrian period.
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bioturbation
o
Cambrian - the reworking of soils and sediments by animals or plants. Its effects include changing texture of sediments (diagenetic), bioirrigation and displacement of microorganisms and non-living particles. Common bioturbators include annelids and bivalves (mussels, clams, gastropods).
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Burgess Shale
o
Cambrian - located in the Canadian Rockies of British Columbia, is one of the world's most celebrated fossil fields. It is famous for the exceptional preservation of the soft parts of its fossils. At 505 million years (Middle Cambrian) old, it is one of the earliest fossil beds containing soft-part imprints.
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Cambrian explosion
o
Cambrian - the relatively rapid appearance, around 530 million years ago, of most major animal phyla, as demonstrated in the fossil record, accompanied by major diversification of organisms
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Iapetus Ocean
Cambrian/Ordovician - Precursor to the Atlantic. An ocean that existed in the Neoproterozoic and Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). The ocean disappeared with the Caledonian, Taconic and Acadian orogenies, when these three continents joined to form one big landmass called Laurussia.
maturity Cambrian
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Paleozoic Era
o
Cambrian - the earliest of three geologic eras of the Phanerozoic Eon, spanning from roughly 541 to 252.2 million years ago. It is the longest of the Phanerozoic eras, and is subdivided into six geologic periods (from oldest to youngest): the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian.
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passive margin
o
Cambrian - the transition between oceanic and continental crust which is not an active plate margin. It is constructed by sedimentation above an ancient rift, now marked by transitional crust. Continental rifting creates new ocean basins.
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trilobite
o
Cambrian - extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest known groups of arthropods. Trilobites finally disappeared in the mass extinction at the end of the Permian about 250 million years ago. The trilobites were among the most successful of all early animals, roaming the oceans for over 270 million years.
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bentonites
o
Ordovician - essentially impure clay consisting mostly of montmorillonite. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin.
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Cincinnati arch
o
Ordovician - when continents crashed together during the two orogeny's you have the Appalachian mountains and then a down drop into the Appalachian basin going west and then going west the next rise is the Cincinnati arch and the next basin is the Illinois basin.
epeir.
Surreal places in the world that transport you to the world of fantasy. Many surreal places are present in the world which are extremely beautiful & mind-blowing.
Yeosu (여수, 麗水) is a beautiful port city of Korea, she will host World Expo 2012. Lishui(麗水), China is one of the sister cities of Yeosu; the city’s name is same as the Hanja name of Yeosu.
神秘的禾木 The amazing Hemu Village
Located within the Kanas Lake scenic area in the north of Xinjiang and near the border of Kazakhstan, Mongolia, and Russia, Hemu is one of the six most beautiful villages in China.
Winter fishing on Chagan Lake 查干湖冬捕 Changan Lake located in China, is the only place that saves the old Mongolian traditional winter fishing method. Winter fishing fair is held annually there in late December… Transcript written by zqPei
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The Cherry Blossom season in Hunza begins in the second week of March and lasts until the end of April, varying with altitude. During this enchanting period, tourists from around the world flock to Hunza Valley to witness its transformation into a vibrant tapestry of white, pink, and green. The valley comes alive with cherry blossoms, creating a picturesque and mesmerizing landscape that captivates visitors.
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In this presentation, we delve into the captivating realm of Antarctica, Earth's southernmost continent. This icy wilderness stands as a testament to extremes, with record-breaking cold temperatures and vast expanses of pristine ice. Antarctica's landscape is dominated by towering glaciers, colossal icebergs, and expansive ice shelves. Yet, amidst this frozen expanse, a rich tapestry of unique wildlife thrives, including penguins, seals, and seabirds, all finely attuned to survive in this harsh environment. Beyond its natural wonders, Antarctica also serves as a vital hub for scientific exploration, providing invaluable insights into climate change and the Earth's history
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Its running cost is among the diverse vital aspects you must consider before buying an electric scooter. Calculate the cost of getting e-scooter charge for your regular usage to calculate its economic efficiency, similar to people who investigate the mileage of petrol or diesel-driven scooters.
2. Danxia landform Danxia Landform is a relatively new kind of landform having been defined and recognized internationally in the last few years.It refers to various landscapes found in southeast and southwest China that “consists of red bed characterized by steep cliffs”. It is a unique type of petrographic geomorphology found in China. Danxia landforms are formed from red-colored sandstones and conglomerates of largely Cretaceous age. The landforms look very much like karst topography that forms in areas underlain by limestones, but since the rocks that form Danxia are sandstones and conglomerates, they have been called "pseudo-karst" landforms. The Danxia landform is named after Mount Danxia, one of the most famous examples of the Danxia landform. 丹霞地貌系由陆相红色砂砾岩构成的具有陡峭坡面的各种地貌形态。形成的必要条件是砂砾岩层巨厚,垂直节理发育。因在中国广东省北部仁化县丹霞山有典型发育而得名。
3. Seven Most Beautiful Danxia Landscapes in China 中国七大丹霞地貌 1Mount Longhu龙虎山 2Mount Langshan崀山 3 Zhangyi张掖丹霞地貌 4ChishuiDanxia赤水丹霞地貌 5Dajin Lake 大金湖 6Mount Wuyi武夷山 7Mont Danxia丹霞山
4. Danxia Landform is widely distributed In the world Though the Danxia landform is named after Mount Danxia, one of the most famous examples of the Danxia landform, it is also widely distributed in the world.The known number of sites with well developed Danxia landform in other regions and countries already amounts to 51, in 19 countries. For example, Arches National Park of USA centralizes the most Stone Windows and natural bridges, natural arches, similar to Danxia Landform. Arches National Park 美国拱门国家公园 丹霞地貌在全世界各处广泛分布 丹霞地貌在全世界广泛存在,已知其他19个国家共有51处丹霞地貌。虽然这些国家的术语不叫“DanxiaLandform”,但都属于丹霞地貌。
18. 赤水丹霞地貌 ChishuiaDanxia landform The formation of the Danxia landform can be dated back to the Jurassic and Cretaceous periods about 100 million years ago. It covers an area of over 1,000 square kilometers. The collapsing and weathering of a thick layer of red quartzose formed the area’s unique landscape, including amazing valleys, sheer precipices and rushing waterfalls. Formed of sandstone, the ChishuiDanxia landform is situated where the Sichuan Basin meets the Northern Guizhou Plateau, an area of humid weather and dense vegetation.
19. Elephant Trunk Hill Elephant Trunk Hill is located between the southeast of Guilin City and the western bank of the Li River. It is the Guilin's best known sight and owns a charming flavor in sunrise and sunset arousing your imagination. The hill is originally named "Li Hill," "Yi Hill" and "Chenshui Hill." It has three hundred and sixteen million years of history. This hill got its name as it resembles elephant leisurely sucking water from the river with its long trunk. With an elevation of 200 meters, the hill towers 55 meters above the water measuring 108 meters in length and 100 meters in width. 象鼻山
27. The World Heritage Committee is including China's Danxia landforms on the World Heritage List. The decision was made at the committee's 34th meeting on Aug 2nd 2010 in Brazil. Danxia Landforms consist of red sedimentary rock and steep cliffs. They are located across six Chinese provinces, including Guangdong and Jiangxi. 联合国教科文组织于2010年在巴西召开的第34届世界遗产委员会上将中国丹霞地貌列入世界遗产名录。丹霞地貌系指有陡崖的陆相红层地貌,位于广东江西等六个省。