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Tai Mo Shan Country Park
Tai Mo Shan is the highest peak in Hong Kong, with an elevation of . It is located at approximately the geographical centre of the New Territories. The Tai Mo Shan Country Park covers an area of around Tai Mo Shan. It is located to the north of Tai Lam Country Park. The Long Falls is the highest waterfall in Hong Kong. Geography The whole Tai Mo Shan mountain range, known as Guan Fu Mountain (官富山, named after the salt field Kwun Fu Cheung (官富場) in present-day Kowloon Bay) in Ming and Qing dynasties, covers over 350 square km, and stretches from Tai Lam Chung Reservoir in the West near Tuen Mun and Ma On Shan in the east and the mountains of Kowloon and Clear Water Bay in the south. Two other significant coastal peaks, the Lantau Peak (934m) on Lantau Island and Mount Wutong in Shenzhen (943.7m) are approximately 27 km to the southwest and 21.5 km to the northeast respectively. Subpeaks There are a few subpeaks that are given names in the Tai Mo Sh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tai To Yan
Tai To Yan () is a mountain that lies in northern Hong Kong near Fanling–Sheung Shui New Town, Fanling. It is close to a similarly named peak called Pak Tai To Yan. Geography Tai To Yan is 566 metres tall and is the tallest mountain in the nearby area. Access Tai To Yan is in the Lam Tsuen Country Park in northern Hong Kong. It is hiked as part of the Razors Edge Ridge Hike which brings hikers to both Tai To Yan (566 m) and nearby Pak Tai To Yan (480 m). Hikers can start their hike near Kadoorie Farm and Botanic Garden, Kadoorie Farm and finish a few hours later at Fanling station, Fanling MTR station or Wah Ming Estate Bus Terminus. See also * List of mountains, peaks and hills in Hong Kong * Lam Tsuen Country Park References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clear Water Bay
Clear Water Bay () is a bay on the eastern shore of Clear Water Bay Peninsula of Hong Kong, located within Clear Water Bay Country Park. There are two beaches at Clear Water Bay: "Clear Water Bay First Beach" and "Clear Water Bay Second Beach". The name is also used to describe the area around the bay on the peninsula. Beaches During the summer, both beaches have life guards on duty. Changing rooms, lockers, shower facilities, toilets and rafts are available at both beaches. A BBQ area can only be found on the first beach, but there is a kiosk selling refreshment on the second beach. There is an unavoidable flight of stairs of about 100 steps for both beaches, so strollers and wheelchairs cannot be used to access the beaches. Both beaches are protected by shark nets after three fatal shark attacks occurred in 1995. On 13 June 1995, a 49-year-old woman Wong Kui-Yong () had her left forearm and left leg bitten off by a shark at Clear Water Bay 1st beach. She died of her injurie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Rock
Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from lava erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and metamorphic rocks and constitute an important element of some sediments and sedimentary rocks. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of Precambrian shield geology, the term "volcanic" is often applied to what are strictly metavolcanic rocks. Volcanic rocks and sediment that form from magma erupted into the air are called "volcaniclastics," and these are technically sedimentary rocks. Volcanic rocks are among the most common rock types on Earth's surface, particularly in the oceans. On land, they are very common at plate boundaries and in flood basalt provinces. It has been estimated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mantle (geology)
A mantle is a layer inside a planetary body bounded below by a Planetary core, core and above by a Crust (geology), crust. Mantles are made of Rock (geology), rock or Volatiles, ices, and are generally the largest and most massive layer of the planetary body. Mantles are characteristic of planetary bodies that have undergone planetary differentiation, differentiation by density. All Terrestrial planet, terrestrial planets (including Earth), a number of Asteroid, asteroids, and some planetary Natural satellite, moons have mantles. Earth's mantle The Earth's mantle is a layer of Silicate minerals, silicate rock between the Crust (geology), crust and the Earth's outer core, outer core. Its mass of 4.01 × 1024 kg is 67% the mass of the Earth. It has a thickness of making up about 84% of Earth's volume. It is predominantly solid, but in Geologic time scale, geological time it behaves as a Viscosity, viscous fluid. Partial melting of the mantle at mid-ocean ridges produ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Period
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define gl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miu Ko Toi
Miu Ko Toi ( Chinese: 妙高台) is a peak in Hong Kong. It is situated in New Territories and stands at a height of above the sea level. It is one of the subpeaks of the tallest mountain in Hong Kong Tai Mo Shan. Name The Cantonese name Miu Ko Toi ( Chinese: 妙高台; Jyutping: Miu6 Gou1 Toi4) literally means "Fantastic High Lookout". Access Miu Ko Toi is only accessible by foot and is south west of Tai Mo Shan. In between trail markers M150 and M151 of Tai Mo Shan Road, there is the entrance for a trail called Heung Shek Path. Assuming that you are walking up toward Tai Mo Shan's summit, turning right when you see Heung Shek Path will lead you to Miu Ko Toi's summit. See also * List of mountains, peaks and hills in Hong Kong * Tai Mo Shan Tai Mo Shan is the highest peak in Hong Kong, with an elevation of . It is located at approximately the geographical centre of the New Territories. The Tai Mo Shan Country Park covers an area of around Tai Mo Shan. It ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wo Yeung Shan
Wo Yeung Shan (), officially known as Wo Yang Shan, is the fifth-highest peak in Hong Kong at a height of . It is located south east of Tai Mo Shan in the New Territories, between Tsuen Wan District and Tai Po District. Name The Cantonese name Wo Yeung Shan ( Chinese: : 禾秧山; Jyutping: Wo4 Joeng1 Saan1) literally means "Rice Seedling Mountain". See also * List of mountains, peaks and hills in Hong Kong The following is a list of mountains, peaks and hills in Hong Kong. In the romanisation system used by the Hong Kong Government known as Standard Romanisation, 'shan' and 'leng' are the transliterations of the Cantonese words for 'mount' ( ... References Mountains, peaks and hills of Hong Kong Tsuen Wan District Tai Po District {{HongKong-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sei Fong Shan
Sze Fong Shan (), located in Tai Po District of the New Territories, is the fourth highest peak in Hong Kong. With a height of 784 m (2,572 ft), it is northeast of Tai Mo Shan. The Eighth Stage of the MacLehose Trail passes near it. Name The Cantonese name Sze Fong Shan ( Chinese: 四方山; Cantonese Yale: sei fōng shāan, Jyutping: Sei3 Fong1 Saan1) literally means "Square Mountain". Subpeak Chau Ma Kong () is a subpeak northnortheast of Sze Fong Shan and east of Ng Tung Chai waterfalls. See also * List of mountains, peaks and hills in Hong Kong The following is a list of mountains, peaks and hills in Hong Kong. In the romanisation system used by the Hong Kong Government known as Standard Romanisation, 'shan' and 'leng' are the transliterations of the Cantonese words for 'mount' ( ... References Mountains, peaks and hills of Hong Kong Tai Po District {{NewTerritories-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shenzhen
Shenzhen (; ; ; ), also historically known as Sham Chun, is a major sub-provincial city and one of the special economic zones of China. The city is located on the east bank of the Pearl River estuary on the central coast of southern province of Guangdong, bordering Hong Kong to the south, Dongguan to the north, and Huizhou to the northeast. With a population of 17.56 million as of 2020, Shenzhen is the third most populous city by urban population in China after Shanghai and Beijing. Shenzhen is a global center in technology, research, manufacturing, business and economics, finance, tourism and transportation, and the Port of Shenzhen is the world's fourth busiest container port. Shenzhen is classified as a Large-Port Megacity, the largest type of port-city in the world. Shenzhen roughly follows the administrative boundaries of Bao'an County, which was established since imperial times. The southern portion of Bao'an County was seized by the British after the Opium Wars an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
