World's major ocean floors can be studied by their submarine reliefs and bathysphere.
- Horizontal distribution of Seawater Temperature (latitudinally)
Australia is a country located in Oceania between the Indian and Pacific oceans. It covers an area of around 7.7 million square kilometers, making it the sixth largest country, and has diverse landscapes including eastern mountain ranges, central lowlands, and a western plateau. The central lowlands contain important river basins like the Murray-Darling, which supports agriculture, and Lake Eyre, a large salt lake. New Zealand is also located in Oceania and consists of two main islands, North and South, separated by Cook Strait. The South Island features high mountain ranges like the Southern Alps, while the North Island has lower volcanic mountains and peninsulas.
The document discusses the national territory of the Philippines according to its constitution. It includes land, water, and air domains. There have been disputes over islands in the South China Sea claimed by several Asian countries, making territorial rights an important issue. The Philippine government has increased its territorial claim to include the Kalayaan Islands based on the archipelago doctrine which defines its territorial waters as extending 12 miles from its outermost islands. The document also describes the topography of the Philippines, including its mountain ranges, volcanoes, and other physical features across its islands.
The document summarizes the major physiographic regions of North America:
- The Canadian Shield is a basement rock region covered by thin soil and dotted with lakes. It is rich in minerals and was heavily glaciated.
- The Appalachian Mountains were formed by tectonic collisions and once reached 20,000 feet high. They run along the eastern US and Canada.
- The Western Mountains include the Rocky Mountains, plateaus like the Colorado Plateau and Columbia Plateau, and coastal ranges like the Pacific Coast Mountains. Landforms include the Grand Canyon.
- The Interior Lowlands contain the Great Plains, stretching from Canada to Mexico along the Rockies, and various coastal plains along the Gulf and Atlantic.
Physical environment and history of se asiaMark McGinley
The physical environment of Southeast Asia, characterized by warm and wet conditions, has supported rainforests and influenced the region's history. The monsoon winds and strategic location along trade routes led to a mix of cultural influences in early states like Srivijaya and Malacca. European colonialism in the 16th-20th centuries gave way to independent nations in the post-WWII era, but some countries still face issues related to ethnic and religious diversity.
Mineralogy and geochemical appraisal of paleo redox indicators in maastrichti...Alexander Decker
This summary provides the key details about the document in 3 sentences:
The document discusses a study of the mineralogy and geochemistry of Maastrichtian shale samples from the Mamu Formation in the Anambra Basin of Nigeria. Various analytical techniques were used to characterize the shale samples and investigate paleo-redox conditions. The results suggest the shales were deposited under oxidizing conditions based on mineralogical and geochemical proxies, and were derived from felsic source rocks that experienced strong chemical weathering.
The Pacific Ocean is the largest ocean in the world. It has significant differences in continental shelf width between its eastern and western coasts. The shelves are broad along eastern Asia and Australia, ranging from 160-1600km wide. The shelves are less extensive along western Americas due to proximity to mountain chains. The ocean contains various basins up to 10,000m deep like the Philippine and Southwestern Pacific basins, as well as the deepest ocean trenches reaching over 11,000m like the Mariana Trench. It also has ridges, rises, and fracture zones that separate regions of the seabed. There are nearly 20,000 islands throughout the Pacific Ocean ranging from continental to volcanic to coral formations.
Australia is the smallest of Earth's continents, with an area of 7.615 million km2. It has a diverse landscape including large deserts in the west and center, sweeping plains and plateaus in the center, and highlands in the east. Structurally, Australia was once part of the ancient supercontinent Gondwana. The climate is mostly tropical and subtropical, with low rainfall across much of the interior.
The Philippines (Archipelago and it's people)Jenver Mojica
The document provides information on the geography of the Philippine archipelago. It notes that the Philippines comprises over 7,000 islands located in Southeast Asia. The five largest islands are Luzon, Mindanao, Samar, Negros, and Panay. The archipelago has many mountains, volcanoes, rivers, lakes and seas. It also describes the different soil and mineral resources found throughout the islands. In conclusion, it briefly discusses four theories for the origins of the archipelago: volcanism, diastrophism, gradation, and land bridges connecting it to mainland Asia in the past.
Australia is a country located in Oceania between the Indian and Pacific oceans. It covers an area of around 7.7 million square kilometers, making it the sixth largest country, and has diverse landscapes including eastern mountain ranges, central lowlands, and a western plateau. The central lowlands contain important river basins like the Murray-Darling, which supports agriculture, and Lake Eyre, a large salt lake. New Zealand is also located in Oceania and consists of two main islands, North and South, separated by Cook Strait. The South Island features high mountain ranges like the Southern Alps, while the North Island has lower volcanic mountains and peninsulas.
The document discusses the national territory of the Philippines according to its constitution. It includes land, water, and air domains. There have been disputes over islands in the South China Sea claimed by several Asian countries, making territorial rights an important issue. The Philippine government has increased its territorial claim to include the Kalayaan Islands based on the archipelago doctrine which defines its territorial waters as extending 12 miles from its outermost islands. The document also describes the topography of the Philippines, including its mountain ranges, volcanoes, and other physical features across its islands.
The document summarizes the major physiographic regions of North America:
- The Canadian Shield is a basement rock region covered by thin soil and dotted with lakes. It is rich in minerals and was heavily glaciated.
- The Appalachian Mountains were formed by tectonic collisions and once reached 20,000 feet high. They run along the eastern US and Canada.
- The Western Mountains include the Rocky Mountains, plateaus like the Colorado Plateau and Columbia Plateau, and coastal ranges like the Pacific Coast Mountains. Landforms include the Grand Canyon.
- The Interior Lowlands contain the Great Plains, stretching from Canada to Mexico along the Rockies, and various coastal plains along the Gulf and Atlantic.
Physical environment and history of se asiaMark McGinley
The physical environment of Southeast Asia, characterized by warm and wet conditions, has supported rainforests and influenced the region's history. The monsoon winds and strategic location along trade routes led to a mix of cultural influences in early states like Srivijaya and Malacca. European colonialism in the 16th-20th centuries gave way to independent nations in the post-WWII era, but some countries still face issues related to ethnic and religious diversity.
Mineralogy and geochemical appraisal of paleo redox indicators in maastrichti...Alexander Decker
This summary provides the key details about the document in 3 sentences:
The document discusses a study of the mineralogy and geochemistry of Maastrichtian shale samples from the Mamu Formation in the Anambra Basin of Nigeria. Various analytical techniques were used to characterize the shale samples and investigate paleo-redox conditions. The results suggest the shales were deposited under oxidizing conditions based on mineralogical and geochemical proxies, and were derived from felsic source rocks that experienced strong chemical weathering.
The Pacific Ocean is the largest ocean in the world. It has significant differences in continental shelf width between its eastern and western coasts. The shelves are broad along eastern Asia and Australia, ranging from 160-1600km wide. The shelves are less extensive along western Americas due to proximity to mountain chains. The ocean contains various basins up to 10,000m deep like the Philippine and Southwestern Pacific basins, as well as the deepest ocean trenches reaching over 11,000m like the Mariana Trench. It also has ridges, rises, and fracture zones that separate regions of the seabed. There are nearly 20,000 islands throughout the Pacific Ocean ranging from continental to volcanic to coral formations.
Australia is the smallest of Earth's continents, with an area of 7.615 million km2. It has a diverse landscape including large deserts in the west and center, sweeping plains and plateaus in the center, and highlands in the east. Structurally, Australia was once part of the ancient supercontinent Gondwana. The climate is mostly tropical and subtropical, with low rainfall across much of the interior.
The Philippines (Archipelago and it's people)Jenver Mojica
The document provides information on the geography of the Philippine archipelago. It notes that the Philippines comprises over 7,000 islands located in Southeast Asia. The five largest islands are Luzon, Mindanao, Samar, Negros, and Panay. The archipelago has many mountains, volcanoes, rivers, lakes and seas. It also describes the different soil and mineral resources found throughout the islands. In conclusion, it briefly discusses four theories for the origins of the archipelago: volcanism, diastrophism, gradation, and land bridges connecting it to mainland Asia in the past.
The International Journal of Engineering and Science (The IJES)theijes
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
Keys to paleogeographical interpretation of the enugu and the mamu formations...Alexander Decker
The document analyzes the lithofacies, palynological assemblages, and facies associations of the Enugu and Mamu Formations in southeastern Nigeria to interpret their depositional environments, paleogeography, and ages. Palynological analysis indicates a Late Campanian to Early Maastrichtian age for the Enugu Formation and Early-Mid Maastrichtian age for the Mamu Formation. The coarsening upward lithofacies and decrease in marine dinoflagellates from the Enugu to Mamu Formations suggest shallowing of the sea during regression. Facies associations grade from transgressive in the Enugu to regressive in the Mamu, representing marine transgression and subsequent shore
Granomeric Analysis of Mamu Formation and Enugu Shale around Ozalla and Its E...iosrjce
The study area lies within the Anambra Basin which geologically made up of Enugu Shale and
Mamu Formation. This study aimed at determining the geology and depositional environments of these
Formations through field relationship and grain size distribution as well as morphometric studies. The field
data shows Enugu Shale as fissile, light grey with extraformational clast which graded into Mamu Formation
which is made up of alternating sequence of shale, siltstone, mudstone, coal and sand, it shows a fluctuating
environment. The granulometric study of sand member of Mamu Formation shows characteristic very well
sorted, fine to medium grains which were deposited in relatively turbulent well aerated marine environment
probably above wave base. The bivariate and the multivariate results reveal Aeolian/shallow marine deposit.
The fissility of Enugu Shale suggests that it was deposited in low energy environment, distal to proximal lagoon
environment and the presence of extraformatonal clast indicates fluvial incursion. However, it can be concluded
that Mamu Formation was deposited in fluctuating environment ranging from an oxygenated shallow marine to
acidic swampy environment. Hence is paralic Formation.
This document provides an overview of coal deposits in the Mamu Formation in the Anambra Basin of Nigeria. It discusses the geology, stratigraphy, evolution and paleoenvironmental characteristics of the basin. It also describes the exploration history of coal in the basin, focusing on deposits in the Mamu Formation. Finally, it discusses the economic potential of the coal deposits for combustion, gasification, and liquefaction. Nigeria has over 2 billion tonnes of coal reserves, with about 650 million tonnes proven, primarily located in the Anambra Basin.
The document provides information about the sedimentary basins in Nigeria, focusing on the Benue Trough. It describes the Benue Trough as a major geological formation underlying a large part of Nigeria. It formed as part of the Central African Rift System during the breakup of the supercontinent Gondwana. The trough contains up to 6000m of Cretaceous sediments and is divided into the Lower, Middle, and Upper Benue basins. While exploration has focused on the adjacent Niger Delta Basin, the Benue Trough shows potential for oil and gas discoveries.
Petrography of ajali sandstone in ayogwiri – fugar – orame area of western an...Alexander Decker
- The document analyzes the petrography of the Ajali Sandstone Formation in the Western Anambra Basin of Nigeria to understand its diagenetic and depositional history.
- Thin section analysis shows the sandstone is a quartz arenite composed mainly of subangular to subrounded quartz grains that have undergone compaction, dissolution, alteration, and corrosion during diagenesis. This left the sandstone friable with little cement.
- Samples from three locations - Ayogwiri, Fugar, and Orame - exhibited similar diagenetic features including authigenic quartz, reaction rims, and corroded grain margins. This diagenesis reduced cementation and led to
The Antarctica is centered asymmetrically around the South Pole. It is the southernmost continent in world. The 66 degree 34 minutes south latitude forms the outermost boundary of the Antarctic circle. The area covered within this circle is called as the Antarctic Continent. It includes parts of the Southern ocean, surrounding seas, ice shelves, continental glaciers, plateaus and mountain ranges. The Antarctica is the coldest, driest, and windiest continent, possessing many unique features to learn.
The document summarizes the hydrogeology of Jammu and Kashmir, India. It describes the region's climate, major water bodies, geological formations, and groundwater conditions. The state has varied climates including cold desert in Ladakh, moderate in Kashmir, and sub-tropical in Jammu. Major rivers include the Jhelum, Chenab, and Indus. Groundwater occurs under both confined and unconfined conditions in different areas, with depth to water tables ranging from just below land surface to over 100 meters deep. While groundwater quality is generally suitable for drinking, some areas have high fluoride or nitrate. Overall development of groundwater resources has been limited compared to potential.
The document summarizes the tectonic framework of India in 3 broad divisions - Peninsular India, Extra-Peninsular India, and the Indo-Gangetic Plain. Peninsular India comprises the Indian shield and its sedimentary basins, and is further divided into the shield areas, mobile belts, and Proterozoic sedimentary basins. Extra-Peninsular India includes the Himalayan mountain ranges, divided into the Lesser Himalayan zone, Central Crystalline zone, and Tethyan zone. The Indo-Gangetic Plain is a deep crustal trough in northern India filled with Quaternary sediments.
The Cambay Basin is an intracratonic rift graben located in northwest India that began forming following the Deccan Traps volcanic event in the late Cretaceous. The basin is filled with up to 8km of Tertiary sedimentary rocks. Major source rocks include the thick Cambay Shale deposited in the early Eocene during a transgression. Hydrocarbon reservoirs are found in the Olpad Formation, Hazad delta sands, and Miocene formations. Multiple petroleum plays exist, including those in the Paleocene-early Eocene, middle Eocene, and late Eocene-Oligocene sequences. The Cambay Shale is a prolific source of oil and gas in the
This document summarizes the land relief and water distribution of several continents and regions including:
- Spain, Europe, Africa, America, Asia, and Oceania. For each area, it describes key physical features such as mountain ranges, deserts, peninsulas, rivers, lakes, seas, and their locations. The document provides information on the average altitude and notable geographic characteristics of each region.
Bombay High is an offshore oilfield located 160 km off the coast of Mumbai, India. It was discovered in 1964-1967 and is operated by ONGC. It supplied 14% of India's oil needs and accounted for 38% of domestic production until 2004. The field is located in the Bombay offshore basin and produces from limestone reservoirs of Miocene age. It has produced over 2 billion barrels of oil and 3 trillion cubic feet of gas to date. A major fire in 2005 destroyed the Mumbai High North platform, costing $1.2 billion to rebuild. ONGC continues exploration and production activities in the area through seismic surveys.
The document summarizes the five major oceans of the world: the Pacific Ocean, the largest and deepest ocean located between Asia/Australia and North/South America; the Atlantic Ocean, the second largest located between Europe/Africa/North America; the Indian Ocean, the third largest located between Africa/Asia/Australia; the Arctic Ocean, the smallest located around the North Pole; and the Southern Ocean surrounding Antarctica. Each ocean is briefly described in terms of location, key waterways, climate patterns, ocean floor features, and surface/ice coverage.
There are two peninsulas that branch off Southeast Asia - the Indochinese Peninsula and the Malay Peninsula. This region also contains many archipelagoes, or closely grouped islands, such as the Philippines. It has extensive coastlines and rivers like the Mekong, which forms a wide delta near the coast. The Mekong is also home to the world's largest catfish. Mountains and volcanoes are common due to the region sitting on the ring of fire, with islands evolving over time from volcanoes to coral atolls.
The document provides information on key concepts related to Earth's atmosphere and natural resources. It defines key terms like the layers of the atmosphere, natural resources, and effects of pollution. It describes the troposphere as the lowest layer where weather occurs and the different gas layers above it. It also explains renewable and non-renewable energy resources and how human activities like burning fossil fuels release harmful substances that cause issues like acid rain, smog and ozone depletion.
This chapter section discusses the composition of ocean waters. The oceans originated from early Earth's hot atmosphere that contained water vapor. As the planet cooled, this water condensed into oceans. While the water is ancient, the ocean basins themselves are only around 200 million years old due to plate tectonics. The oceans are salty because they contain dissolved salts and minerals from the erosion of land areas. Salinity, or salt concentration, varies depending on temperature, currents, and freshwater input from rain and melting ice. It is highest in warm, arid areas where evaporation leaves behind salt concentrations.
Benjamin Franklin published a map of the Gulf Stream in the 1700s based on fishermen's and merchants' experiences, in an effort to speed up mail delivery across the Atlantic Ocean when he was the first Postmaster General of the United States. The first global oceanographic cruise for scientific study was made by the British ship HMS Challenger between 1872-1876. This expedition circumnavigated the world, took over 360 ocean depth measurements, collected thousands of biological and sediment samples, and identified over 4,700 new species. Modern techniques for studying the ocean include tools like satellites that map ocean features, sonar for seafloor mapping, and submersibles that can investigate the deepest ocean trenches.
The sphere of water on earth refers to the hydrosphere.
It encompasses all the water present in seas, oceans, lakes, rivers, reservoirs, ice caps, soil moisture, water vapor in the atmosphere and also as groundwater.
Among all these, ocean stands as a principal component of the hydrosphere. About 97 per cent of all the water available on the earth are existing as oceans. This module explains the global seas and oceans.
The document summarizes the 5 oceans of the world: 1) Pacific Ocean is the largest and deepest, located between Asia/Oceania, Americas, and bounded by the Arctic and Southern Oceans. 2) Atlantic Ocean is the second largest with important waterways like the Strait of Gibraltar. 3) Indian Ocean is the third largest located between Africa, Asia, Australia with waterways like the Strait of Malacca. 4) Arctic Ocean is the smallest located around the North Pole with seasonal passageways. 5) Southern Ocean surrounds Antarctica between the Pacific, Atlantic, and Indian Oceans with a narrow Drake Passage.
Australia is located in the southern hemisphere between latitudes 33'57 S and 151'11E. It has a land area of 7.686 million square kilometers and is composed of the Australian mainland as well as over 8,000 smaller islands. The topography is defined by plains, ranges, capes and deserts with the Great Dividing Range being the most significant geographic feature, dividing the coastal and inland zones. Some of the most important physical features include the Great Sandy Desert, Great Victoria Desert, Murray River, and Mount Kosciuszko, which is the highest peak in Australia.
The International Journal of Engineering and Science (The IJES)theijes
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
Keys to paleogeographical interpretation of the enugu and the mamu formations...Alexander Decker
The document analyzes the lithofacies, palynological assemblages, and facies associations of the Enugu and Mamu Formations in southeastern Nigeria to interpret their depositional environments, paleogeography, and ages. Palynological analysis indicates a Late Campanian to Early Maastrichtian age for the Enugu Formation and Early-Mid Maastrichtian age for the Mamu Formation. The coarsening upward lithofacies and decrease in marine dinoflagellates from the Enugu to Mamu Formations suggest shallowing of the sea during regression. Facies associations grade from transgressive in the Enugu to regressive in the Mamu, representing marine transgression and subsequent shore
Granomeric Analysis of Mamu Formation and Enugu Shale around Ozalla and Its E...iosrjce
The study area lies within the Anambra Basin which geologically made up of Enugu Shale and
Mamu Formation. This study aimed at determining the geology and depositional environments of these
Formations through field relationship and grain size distribution as well as morphometric studies. The field
data shows Enugu Shale as fissile, light grey with extraformational clast which graded into Mamu Formation
which is made up of alternating sequence of shale, siltstone, mudstone, coal and sand, it shows a fluctuating
environment. The granulometric study of sand member of Mamu Formation shows characteristic very well
sorted, fine to medium grains which were deposited in relatively turbulent well aerated marine environment
probably above wave base. The bivariate and the multivariate results reveal Aeolian/shallow marine deposit.
The fissility of Enugu Shale suggests that it was deposited in low energy environment, distal to proximal lagoon
environment and the presence of extraformatonal clast indicates fluvial incursion. However, it can be concluded
that Mamu Formation was deposited in fluctuating environment ranging from an oxygenated shallow marine to
acidic swampy environment. Hence is paralic Formation.
This document provides an overview of coal deposits in the Mamu Formation in the Anambra Basin of Nigeria. It discusses the geology, stratigraphy, evolution and paleoenvironmental characteristics of the basin. It also describes the exploration history of coal in the basin, focusing on deposits in the Mamu Formation. Finally, it discusses the economic potential of the coal deposits for combustion, gasification, and liquefaction. Nigeria has over 2 billion tonnes of coal reserves, with about 650 million tonnes proven, primarily located in the Anambra Basin.
The document provides information about the sedimentary basins in Nigeria, focusing on the Benue Trough. It describes the Benue Trough as a major geological formation underlying a large part of Nigeria. It formed as part of the Central African Rift System during the breakup of the supercontinent Gondwana. The trough contains up to 6000m of Cretaceous sediments and is divided into the Lower, Middle, and Upper Benue basins. While exploration has focused on the adjacent Niger Delta Basin, the Benue Trough shows potential for oil and gas discoveries.
Petrography of ajali sandstone in ayogwiri – fugar – orame area of western an...Alexander Decker
- The document analyzes the petrography of the Ajali Sandstone Formation in the Western Anambra Basin of Nigeria to understand its diagenetic and depositional history.
- Thin section analysis shows the sandstone is a quartz arenite composed mainly of subangular to subrounded quartz grains that have undergone compaction, dissolution, alteration, and corrosion during diagenesis. This left the sandstone friable with little cement.
- Samples from three locations - Ayogwiri, Fugar, and Orame - exhibited similar diagenetic features including authigenic quartz, reaction rims, and corroded grain margins. This diagenesis reduced cementation and led to
The Antarctica is centered asymmetrically around the South Pole. It is the southernmost continent in world. The 66 degree 34 minutes south latitude forms the outermost boundary of the Antarctic circle. The area covered within this circle is called as the Antarctic Continent. It includes parts of the Southern ocean, surrounding seas, ice shelves, continental glaciers, plateaus and mountain ranges. The Antarctica is the coldest, driest, and windiest continent, possessing many unique features to learn.
The document summarizes the hydrogeology of Jammu and Kashmir, India. It describes the region's climate, major water bodies, geological formations, and groundwater conditions. The state has varied climates including cold desert in Ladakh, moderate in Kashmir, and sub-tropical in Jammu. Major rivers include the Jhelum, Chenab, and Indus. Groundwater occurs under both confined and unconfined conditions in different areas, with depth to water tables ranging from just below land surface to over 100 meters deep. While groundwater quality is generally suitable for drinking, some areas have high fluoride or nitrate. Overall development of groundwater resources has been limited compared to potential.
The document summarizes the tectonic framework of India in 3 broad divisions - Peninsular India, Extra-Peninsular India, and the Indo-Gangetic Plain. Peninsular India comprises the Indian shield and its sedimentary basins, and is further divided into the shield areas, mobile belts, and Proterozoic sedimentary basins. Extra-Peninsular India includes the Himalayan mountain ranges, divided into the Lesser Himalayan zone, Central Crystalline zone, and Tethyan zone. The Indo-Gangetic Plain is a deep crustal trough in northern India filled with Quaternary sediments.
The Cambay Basin is an intracratonic rift graben located in northwest India that began forming following the Deccan Traps volcanic event in the late Cretaceous. The basin is filled with up to 8km of Tertiary sedimentary rocks. Major source rocks include the thick Cambay Shale deposited in the early Eocene during a transgression. Hydrocarbon reservoirs are found in the Olpad Formation, Hazad delta sands, and Miocene formations. Multiple petroleum plays exist, including those in the Paleocene-early Eocene, middle Eocene, and late Eocene-Oligocene sequences. The Cambay Shale is a prolific source of oil and gas in the
This document summarizes the land relief and water distribution of several continents and regions including:
- Spain, Europe, Africa, America, Asia, and Oceania. For each area, it describes key physical features such as mountain ranges, deserts, peninsulas, rivers, lakes, seas, and their locations. The document provides information on the average altitude and notable geographic characteristics of each region.
Bombay High is an offshore oilfield located 160 km off the coast of Mumbai, India. It was discovered in 1964-1967 and is operated by ONGC. It supplied 14% of India's oil needs and accounted for 38% of domestic production until 2004. The field is located in the Bombay offshore basin and produces from limestone reservoirs of Miocene age. It has produced over 2 billion barrels of oil and 3 trillion cubic feet of gas to date. A major fire in 2005 destroyed the Mumbai High North platform, costing $1.2 billion to rebuild. ONGC continues exploration and production activities in the area through seismic surveys.
The document summarizes the five major oceans of the world: the Pacific Ocean, the largest and deepest ocean located between Asia/Australia and North/South America; the Atlantic Ocean, the second largest located between Europe/Africa/North America; the Indian Ocean, the third largest located between Africa/Asia/Australia; the Arctic Ocean, the smallest located around the North Pole; and the Southern Ocean surrounding Antarctica. Each ocean is briefly described in terms of location, key waterways, climate patterns, ocean floor features, and surface/ice coverage.
There are two peninsulas that branch off Southeast Asia - the Indochinese Peninsula and the Malay Peninsula. This region also contains many archipelagoes, or closely grouped islands, such as the Philippines. It has extensive coastlines and rivers like the Mekong, which forms a wide delta near the coast. The Mekong is also home to the world's largest catfish. Mountains and volcanoes are common due to the region sitting on the ring of fire, with islands evolving over time from volcanoes to coral atolls.
The document provides information on key concepts related to Earth's atmosphere and natural resources. It defines key terms like the layers of the atmosphere, natural resources, and effects of pollution. It describes the troposphere as the lowest layer where weather occurs and the different gas layers above it. It also explains renewable and non-renewable energy resources and how human activities like burning fossil fuels release harmful substances that cause issues like acid rain, smog and ozone depletion.
This chapter section discusses the composition of ocean waters. The oceans originated from early Earth's hot atmosphere that contained water vapor. As the planet cooled, this water condensed into oceans. While the water is ancient, the ocean basins themselves are only around 200 million years old due to plate tectonics. The oceans are salty because they contain dissolved salts and minerals from the erosion of land areas. Salinity, or salt concentration, varies depending on temperature, currents, and freshwater input from rain and melting ice. It is highest in warm, arid areas where evaporation leaves behind salt concentrations.
Benjamin Franklin published a map of the Gulf Stream in the 1700s based on fishermen's and merchants' experiences, in an effort to speed up mail delivery across the Atlantic Ocean when he was the first Postmaster General of the United States. The first global oceanographic cruise for scientific study was made by the British ship HMS Challenger between 1872-1876. This expedition circumnavigated the world, took over 360 ocean depth measurements, collected thousands of biological and sediment samples, and identified over 4,700 new species. Modern techniques for studying the ocean include tools like satellites that map ocean features, sonar for seafloor mapping, and submersibles that can investigate the deepest ocean trenches.
The sphere of water on earth refers to the hydrosphere.
It encompasses all the water present in seas, oceans, lakes, rivers, reservoirs, ice caps, soil moisture, water vapor in the atmosphere and also as groundwater.
Among all these, ocean stands as a principal component of the hydrosphere. About 97 per cent of all the water available on the earth are existing as oceans. This module explains the global seas and oceans.
The document summarizes the 5 oceans of the world: 1) Pacific Ocean is the largest and deepest, located between Asia/Oceania, Americas, and bounded by the Arctic and Southern Oceans. 2) Atlantic Ocean is the second largest with important waterways like the Strait of Gibraltar. 3) Indian Ocean is the third largest located between Africa, Asia, Australia with waterways like the Strait of Malacca. 4) Arctic Ocean is the smallest located around the North Pole with seasonal passageways. 5) Southern Ocean surrounds Antarctica between the Pacific, Atlantic, and Indian Oceans with a narrow Drake Passage.
Australia is located in the southern hemisphere between latitudes 33'57 S and 151'11E. It has a land area of 7.686 million square kilometers and is composed of the Australian mainland as well as over 8,000 smaller islands. The topography is defined by plains, ranges, capes and deserts with the Great Dividing Range being the most significant geographic feature, dividing the coastal and inland zones. Some of the most important physical features include the Great Sandy Desert, Great Victoria Desert, Murray River, and Mount Kosciuszko, which is the highest peak in Australia.
This document provides information about the land relief and water distribution of different continents and regions including Spain, Europe, Africa, America, and Asia. It describes key physical features such as mountain ranges, plateaus, peninsulas, islands, rivers, lakes, seas, gulfs, straits, deserts, and plains. For each region or continent, it lists the major landforms and bodies of water and their locations.
Antarctica is covered almost entirely by ice and has few distinguishing physical features. The continent is dominated by the Antarctic ice sheet which covers over 99% of its land area. The only exposed land lies along the coasts, which are fringed by ice shelves. The largest of these ice shelves is the Ross Ice Shelf. Within the continent are also the Transantarctic Mountains and a large plateau.
Plates and list of all major and minor plates in the worldTahsin Islam Ornee
The definition of plates, Earth's interior, Boundaries and the list of the major and minor plates are included in the presentation with images, videos and information.
Antarctica is located inside the Antarctic Circle. As a result, almost its entire surface is covered by ice. This continent is made up of many islands and a large continental mass with a large plateau and the Transantarctic Mountains, which include Mount Vison at 5,140 meters.
The document provides information about an upcoming geography exam, including:
- The exam has 3 parts: multiple choice, short answer, and extended answer
- Part A has 20 multiple choice questions worth 1 mark each
- Part B has short answer and diagram questions worth 20 marks total
- Part C has 3 extended answer sections with 2 questions each, and students must choose 1 question from each section
- The exam covers various geography topics studied in class
1 10 ocean composition-location Water in Earth’s Processesaalleyne
Water in Earth’s Processes
S6E3. Students will recognize the significant role of water in earth processes.
c. Describe the composition, location, and subsurface topography of the world’s oceans.
The document discusses two island groups of India - the Lakshadweep Islands and the Andaman and Nicobar Islands. The Lakshadweep Islands are a group of 36 coral islands located in the Arabian Sea, off the coast of Kerala. They have a total land area of 32 square kilometers. The Andaman and Nicobar Islands are located in the Bay of Bengal and comprise over 570 islands, of which around 38 are permanently inhabited. India's only active volcano is located on Barren Island in the Andaman and Nicobar Islands. Both island groups are known for their natural beauty and biodiversity.
Australasia includes Australia, New Zealand, and surrounding islands. The region has diverse geography, including deserts, forests, and mountain ranges. Australia and New Zealand have developed economies based around agriculture, mining, and services. Major cities include Sydney, Melbourne, Brisbane, Perth, Adelaide, Auckland, Wellington, Christchurch and their populations are primarily concentrated along the coasts. The climate varies from tropical to temperate but natural disasters like floods and earthquakes occasionally occur. Tourism is an important industry focused on the natural scenery and environments.
This document provides an overview of the physical geography, climate, and human-environment interactions of Southeast Asia, Oceania, and Antarctica. It describes the varied landforms and climates of the region, from tropical islands and coasts to inland deserts and the Antarctic ice sheet. Pacific Islanders developed advanced seafaring and navigation to settle the far-flung Pacific, while European colonization introduced invasive species like rabbits and nuclear testing contaminated Pacific atolls. The region exhibits extremes from volcanic tropics to polar ice, with human activities both benefiting and damaging the environment.
The document discusses the waters of the Earth, including the oceans and ocean floor. It describes the five oceans - Pacific, Atlantic, Indian, Arctic, and Antarctic oceans. It also discusses ocean resources like food, minerals, and fossil fuels. The ocean floor is described as having different layers like basalt and granite. Features of the ocean floor include ridges, seamounts, and trenches, with the deepest being the Marianas Trench.
Similar to Oceanography: Ocean floor of the World (20)
ESPP presentation to EU Waste Water Network, 4th June 2024 “EU policies driving nutrient removal and recycling
and the revised UWWTD (Urban Waste Water Treatment Directive)”
Remote Sensing and Computational, Evolutionary, Supercomputing, and Intellige...University of Maribor
Slides from talk:
Aleš Zamuda: Remote Sensing and Computational, Evolutionary, Supercomputing, and Intelligent Systems.
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Inter-Society Networking Panel GRSS/MTT-S/CIS Panel Session: Promoting Connection and Cooperation
https://www.etran.rs/2024/en/home-english/
When I was asked to give a companion lecture in support of ‘The Philosophy of Science’ (https://shorturl.at/4pUXz) I decided not to walk through the detail of the many methodologies in order of use. Instead, I chose to employ a long standing, and ongoing, scientific development as an exemplar. And so, I chose the ever evolving story of Thermodynamics as a scientific investigation at its best.
Conducted over a period of >200 years, Thermodynamics R&D, and application, benefitted from the highest levels of professionalism, collaboration, and technical thoroughness. New layers of application, methodology, and practice were made possible by the progressive advance of technology. In turn, this has seen measurement and modelling accuracy continually improved at a micro and macro level.
Perhaps most importantly, Thermodynamics rapidly became a primary tool in the advance of applied science/engineering/technology, spanning micro-tech, to aerospace and cosmology. I can think of no better a story to illustrate the breadth of scientific methodologies and applications at their best.
Unlocking the mysteries of reproduction: Exploring fecundity and gonadosomati...AbdullaAlAsif1
The pygmy halfbeak Dermogenys colletei, is known for its viviparous nature, this presents an intriguing case of relatively low fecundity, raising questions about potential compensatory reproductive strategies employed by this species. Our study delves into the examination of fecundity and the Gonadosomatic Index (GSI) in the Pygmy Halfbeak, D. colletei (Meisner, 2001), an intriguing viviparous fish indigenous to Sarawak, Borneo. We hypothesize that the Pygmy halfbeak, D. colletei, may exhibit unique reproductive adaptations to offset its low fecundity, thus enhancing its survival and fitness. To address this, we conducted a comprehensive study utilizing 28 mature female specimens of D. colletei, carefully measuring fecundity and GSI to shed light on the reproductive adaptations of this species. Our findings reveal that D. colletei indeed exhibits low fecundity, with a mean of 16.76 ± 2.01, and a mean GSI of 12.83 ± 1.27, providing crucial insights into the reproductive mechanisms at play in this species. These results underscore the existence of unique reproductive strategies in D. colletei, enabling its adaptation and persistence in Borneo's diverse aquatic ecosystems, and call for further ecological research to elucidate these mechanisms. This study lends to a better understanding of viviparous fish in Borneo and contributes to the broader field of aquatic ecology, enhancing our knowledge of species adaptations to unique ecological challenges.
Immersive Learning That Works: Research Grounding and Paths ForwardLeonel Morgado
We will metaverse into the essence of immersive learning, into its three dimensions and conceptual models. This approach encompasses elements from teaching methodologies to social involvement, through organizational concerns and technologies. Challenging the perception of learning as knowledge transfer, we introduce a 'Uses, Practices & Strategies' model operationalized by the 'Immersive Learning Brain' and ‘Immersion Cube’ frameworks. This approach offers a comprehensive guide through the intricacies of immersive educational experiences and spotlighting research frontiers, along the immersion dimensions of system, narrative, and agency. Our discourse extends to stakeholders beyond the academic sphere, addressing the interests of technologists, instructional designers, and policymakers. We span various contexts, from formal education to organizational transformation to the new horizon of an AI-pervasive society. This keynote aims to unite the iLRN community in a collaborative journey towards a future where immersive learning research and practice coalesce, paving the way for innovative educational research and practice landscapes.
Phenomics assisted breeding in crop improvementIshaGoswami9
As the population is increasing and will reach about 9 billion upto 2050. Also due to climate change, it is difficult to meet the food requirement of such a large population. Facing the challenges presented by resource shortages, climate
change, and increasing global population, crop yield and quality need to be improved in a sustainable way over the coming decades. Genetic improvement by breeding is the best way to increase crop productivity. With the rapid progression of functional
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Authoring a personal GPT for your research and practice: How we created the Q...Leonel Morgado
Thematic analysis in qualitative research is a time-consuming and systematic task, typically done using teams. Team members must ground their activities on common understandings of the major concepts underlying the thematic analysis, and define criteria for its development. However, conceptual misunderstandings, equivocations, and lack of adherence to criteria are challenges to the quality and speed of this process. Given the distributed and uncertain nature of this process, we wondered if the tasks in thematic analysis could be supported by readily available artificial intelligence chatbots. Our early efforts point to potential benefits: not just saving time in the coding process but better adherence to criteria and grounding, by increasing triangulation between humans and artificial intelligence. This tutorial will provide a description and demonstration of the process we followed, as two academic researchers, to develop a custom ChatGPT to assist with qualitative coding in the thematic data analysis process of immersive learning accounts in a survey of the academic literature: QUAL-E Immersive Learning Thematic Analysis Helper. In the hands-on time, participants will try out QUAL-E and develop their ideas for their own qualitative coding ChatGPT. Participants that have the paid ChatGPT Plus subscription can create a draft of their assistants. The organizers will provide course materials and slide deck that participants will be able to utilize to continue development of their custom GPT. The paid subscription to ChatGPT Plus is not required to participate in this workshop, just for trying out personal GPTs during it.
EWOCS-I: The catalog of X-ray sources in Westerlund 1 from the Extended Weste...Sérgio Sacani
Context. With a mass exceeding several 104 M⊙ and a rich and dense population of massive stars, supermassive young star clusters
represent the most massive star-forming environment that is dominated by the feedback from massive stars and gravitational interactions
among stars.
Aims. In this paper we present the Extended Westerlund 1 and 2 Open Clusters Survey (EWOCS) project, which aims to investigate
the influence of the starburst environment on the formation of stars and planets, and on the evolution of both low and high mass stars.
The primary targets of this project are Westerlund 1 and 2, the closest supermassive star clusters to the Sun.
Methods. The project is based primarily on recent observations conducted with the Chandra and JWST observatories. Specifically,
the Chandra survey of Westerlund 1 consists of 36 new ACIS-I observations, nearly co-pointed, for a total exposure time of 1 Msec.
Additionally, we included 8 archival Chandra/ACIS-S observations. This paper presents the resulting catalog of X-ray sources within
and around Westerlund 1. Sources were detected by combining various existing methods, and photon extraction and source validation
were carried out using the ACIS-Extract software.
Results. The EWOCS X-ray catalog comprises 5963 validated sources out of the 9420 initially provided to ACIS-Extract, reaching a
photon flux threshold of approximately 2 × 10−8 photons cm−2
s
−1
. The X-ray sources exhibit a highly concentrated spatial distribution,
with 1075 sources located within the central 1 arcmin. We have successfully detected X-ray emissions from 126 out of the 166 known
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Or: Beyond linear.
Abstract: Equivariant neural networks are neural networks that incorporate symmetries. The nonlinear activation functions in these networks result in interesting nonlinear equivariant maps between simple representations, and motivate the key player of this talk: piecewise linear representation theory.
Disclaimer: No one is perfect, so please mind that there might be mistakes and typos.
dtubbenhauer@gmail.com
Corrected slides: dtubbenhauer.com/talks.html
6. Atlantic Ocean Floor
- S-shaped ridge in the middle of the
ocean.
- Atlantic ocean occupies 1/6th
part of
total earth surface.
- Continental Shelf is narrow along
S.Atlantic , broad along USA, UK,
Argentina.
other ridges are :-
1.Dolphine ridge / rise- N.Atlantic
2.Challenger ridge / rise – S.Atlantic
3.Walvis ridge / rise
4.Rio Grande rise/ ridge
Ocean Basins / Abyssal Plains :-
a.Labrador basin
b.NW Atlantic – largest in extent
c.Cape Verde basin
d.Brazil basin
e.Argentina
f.Agulas basin
1
2 3
4
b
c
a
d
e f
iii
ii
i
7. Ocean Deeps/ Trenches:-
i. Peuto Rico deep (8660 m)
ii. South Sandwich (7881 m)
iii. Romanche Trench (7254 m) –
cuts and divides dalphin and
challenger rise.
--------------------------------------------------
• small seas – Carribean sea,
North sea, Mediterranean sea,
Hudson bay, English
channel,etc.
• --------------------------------------------
-----
• Lack of islands
• New Folkland (famous for foggy
weather , fog is formed due to
mixing of Brazilian warm and
Antarctic cold ocean current)
and British Isles
• Carribean / West Indies islands.
9. other ridges :-
- Very few ridges/ rise
1. East Pacific ridge
2. Macquaries ridge
3.Hawaiin rise
4.Aleutian rise
Ocean Basins / Abyssal Plains along
with plateaus:-
a.Aleutian basin/ plain
b.Philippine
c.Fiji
d.W and E Caroline abyssal plain
e.Tasmanian basin
f.SW Pacific basin
Ocean Deeps/ Trenches:-
Total 32 deeps alone in pacific
i.Mariana/ Nero Trench(11,030m)
ii.Aleutian
iii.Kurile and Japan Trench
iv.Tonga- Kermadac
v.Peru- Chile Trench
1
2
4
3
10. PACIFIC OCEAN FLOOR
• Cover 33% of earth’s total surface..
• Roughly triangular in shape
• Bordered by – N. S. America towards east
- Eurasia and Australia towards west
• length :- 14,900 km and width :- 16,000 km
• Average depth – ~5000m
•Its divided into 4 parts :-
1.N Pacific - deepest part of the world
2.Central P. - famous for corals and volcanic islands – max in world.
3.SW P. - Trenches are max. Shelves are broadest- fishing ground
4.SE P. - Submarine ridges and plateau
Continental Shelf :- Easter margin is narrow due to Rockies – Andies
Western margin is broad
average width ~ 160-1600km
on these shelves lies islands and seas.
11. INDIAN OCEAN
- Warm ocean covering 20%
Of total earth’s surface.
-The Indian Ocean is
bounded on the north by
Asia; on the west by Africa;
on the east by Australia; and
on the south by Antarctica.
Shape is compact, bold and
with regular.
- Average depth – 4000m
-Continental Shelf :-
-Width is varying and not
specific. Average- 96 km
- Generally narrow along
Sumatra and Australia ,
-but wider near Bay of
Bengal, African coast.
- Narrowest along Antarctica
13. INDIAN OCEAN
Ridges and basins :-
A. It has continuous Central ridge called ‘Arabian- Indian ridge’ – bifurcated into many
ridges separating Indian Sub-continent, Africa, Antarctica .e.g.
B.East –Indian/ Ninety East ridge,
C.Madagascar ridge,
D.Socorta-Chagos ridge,
E.Kerguelen- Gaussberg ridge – connected to Antarctica continent.
F.South East Indian Ridge
Ocean basin / Abyssal plain :-
Central Ridge divides abyssal plains into various basins (~ 4000 – 6000 m) almost
50% of Indian Ocean is covered by plains.
1.Oman basin
2.Arabian extends as-
3.Socorta - Chagos ridge
4.Somali basin
5.Mauritius / Madagascar plain
6.Natal plain
7.Kerguelen plain
8.Anadaman basin
9.Cocos plain/ basin 9a. Ceylon plain
Ocean Deeps/ Trenches :- almost absent
Sunda Trench (450 m), Nicobar Trench
14.
15.
16.
17.
18. PROCESSES OF HEATING
Major Minor
1. Absorption of insolation Transformation of kinetic energy
into heat energy.
2. Conventional current formation
due to internal heat of earth
heating of water due to Chemical
processes
Condensation of water vapour
19. FACTORS AFFECTING THE DISTRIBUTION OF
SEA WATER TEMPERTURE
1.Intensity and daily duration of solar energy.
2.The depletion of this energy in the atmosphere by – reflection,
scattering, absorption.
3.Heat balance/ budget
4.Latitudes ( seasonal variation, insolation, land –sea distribution)
5.Ocean currents
6.Prevailing winds ( landlocked seas get highly affected)
7.Local weather (land –sea breezes, vegetation cover, land use)
8.Seepage of nuclear power plants (anthropogenic effect)
20. Horizontal Distribution of Sea-water Temperature (latitudial)
26.80
C
25.6
23.9
12.9
20.3
8.9
4.3
-1.4
The surface water temperature varies
according to angle of
Sunrays & latitudes.
avrg. Temp. = 26.80
C
may increase upto
300
C in summer.
Prevailing winds
are responsible
to drive the
water-warm
or cold.
thus ocean currents/ drifts
brings warm currents
from equator , cold currents
from poles.
Local weather also affects
the distribution and properties
of ocean currents.
--- Thus, Water surface temp. decreases from equator towards poles