Search results for Cite

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Ile Saint-Louis, is one of two natural islands in the Seine river, in Paris, France. The island is named after King Louis IX of France (Saint Louis). The island is connected to the rest of Paris by bridges to both banks of the river and by the Pont Saint Louis to the Ile de la Cite
Ile Saint-Louis, is one of two natural islands in the Seine river, in Paris, France. The island is named after King Louis IX of France (Saint Louis). The island is connected to the rest of Paris by bridges to both banks of the river and by the Pont Saint Louis to the Ile de la Cite.
Location: Ile Saint-Louis, Paris, France
Image ID: 28245  
Ile Saint-Louis, is one of two natural islands in the Seine river, in Paris, France. The island is named after King Louis IX of France (Saint Louis). The island is connected to the rest of Paris by bridges to both banks of the river and by the Pont Saint Louis to the Ile de la Cite
Ile Saint-Louis, is one of two natural islands in the Seine river, in Paris, France. The island is named after King Louis IX of France (Saint Louis). The island is connected to the rest of Paris by bridges to both banks of the river and by the Pont Saint Louis to the Ile de la Cite.
Location: Ile Saint-Louis, Paris, France
Image ID: 28253  
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris.
Location: Notre Dame de Paris, France
Image ID: 28255  
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris.
Location: Notre Dame de Paris, France
Image ID: 28257  
La Sainte-Chapelle, The Holy Chapel, is one of the only surviving buildings of the Capetian royal palace on the Ile de la Cite in the heart of Paris, France. It was commissioned by King Louis IX of France to house his collection of Passion Relics, including the Crown of Thorns - one of the most important relics in medieval Christendom
La Sainte-Chapelle, The Holy Chapel, is one of the only surviving buildings of the Capetian royal palace on the Ile de la Cite in the heart of Paris, France. It was commissioned by King Louis IX of France to house his collection of Passion Relics, including the Crown of Thorns - one of the most important relics in medieval Christendom.
Location: La Sainte-Chapelle, Paris, France
Image ID: 28033  
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris.
Location: Notre Dame de Paris, France
Image ID: 28128  
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris.
Location: Notre Dame de Paris, France
Image ID: 28129  
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris
Notre Dame de Paris. Notre Dame de Paris ("Our Lady of Paris"), also known as Notre Dame Cathedral or simply Notre Dame, is a historic Roman Catholic Marian cathedral on the eastern half of the Ile de la Cite in the fourth arrondissement of Paris, France. Widely considered one of the finest examples of French Gothic architecture and among the largest and most well-known churches in the world ever built, Notre Dame is the cathedral of the Catholic Archdiocese of Paris.
Location: Notre Dame de Paris, France
Image ID: 28130  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12514  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12515  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12516  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12517  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12518  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12520  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12521  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12522  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12523  
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12524  
Checkerboard Mesa, a good example of crossbedding (horizontal lines) and vertical cracks caused by thermal expansion/contraction. Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone
Checkerboard Mesa, a good example of crossbedding (horizontal lines) and vertical cracks caused by thermal expansion/contraction. Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12526  
Visitors admire the Pipe Organ formation of calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
Visitors admire the Pipe Organ formation of calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09910  
Visitors admire the Pipe Organ formation of calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
Visitors admire the Pipe Organ formation of calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09911  
The Pipe Organ, a formation of calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
The Pipe Organ, a formation of calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09912  
The Pipe Organ, a formation of calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
The Pipe Organ, a formation of calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09913  
The Pipe Organ, a formation of calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
The Pipe Organ, a formation of calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09914  
Calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09915  
Calcite flowstone and cave curtains, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite flowstone and cave curtains.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09916  
Calcite stalactites hanging from above have joined with stalagmites growing on the cave floor to form a solid column, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite stalactites hanging from above have joined with stalagmites growing on the cave floor to form a solid column.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09922  
Calcite stalactites and stalagmites, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite stalactites and stalagmites.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09923  
Calcite stalactites and stalagmites, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite stalactites and stalagmites.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09924  
Calcite stalactites and stalagmites, Crystal Cave, Sequoia Kings Canyon National Park, California
Calcite stalactites and stalagmites.
Location: Crystal Cave, Sequoia Kings Canyon National Park, California
Image ID: 09925  
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