The Horse Lava Tube System (or Horse system) is a series of lava tubes within Deschutes County, Oregon, of the United States. The system starts within the Deschutes National Forest on the northern flank of Newberry Volcano and heads north into and near the city of Bend. The system continues north to Redmond and includes the Redmond Caves. The flow diverts into the Redmond Dry Canyon, where the last known segment is known to exist; however, the basalt flow that created the system goes beyond to Crooked River Ranch and terminates just short of the Crooked River Gorge. The lava flow that created the Horse system is also referred to as the Horse Cave lobe and it filled the ancient channel of the Deschutes River which at that time flowed around the east side of Pilot Butte. The Horse Cave lobe
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- Horse Lava Tube System (fr)
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| - The Horse Lava Tube System (or Horse system) is a series of lava tubes within Deschutes County, Oregon, of the United States. The system starts within the Deschutes National Forest on the northern flank of Newberry Volcano and heads north into and near the city of Bend. The system continues north to Redmond and includes the Redmond Caves. The flow diverts into the Redmond Dry Canyon, where the last known segment is known to exist; however, the basalt flow that created the system goes beyond to Crooked River Ranch and terminates just short of the Crooked River Gorge. The lava flow that created the Horse system is also referred to as the Horse Cave lobe and it filled the ancient channel of the Deschutes River which at that time flowed around the east side of Pilot Butte. The Horse Cave lobe (en)
- Le Horse Lava Tube System (ou Horse system) est une série de tunnels de lave situés dans le comté de Deschutes, dans l'Oregon, aux États-Unis. Le système commence dans la forêt nationale de Deschutes sur le flanc nord du cratère Newberry et se dirige vers le nord en direction et près de la ville de Bend. Le système continue vers le nord jusqu'à Redmond aux (en) et dans le Redmond Canyon, où l'on sait que le dernier segment connu existe ; cependant, la coulée de basalte qui a créé le système va au-delà jusqu'à (en) et se termine juste avant la gorge de la rivière Crooked. La coulée de lave qui a créé le Horse system est également appelée le Horse Cave lobe et elle a rempli l'ancien canal de la rivière Deschutes qui, à l'époque, coulait autour du côté est de Pilot Butte. Le lobe de Horse C (fr)
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| - Horse Lava Tube System (en)
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| - Horse Lava Tube System (en)
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| - Deschutes County, Oregon, United States (en)
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| - Vulture Cave of the Horse Lava Tube System.jpg (en)
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| - Vulture Cave of the Horse Lava Tube System (en)
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| - The Horse Lava Tube System (or Horse system) is a series of lava tubes within Deschutes County, Oregon, of the United States. The system starts within the Deschutes National Forest on the northern flank of Newberry Volcano and heads north into and near the city of Bend. The system continues north to Redmond and includes the Redmond Caves. The flow diverts into the Redmond Dry Canyon, where the last known segment is known to exist; however, the basalt flow that created the system goes beyond to Crooked River Ranch and terminates just short of the Crooked River Gorge. The lava flow that created the Horse system is also referred to as the Horse Cave lobe and it filled the ancient channel of the Deschutes River which at that time flowed around the east side of Pilot Butte. The Horse Cave lobe is a part of the basalt of Lava Top Butte which also consists of the Arnold Lava Tube System, the Badlands rootless shield, and the Lava Top butte basalt. All have a geologic age around 80,000 years old. (en)
- Le Horse Lava Tube System (ou Horse system) est une série de tunnels de lave situés dans le comté de Deschutes, dans l'Oregon, aux États-Unis. Le système commence dans la forêt nationale de Deschutes sur le flanc nord du cratère Newberry et se dirige vers le nord en direction et près de la ville de Bend. Le système continue vers le nord jusqu'à Redmond aux (en) et dans le Redmond Canyon, où l'on sait que le dernier segment connu existe ; cependant, la coulée de basalte qui a créé le système va au-delà jusqu'à (en) et se termine juste avant la gorge de la rivière Crooked. La coulée de lave qui a créé le Horse system est également appelée le Horse Cave lobe et elle a rempli l'ancien canal de la rivière Deschutes qui, à l'époque, coulait autour du côté est de Pilot Butte. Le lobe de Horse Cave fait partie du basalte de la butte Lava Top, qui comprend également le (en), le bouclier sans racines Badlands et le basalte de la butte Lava Top, tous ayant un âge géologique d'environ 80 000 ans. (fr)
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