SKU: KJ.SO165F
Composer/Arranger Doris Gazda discovered a beautiful Mexican song Saludo A Santo San Francisco while visiting the San Xavier Mission located south of Tucson, Arizona. This mission serves as an active church on a reservation, yet is also a museum that attracts thousands of tourists each year. This arrangement is in the key of G minor and is in 6/8 time. A harp part is included.
SKU: CF.CAS7
ISBN 9780825847578. UPC: 798408047573. 8.5 X 11 inches. Key: D major.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista.The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color.Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
SKU: CF.CAS3
ISBN 9780825844881. UPC: 798408044886. 8.5 X 11 inches. Key: D major.
A copse is a thicket of trees and bushes that may be found in a meadow or in open land. In England, a copse will often be found on a moor. A copse needs a source of water that is usually a stream, small river or pond. A copse has abundant plant and animal life because it provides the perfect habitat and shelter for moisture loving plants, insects, small mammals, rodents, reptiles, and birds. If you were walking through the copse in the midst of willow trees, bluebells and march marigolds, you would see beautiful butterflies, dragonflies and moths. You might see a frog or toad jumping on the banks of the pond and you would hear the call of numerous birds. Ornithologists often spend many hours watching and counting birds in and around a copse. Migrating birds such as geese and herons may also be spotted at certain times of the year. If you sit very quietly, you might catch sight of a red fox, a rabbit or squirrel. A copse is a happy place to spend an afternoon or to go for a walk. Perhaps you will get to visit a nature preserve near your home where you can observe the wonderful world of the woodland wild life that can be found in abundance in a copse. To assist you in learning some of the techniques that you need to be able to use when playing Willow-Wood Copse, you may wish to work on the studies that accompany the piece.A copse is a thicket of trees and bushes that may be found in a meadow or in open land. In England, a copse will often be found on a moor. A copse needs a source of water that is usually a stream, small river or pond. A copse has abundant plant and animal life because it provides the perfect habitat and shelter for moisture loving plants, insects, small mammals, rodents, reptiles, and birds. If you were walking through the copse in the midst of willow trees, bluebells and march marigolds, you would see beautiful butterflies, dragonflies and moths. You might see a frog or toad jumping on the banks of the pond and you would hear the call of numerous birds. Ornithologists often spend many hours watching and counting birds in and around a copse. Migrating birds such as geese and herons may also be spotted at certain times of the year. If you sit very quietly, you might catch sight of a red fox, a rabbit or squirrel. A copse is a happy place to spend an afternoon or to go for a walk. Perhaps you will get to visit a nature preserve near your home where you can observe the wonderful world of the woodland wild life that can be found in abundance in a copse. To assist you in learning some of the techniques that you need to be able to use when playingA Willow-Wood Copse, you may wish to work on the studies that accompany the piece.A copse is a thicket of trees and bushes that may be found in a meadow or in open land. In England, a copse will often be found on a moor. A copse needs a source of water that is usually a stream, small river or pond. A copse has abundant plant and animal life because it provides the perfect habitat and shelter for moisture loving plants, insects, small mammals, rodents, reptiles, and birds. If you were walking through the copse in the midst of willow trees, bluebells and march marigolds, you would see beautiful butterflies, dragonflies and moths. You might see a frog or toad jumping on the banks of the pond and you would hear the call of numerous birds. Ornithologists often spend many hours watching and counting birds in and around a copse. Migrating birds such as geese and herons may also be spotted at certain times of the year. If you sit very quietly, you might catch sight of a red fox, a rabbit or squirrel. A copse is a happy place to spend an afternoon or to go for a walk. Perhaps you will get to visit a nature preserve near your home where you can observe the wonderful world of the woodland wild life that can be found in abundance in a copse. To assist you in learning some of the techniques that you need to be able to use when playing Willow-Wood Copse, you may wish to work on the studies that accompany the piece.A copse is a thicket of trees and bushes that may be found in a meadow or in open land. In England, a copse will often be found on a moor. A copse needs a source of water that is usually a stream, small river or pond. A copse has abundant plant and animal life because it provides the perfect habitat and shelter for moisture loving plants, insects, small mammals, rodents, reptiles, and birds.If you were walking through the copse in the midst of willow trees, bluebells and march marigolds, you would see beautiful butterflies, dragonflies and moths. You might see a frog or toad jumping on the banks of the pond and you would hear the call of numerous birds. Ornithologists often spend many hours watching and counting birds in and around a copse. Migrating birds such as geese and herons may also be spotted at certain times of the year. If you sit very quietly, you might catch sight of a red fox, a rabbit or squirrel.A copse is a happy place to spend an afternoon or to go for a walk. Perhaps you will get to visit a nature preserve near your home where you can observe the wonderful world of the woodland wild life that can be found in abundance in a copse.To assist you in learning some of the techniques that you need to be able to use when playing Willow-Wood Copse, you may wish to work on the studies that accompany the piece.
SKU: FJ.ST6396S
English.
The bittersweet longing for a love across cultural boundaries begins this visit to Ireland with The Flower of Magherally and solo opportunities for your principal violist. A boisterous slip jig in 9/8 meter gives all students a workout with a variety of bowings and styles both on and off the string.
About FJH String Orchestra
More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up
SKU: KJ.SO76F
3Christmas Reflections is an arrangement of three Christmas carols. The first carol, The Friendly Beasts, is a traditional English carol. It is based on an old belief that farm animals receive the gift of speech at midnight on Christmas eve. The second carol is a traditional carol from Austria. As Lately We Watched is a description of the nativity scene as observed by shepherds guarding their flocks. The third carol in the arrangement, O Come Little Children, was written by German composer, J. A. P. Schulz (1747-1800). Schulz studied music in Berlin and was a prolific composer of sacred vocal music. He also composed operettas, instrumental works, and various piano pieces. The carol is an invitation for all people, especially children, to visit the nativity.
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