SKU: KJ.SO326F
UPC: 8402703955.
Take a trip to beautiful Canada with this sensational three-movement work. Each movement is richly scored and showcases each section with key thematic material. Specially selected movements are: Vive la Canadienne!, An Emigrant's Daughter, and Northland Frolic (I'se the Bye & The Mouth of the Tobique).
SKU: KJ.SO326C
UPC: 8402703953.
SKU: CF.BAS5
ISBN 9780825845086. UPC: 798408045081. 8.5 X 11 inches. Key: D major.
The musical effect of Prarie Lullaby should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close to p as possible. Beginning at m.39, the violin and viola parts are marked pizzicato. If young players are unable to return quickly to argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score. The divisi notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes. Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead. The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54. Performance time with the repeat is two and a half minutes.The musical effect ofA Prarie LullabyA should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close toA p as possible. Beginning at m.39, the violin and viola parts are markedA pizzicato. If young players are unable to return quickly toA argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score. TheA divisiA notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes. Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead. The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54. Performance time with the repeat is two and a half minutes.The musical effect ofA Prarie LullabyA should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close toA p as possible. Beginning at m.39, the violin and viola parts are markedA pizzicato. If young players are unable to return quickly toA argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score. TheA divisiA notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes. Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead. The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54. Performance time with the repeat is two and a half minutes.The musical effect of Prarie Lullaby should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close to p as possible. Beginning at m.39, the violin and viola parts are marked pizzicato. If young players are unable to return quickly to argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score. The divisi notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes. Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead. The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54. Performance time with the repeat is two and a half minutes.The musical effect of Prarie Lullaby should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close to p as possible. Beginning at m.39, the violin and viola parts are marked pizzicato. If young players are unable to return quickly to argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score. The divisi notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes. Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead. The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54. Performance time with the repeat is two and a half minutes.The musical effect of Prarie Lullaby should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close to p as possible.Beginning at m.39, the violin and viola parts are marked pizzicato. If young players are unable to return quickly to argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score.The divisi notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes.Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead.The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54.Performance time with the repeat is two and a half minutes.
About Carl Fischer Beginning String Orchestra Series
This series of Grade 1 pieces is designed for first year string groups. The pieces in this series are characterized by:
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.
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