SKU: KJ.SO389F
UPC: 8402704821.
Serenade for Strings, Op. 22, First Movement is presented in its entirety in G Major, making it wonderfully accessible to less advanced ensembles. A staple in classical string orchestra literature, this is not to be missed! This Woolstenhulme arrangement belongs in all school libraries.
SKU: KJ.SO393C
UPC: 8402704886.
SKU: KN.9461
UPC: 822795094619.
Brimming with intrigue and suspense, this exciting marriage of themes from The Barber of Seville with an iconic shark in the water motive will keep everyone on the edge of their seat. All Seville themes have been expertly adjusted for young students, and all recurring shark figures are well-fingered and easy to teach. A compelling thriller from start to finish! Duration 3:30.Instrumentation: standard string orchestra (88555) with opt. 3rd Violin/Viola TC (3) and piano.
SKU: KN.KAS2201
12 x 9 inches.
SKU: CF.YAS15
ISBN 9780825851995. UPC: 798408051990. 8.5 X 11 inches. Key: D minor.
Lower strings be sure to maintain a steady pulse and dont rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 121. If the soloist is comfortable using third position, play mm. 119 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.Lower strings be sure to maintain a steady pulse and donat rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1a21. If the soloist is comfortable using third position, play mm. 1a19 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.Lower strings be sure to maintain a steady pulse and don't rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1-21. If the soloist is comfortable using third position, play mm. 1-19 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.Lower strings be sure to maintain a steady pulse and don’t rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1–21. If the soloist is comfortable using third position, play mm. 1–19 and the first half of m. 20 one octave higher.All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance.String editing by Amy Rosen.
About Carl Fischer Young String Orchestra Series
This series of Grade 2/Grade 2.5 pieces is designed for second and third year ensembles. The pieces in this series are characterized by:--Occasionally extending to third position--Keys carefully considered for appropriate difficulty--Addition of separate 2nd violin and viola parts--Viola T.C. part included--Increase in independence of parts over beginning levels
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.YAS41
ISBN 9780825861291. UPC: 798408061296. 8.5 X 11 inches. Key: G major.
Larry Clark does it again with this tuneful new feel good piece. You and your students will walk away humming this tune. There is even a nice contrasting lyrical middle section in the relative minor to break up the piece.Solstice: one of two times in the year when the sun is at its greatest distancefrom the celestial equator.A solstice happens at the mid-point of summer, about June 21, and the midpoint of winter, about December 22. Each of those times of year is delightful. The carefree days of summer have just begun around June 21, when the mind wanders to long bike rides or walks on the beach. During the winter solstice the mind is filled with all of the delights that the holiday season has to offer. Either way, a solstice is a joyous and fun filled time of year, and this piece is intended to bring to mind some of these wonderful times. The main theme should be performed in a light carefree manner, which is then contrasted by the more lyrical and passionate middle section.As with all of my pieces for younger students, the tempo indicated is merely a guide. Adjust the tempo to fit the needs of your students. It has been my pleasure to have the opportunity to write this piece. I hope you and your students enjoy it and find it useful for your program.
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