SKU: CF.FAS21

ISBN 9780825853067. UPC: 798408053062. 8.5 X 11 inches. Key: B minor.

Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece. As with all of my pieces at this level, the tempo is merely a suggestion and should be adjusted slower or faster to fit the needs of your students and the performance situation. 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. -Larry Clark New York, NY 2003.
Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece. As with all of my pieces at this level, the tempo is merely a suggestion and should be adjusted slower or faster to fit the needs of your students and the performance situation. 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. -Larry Clark New York, NY 2003.
Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece.As with all of my pieces at this level, the tempo is merely a suggestion and should be adjusted slower or faster to fit the needs of your students and the performance situation.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.-Larry ClarkNew York, NY 2003.

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: HL.4493082

UPC: 196288182122.

Unleash awe-inspiring beauty of â??Theme from Jurassic Parkâ? with this enchanting string orchestra arrangement by Robert Longfield. John Williams' iconic score comes to life, allowing your orchestra to recreate the majestic wonder of prehistoric times. Elevate your performance with luch harmonies and captivating melodies that transport audiences to the heart of Jurassic Park. Perfect for young orchestras seeking a timeless cinematic experience, this arrangement promises to captivate and inspire, making your performance a Jurassic journey like never before.

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.

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