SKU: FJ.ST6446

UPC: 241444387580. English.

The stately spirits of soirees past appear, dancing the midnight waltz in the haunted ballroom. Dazzle your audience with this chilling, yet lighthearted tune; perfect for your fall and Halloween concerts. The piece offers a variety of fun chromatics, quirky col legno effects and harmonic glissandi. Certain to be a spooktacular addition to your next concert program!

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: CF.FAS26

ISBN 9780825854811. UPC: 798408054816. 8.5 X 11 inches. Key: D major.

Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless. Arches is an effective piece in teaching pizzicato playing as a melodic device. Most often, pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the main pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing these pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of these pizzicato lines.
Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless. Arches is an effective piece in teachingA pizzicato playing as a melodic device. Most often,A pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the mainA pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing theseA pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of theseA pizzicatoA lines.
Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless. Arches is an effective piece in teachingA pizzicato playing as a melodic device. Most often,A pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the mainA pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing theseA pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of theseA pizzicatoA lines.
Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless. Arches is an effective piece in teaching pizzicato playing as a melodic device. Most often, pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the main pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing these pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of these pizzicato lines.
Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless. Arches is an effective piece in teaching pizzicato playing as a melodic device. Most often, pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the main pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing these pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of these pizzicato lines.
Arches is a piece for the developing string orchestra that derives its title from the national park in Utah. I visited the Arches National Monument in June of 2003 during a cross-country trip. The Delicate Arch is the recognizable landmark from this beautiful national park. In order to see this remarkable natural formation up close, you have to hike a trail of over two miles. The music in this piece is inspired by my journey to see the arch. Once there, you are treated to a vast panoramic view of the golden Utah landscape that leaves one breathless.Arches is an effective piece in teaching pizzicato playing as a melodic device. Most often, pizzicato is used as an effect or punctuation mark to larger melodic ideas. There is a brief arco section to provide contrast and build up to the dramatic return of the main pizzicato melody. Each section in the ensemble has a statement of the melody. It is important to think linearly in addition to vertically when playing these pizzicato lines. Forward motion is of up-most importance in terms of making musical phrases out of these pizzicato lines.

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.