Spring from the Four Seasons by Antonio Vivaldi (1678-1741). Arranged by Richard Meyer. Orchestra. Masterworks; String Orchestra. Strictly Strings Series. Form: Overture. Baroque; Masterwork Arrangement; Spring. Grade 1. Conductor Score and Parts. 140 pages. Published by Alfred Music Publishing

Arranged by Carrie Lane Gruselle. Beginning String Orchestra. FJH Beginning Strings. Score for this title: ST6108S. Extra part for this title: ST6108P. String Orchestra. Level: 1. Score and Set of Parts. Published by The FJH Music Company Inc.

By Franz Joseph Haydn. Arranged by Robert D. Mccashin. String Orchestra. FJH String Orchestra. Late in life, Franz Joseph Haydn wrote twelve symphonies known as the "London" or "Salomon" Symphonies. They were composed for and during his two visits to London between 1791 and 1795. It was during his first visit that he was awarded the honorary degree of Doctor of Music from Oxford University (1791). Haydn had been invited to come to London by Johann Peter Salomon, London violinist and concert impresario. The invitation included the writing and conducting of some twenty new works as part of a dedicated concert series. Symphony No. 104 in D Major is the last of the 12 London Symphonies from which this arrangement is drawn. Despite the dramatic slow introduction of the first movement, the entire symphony reflects the great satisfaction and joyful energy of Haydn's existence during these visits to England. Score for this title: ST6097S. Extra part for this title: ST6097P. Level: 4.5. Published by The FJH Music Company Inc.

Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (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.

By Frank Halferty. For string orchestra. Playground String Orchestra Series. Grade 1. Score and Set of Parts. Published by Kendor Music Inc

Arranged by Bert Ligon. For strings with optional rhythm section. Standard strings with optional rhythm section. Kendor Jazz Classics for String Orchestra Series. Grade 4. Score and parts. Duration 3 minutes 55 seconds. Published by Kendor Music Inc

Composed by Wolfgang Amadeus Mozart (1756-1791). Arranged by Arthur Frackenpohl. Concert String Orchestra Series. Score and set of parts. Published by Kendor Music Inc (KN.10048).

Composed by Franz Joseph Haydn (1732-1809). Edited by Sonja Gerlach and Sterling E. Murray. This edition: urtext edition. Stapled. Score. Hob. I:76. Baerenreiter Verlag #BA10987. Published by Baerenreiter Verlag

By Richard Meyer. Orchestra. String Orchestra. Highland String Orchestra. Form: Variations. Contemporary; Light Concert; Novelty. Grade 3. Conductor Score and Parts. 124 pages. Published by Alfred Music Publishing

Orchestra String Orchestra - Grade 1.5

SKU: FJ.ST6260S

Score Only. Composed by Robert D McCashin. Series; String Orchestra. FJH Beginning Strings. Light Concert; Multicultural; Novelty. Score. Duration 1:30. The FJH Music Company Inc #98-ST6260S. Published by The FJH Music Company Inc (FJ.ST6260S).

English.

Experie nce the Spanish styles of the late 19th century in this clever original for strings! Melodies are shared equally across the ensemble without sounding contrived, and there are many stylistic teaching opportunities ranging from a warm legato sound to a clean staccato bow stroke. Sure to be a hit with both your ensemble and audience!

About FJH Beginning Strings

Ap propriate for first year string students. All instruments stay in first position, and optional third violin (viola) parts and piano are included to aid in rehearsal and performance situations. Grade 1 - 1.5

By Edvard Grieg. Arranged by Brendan Mcbrien. Music by Edvard Grieg / arr. Brendan McBrien. For String Orchestra. String Orchestra. String Orchestra. Conductor Score and Parts. 2 pages. Published by Alfred Publishing.

By Edvard Grieg. Arranged by Brendan Mcbrien. Music by Edvard Grieg / arr. Brendan McBrien. For String Orchestra. String Orchestra. String Orchestra. Level: 3.5 (grade 3.5). Conductor Score. 12 pages. Published by Alfred Publishing.

By Edvard Grieg. Arranged by Brendan Mcbrien. Music by Edvard Grieg / arr. Brendan McBrien. For String Orchestra. String Orchestra. String Orchestra. Level: 3.5 (grade 3.5). Conductor Score and Parts. Published by Alfred Publishing.

By Edvard Grieg. Arranged by Brendan Mcbrien. Music by Edvard Grieg / arr. Brendan McBrien. For String Orchestra. String Orchestra. String Orchestra. Conductor Score. 16 pages. Published by Alfred Publishing.

Arranged by Owen Goldsmith. Orchestra. String Orchestra. String Orchestra. Christmas; Winter. Grade 2. Conductor Score. 8 pages. Published by Alfred Music Publishing

Composed by Daniel DiMarino. For string orchestra. Original Concert Work. Grade 4. Score and set of parts. Duration 4:06. Published by Wingert- Jones Publications

By Richard Meyer. Music by Richard Meyer. For String Orchestra. String Orchestra. String Orchestra. Level: 2 (grade 2). Conductor Score and Parts. 1 pages. Published by Alfred Publishing.

Composed by Michael Story. Part(s); Score; String Orchestra. Belwin Beginning String Orchestra. Form: Dance. 76 pages. Published by Belwin Music (AP.44787).

String Orchestra Orchestra - Grade 3

SKU: XC.RSO2001

Composed by Peter Sciaino. Rhapsody String Orchestra Series. Concert and Contest. Concert and contest. Set of parts. Excelcia Music Publishing #RSO2001. Published by Excelcia Music Publishing (XC.RSO2001).

UPC: 812598034493. 9 x 12 inches.

Insomnia was inspired by the frustration and tension associated with a sleepless night. Using the phrygian mode, Insomnia has wide stylistic and dynamic ranges, representing a range of emotion before ultimately coming to a dramatic finish. Stay awake with this cool new work for strings!