Arranged by Douglas E. Wagner. Part(s); Score; String Orchestra. Belwin Beginning String Orchestra. Form: Medley. Christmas; Sacred; Secular; Winter. 72 pages. Published by Belwin Music (AP.45820).

Composed by Franz Xaver Gruber. Arranged by Jeffrey E. Turner. Part(s); Score; SmartMusic; String Orchestra. Belwin Intermediate String Orchestra. Christmas; Sacred; Winter. 76 pages. Published by Belwin Music (AP.44799).

(Volume 2 - Violin 3). Arranged by Leonard Slatkin. For String Orchestra (Violin). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

(Volume 2 - Cello). Arranged by Leonard Slatkin. For String Orchestra (Cello). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

(Volume 2 - Bass). Arranged by Leonard Slatkin. For String Orchestra (Double Bass). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

(Volume 2 - Violin 2). Arranged by Leonard Slatkin. For String Orchestra (Violin). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

(Volume 2 - Solo Piano). Arranged by Leonard Slatkin. For String Orchestra (Piano). Easy Music For Strings. Grade 2. 24 pages. Published by Hal Leonard

(Volume 2 - Violin 1). Arranged by Leonard Slatkin. For String Orchestra (Violin). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

(Volume 2 - Viola). Arranged by Leonard Slatkin. For String Orchestra (Viola). Easy Music For Strings. Grade 2. 12 pages. Published by Hal Leonard

Arranged by Jon Ward Bauman. (Score and Parts). Easy Music For String. Published by Hal Leonard.

Composed by Adolphe-Charles Adam (1803-1856). Arranged by Jeffrey E. Turner. Orchestra. Part(s); Score; String Orchestra. Belwin Intermediate String Orchestra. Christmas; Light Concert; Winter. Grade 3. 74 pages. Published by Belwin Music

(As performed by Trans-Siberian Orchestra). Arranged by Paul O'Neill [Trans-Siberian Orchestra], setting by Bob Phillips. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Form: March. Christmas; Rock; Sacred; Winter. Grade 3. 148 pages. Published by Alfred Music

Orchestra String Orchestra - Grade 2.5

SKU: FJ.ST6286S

Score Only. Arranged by Lauren Bernofsky. Series; String Orchestra. FJH Developing Strings. Christmas; Holiday Pops. Score. Duration 3:00. The FJH Music Company Inc #98-ST6286S. Published by The FJH Music Company Inc (FJ.ST6286S).

English.

Christm as and Chanukah faiths collide in this hilarious yet musically satisfying option for your winter program! Four popular Christmas melodies are set in four distinct and characteristic klezmer styles. Opening with Jingle Bells over a slow and dramatic Doina, the music moves into a lively version of We Wish You a Merry Christmas as a Bulgar. A Khosidl is the setting for a slower, restrained version of Hark! The Herald Angels Sing (complete with shout chorus!). Then the music takes off with Deck the Halls presented as a Sher. Of course, the Dreidel Song makes a cameo appearance at the end. Tons of fun and wildly entertaining!

About FJH Developing Strings

Sl ightly more advanced than Beginning Strings, this series begins to involve more position work and a slightly more complex rhythmic figures. Rehearsal piano is often provided. Ideal for middle school and smaller high school programs. Grade 2 - 2.5

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.

Orchestra String Orchestra - Grade 2

SKU: FJ.ST6432S

Score Only. Arranged by Kathryn Griesinger. Series; String Orchestra. FJH Developing Strings. Holiday Pops. Score. Duration 2:00. The FJH Music Company Inc #98-ST6432S. Published by The FJH Music Company Inc (FJ.ST6432S).

English.

A rocking celebration of the season! Set in first position with simple rhythms and no slurs, this contemporary arrangement includes the familiar carols Deck the Hall, Hark, the Herald Angels Sing, and Ding, Dong, Merrily On High. Every section of the orchestra is featured and the energetic cello/bass groove is driven by optional drum set and sleigh bells. An exuberant finale for your holiday concert!

About FJH Developing Strings

Sl ightly more advanced than Beginning Strings, this series begins to involve more position work and a slightly more complex rhythmic figures. Rehearsal piano is often provided. Ideal for middle school and smaller high school programs. Grade 2 - 2.5

(Combined Concert Band, String Orchestra and Full Orchestra Accompaniment for Choir). Composed by Michael and Angela Souders. Arranged by Jerry Brubaker. Orchestra. Full Orchestra; Score. Pop Intermediate Full Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 12 pages. Published by Alfred Music

(Combined Concert Band, String Orchestra and Full Orchestra Accompaniment for Choir). By Michael and Angela Souders. Arranged by Jerry Brubaker. Orchestra. Full Orchestra; Part(s); Score. Pop Intermediate Full Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 130 pages. Published by Alfred Music Publishing