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.

Score and Parts String Orchestra (Score and Parts) - Grade 3-4

SKU: HL.4493066

Composed by Jeremy Soule. Arranged by Robert Longfield. Pop Specials for Strings. Video Games. Softcover. Duration 2520 seconds. Published by Hal Leonard (HL.4493066).

UPC: 196288177722.

Exper ience the epic world of Skyrim like never before with â??Dragonborn - Skyrim Themeâ? by Jeremy Soule, expertly arranged for string orchestra by Robert Longfield. Immerse your audience in the captivating melodies and soaring harmonies that define this iconic soundtrack. This 6/8 arrangement in B minor brings the magic, majesty, and driving energy of Tamriel to life!

By Rob Grice. Beginning String Orchestra. FJH Beginning Strings. Score for this title: ST6100S. Extra part for this title: ST6100P. String Orchestra. Level: 1. Score and Set of Parts. Published by The FJH Music Company Inc.

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

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.

By Richard Meyer. Music by Richard Meyer. For String Orchestra. String Orchestra. String Orchestra. Level: 2.5 (grade 2.5). Conductor Score

Composed by Rob Grice. Orchestra. Score; String Orchestra. Belwin Beginning String Orchestra. Grade 1. 12 pages. Published by Belwin Music

(String Pak (to accompany band/choir version)). By Irving Berlin. Arranged by Audrey Snyder and Paul Murtha. Score and Parts. Music for String Orchestra. Grade 3-4. Published by Hal Leonard

By Rob Grice. Orchestra. Score; String Orchestra. Belwin Beginning String Orchestra. Grade 1.5. 8 pages. Published by Alfred Music Publishing

By Rob Grice. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Belwin Beginning String Orchestra. Grade 1.5. 76 pages. Published by Belwin Publishing

Orchestra strings - beginner

SKU: KJ.SO336F

Composed by Raymond Brown. Arranged by Raymond Brown. Score. Neil A. Kjos Music Company #SO336F. Published by Neil A. Kjos Music Company (KJ.SO336F).

UPC: 8402704167.

Into the Dragon's Den focuses on playing F-sharps and F-naturals, and helps students become more comfortable with 2-note slurs. The piece centers around E minor, offering the perfect mood for the subject: confronting difficult things and handling fear. As Mr. Brown mentions in his program notes, Like the brave knight [heading into the dragon's den], beginning string students have to venture into the dark unknown to confront F-natural. Approx. time - 2:30

Steps to Successful Literature presents exceptional performance pieces - concert and festival works for beginning to intermediate string orchestras. Each piece is correlated with a specific location in String BasicsTM Books 1 or 2. Literature reinforces musical skills, concepts, and terms introduced in the method. Sometimes, a few new concepts are included and are officially introduced and defined in the score and parts. Each string orchestra work offers extended learning opportunities and briefly taps into one or more elements related to common core state standards.

By Imagine Dragons. Arranged by Larry Moore. For String Orchestra (Score and Parts). Pop Specials for Strings. Grade 3-4. Published by Hal Leonard

By Samuel Augustus Ward. Arranged by Carmen Dragon, adapted by Douglas E. Wagner. Orchestra. Part(s); Score; String Orchestra. Pop Beginning String Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 72 pages. Published by Alfred Music Publishing

By Samuel Augustus Ward. Arranged by Carmen Dragon, adapted by Douglas E. Wagner. Orchestra. Score; String Orchestra. Pop Beginning String Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 8 pages. Published by Alfred Music Publishing

By Michael Story and Michael Story. Orchestra. Score; String Orchestra. Orchestra Expressions Book 1. Form: Dance. Light Concert; World. Grade 1. 8 pages. Published by Alfred Music Publishing

Composed by John Powell. Arranged by Robert Longfield. Easy Pop Specials For Strings. Concert, Movies. Softcover. Duration 100 seconds. Published by Hal Leonard

By Michael Story and Michael Story. Orchestra. For string. Part(s); Score; String Orchestra. Orchestra Expressions Book 1. Form: Dance. Light Concert; World. Grade 1. 62 pages. Published by Alfred Music Publishing

By Scott Joplin. Arranged by William Zinn. For 2nd Violin. String Orchestra Collection. Book. 20 pages. Published by Alfred Publishing.

By Nicholas Hooper. Arranged by Jack Bullock. For String Orchestra. String Orchestra. Pop Beginning String Orchestra. Light Concert; Movie. 2 (grade 2). Conductor Score. 8 pages. Published by Alfred Music Publishing

By Wolfgang Amadeus Mozart (1756-1791). Arranged by Jamin Hoffman. Score and Parts. Music for String Orchestra. Grade 3-4. Published by Hal Leonard

By One Direction. Arranged by Larry Moore. Pop Specials for Strings. Softcover. Published by Hal Leonard

By Nicholas Hooper. Arranged by Jack Bullock. For String Orchestra. String Orchestra. Pop Beginning String Orchestra. Light Concert; Movie. 2 (grade 2). Conductor Score and Parts. 72 pages. Published by Alfred Music Publishing

Orchestra String Orchestra - Grade 1.5-2

SKU: CF.FAS21

Composed by Larry Clark. Edited by Amy Rosen. SWS - FS. Carl Fischer First Plus String Orchestra Series. Classical. Score and Parts. With Standard notation. 8+8+2+5+5+5+2+8 pages. Carl Fischer Music #FAS21. Published by Carl Fischer Music (CF.FAS21).

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

Characte r 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.