Grade 2

SKU: CL.014-0105-00

Waltz. Composed by King. Band. Score and set of parts. Composed 1931. C.L. Barnhouse #014-0105-00. Published by C.L. Barnhouse (CL.014-0105-00).

Note: This is a reprint from a vintage publication of 1931. No conductor score is published for this work. The Solo Cornet part serves as a conductor guide. Parts for Eb Horns are included; no F Horn parts are published for this work. If a C Piccolo/C Flute part was not published originally, one has been subsequently added by our editorial staff.

Orchestra String Orchestra - Grade 2-2.5

SKU: CF.YAS15

Composed by Traditional Holiday Song. Edited by Amy Rosen. Arranged by Bud Caputo. SWS FS. Carl Fischer Young String Orchestra Series. Score and Parts. With Standard notation. 16+2+4+16+10+10+3+10+12 pages. Carl Fischer Music #YAS15. Published by Carl Fischer Music (CF.YAS15).

ISBN 9780825851995. UPC: 798408051990. 8.5 X 11 inches. Key: D minor.

Lower strings be sure to maintain a steady pulse and dont rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 121. If the soloist is comfortable using third position, play mm. 119 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.
Lower strings be sure to maintain a steady pulse and donat rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1a21. If the soloist is comfortable using third position, play mm. 1a19 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.
Lower strings be sure to maintain a steady pulse and don't rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1-21. If the soloist is comfortable using third position, play mm. 1-19 and the first half of m. 20 one octave higher. All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance. String editing by Amy Rosen.
Lower strings be sure to maintain a steady pulse and don’t rush the walking figure at the opening. When the melody is transferred to the lower strings (pick-up to m. 10 and m. 13), play with a full sound. Be careful of the balance and allow the soloist to dominate in mm. 1–21. If the soloist is comfortable using third position, play mm. 1–19 and the first half of m. 20 one octave higher.All parts should be in a solid marcato style in the fast section (m. 22 to the end). In m.50, Violin I should bring out the Hava Nagila quote equal to the volume of the rest of the orchestra. Be sure to observe all the soft dynamics to add interest to the performance.String editing by Amy Rosen.

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

Bb Edition. Fake Book (Includes melody line and chords). Size 9x12 inches. 816 pages. Published by Hal Leonard.

645 Songs from 285 Shows. Composed by Various. Fake Book. Broadway. Softcover. 696 pages. Published by Hal Leonard

By Amy Grant and Michael W. Smith. By Amy Grant, Michael W. Smith, and Wes King. Arranged by Heather Sorenson. For Choral (SATB). Sacred Choral. 12 pages. Published by Hal Leonard

By Amy Grant and Michael W. Smith. By Amy Grant, Michael W. Smith, and Wes King. Arranged by Heather Sorenson. For Choral (CHOIRTRAX CD). Sacred Choral. CD only. Published by Hal Leonard

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

SKU: SU.32040140

For Orchestra. Composed by Amy Riebs Mills. Orchestra. Full Score. Subito Music Corporation #32040140. Published by Subito Music Corporation (SU.32040140).

2222; 4331; timp, 2 perc, pno; stgs Duration: 13'30 Composed: 2016 Published by: Amy Mills Music, LLC Like a modern Pictures at an Exhibition…. Ha Shamayim is an original piece for orchestra that was inspired by photographs taken by the Hubble space telescope. Each section is inspired by one photo; the title of each section is the title that NASA gave to the photograph. The words Ha Shamayim are Hebrew for The Heavens. They are written in Genesis 1:1, In the beginning God created the heavens and the earth. The words are also seen in Psalm 19. Section I: Warped Edge-On Galaxy ESO 510-G13 The piece begins in outer space with its glistening stars. Glissandi are used to depict the strange but beautiful warp seen in the photograph. Section II: Galaxy Fires at Neighboring Galaxy Suddenly the piece erupts as one galaxy fires blue gas at its neighbor. They engage in a cosmic battle. Section III: Youthful-looking Galaxy May Be an Adult The adolescent galaxy is personified by a humorous, gawky melody reminiscent of teenage boys who walk on feet that are still too big. Occasionally there is an argument with an authority figure, but the joy of exploring the universe quickly returns. Section IV: Star Birth in Galaxy M83 The dramatic photograph looks like a womb with veins. The music begins on one note, then it begins to explore the initial swelling and stretching. It morphs into an energetic fast theme, still growing. Ultimately it becomes glorious and expansive, like the new star. Section V: String of ‘Cosmic Pearls’ Surrounds an Exploding Star The first theme is a happy circle dance inspired by the circle of white dots in the photograph. The second theme is noble and joyful. It is reminiscent of the melody in the famous chorus in Haydn’s The Creation with the words from Psalm 19, The heavens are telling the glory of God. The music then has flashbacks to the earlier sections, and ends in triumph. The five sections in Ha Shamayim are continuous with no breaks. Difficulty Level: 5 (Advanced/Professional) See composer website for audio sample. Performance materials available on rental only:.

Mezzo-Soprano & Piano

SKU: SU.32040040

For Mezzo-Soprano & Piano. Composed by Amy Riebs Mills. Vocal/Choral, Solo Voice. Accompanied by piano. Piano Vocal Score. Subito Music Corporation #32040040. Published by Subito Music Corporation (SU.32040040).

Mezzo-Soprano & Piano Duration: 17' Composed: 2014 Published by: Amy Mills Music, LLC These three art songs can be performed independently or in sequence, at any time of the year. Stuart McAlpine’s profound text explores three men from the Christmas story, Joseph, the Inn-keeper, and Simeon. The creative and beautiful musical settings allow for powerfully dramatic interpretation and performance. To Joseph (who taught me how to look at art) The singer sings to Joseph, …you beheld a work of art, the making of a holy heart… and watching through Joseph’s eyes, when hung at last, its meaning was decreed. (4:40) The Inn-keeper’s Lament McAlpine brilliantly explores the possibility…what if the inn-keeper who turned away Mary & Joseph later became the inn-keeper who accepted the injured man brought in by the Good Samaritan? This powerfully dramatic piece depicts the Bethlehem inn-keeper’s bravado, Caeser’s decree was heaven sent, as guests raised glasses, I raised rent! But as the enormity of his mistake became apparent, in later years he bemoans, …if I’d known then what I know now… and finally declares at the end, I know now! (7:50) Simeon’s Last Prayer Simeon sings of being summoned to the temple where he holds his infant Savior. …then as grandfathers do, rejoiced as if he were my one-and-only too. As he leaves he whispers his final prayer, …dismiss your servant, to find You face-to-face. (4:30) Difficulty Level: Baritone/Mezzo-Soprano 6 (Professional) (Baritone Range: low A (optional low G) to high F# (optional high G,A) (Mezzo Range: low A (optional low G) to high G (optional high A) Piano 6 (Professional)(Same level as Debussy or Ravel) See also the version for Baritone Voice and Piano See composer website for audio sample.

SKU: LO.99-3042H

Composed by Amy F Bernon. Choral. Concert. Performance/accompaniment CD. Heritage Music Press #99/3042H. Published by Heritage Music Press (LO.99-3042H).

UPC: 000308132861.

Cheeky and cheerful, this charming original piece by Amy Bernon is an invitation to sing, dance, and explore the partnerships that come from making music together. Full of engaging wordplay and unexpected moments, you won't want to miss this rhythmic and whimsical choice for young singers.

The Ukulele Decade Series. Composed by Various. Ukulele. Pop, Rock. Softcover. 184 pages. Published by Hal Leonard

(Decade Series Play-Along). Composed by Various. For Piano/Vocal/Guitar. Piano/Vocal/Guitar Songbook. Softcover Audio Online. 352 pages. Published by Hal Leonard

(B-Flat Instruments). Composed by Various. Arranged by Robert Rawlins. For B-flat Instruments. Fake Book. Softcover. 380 pages. Published by Hal Leonard