SKU: FJ.ST6241S
English.
This clever arrangement uses melodies from Joy to the World and Beethoven's Ode to Joy before combining the two in the final section of the piece. Students will develop hooked bowing technique in addition to other important concepts. Accented notes represent chiming bells and will surely spread joy among your students and audience with spirited resonance!
About FJH Beginning Strings
Appropriate 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
SKU: AP.36-52255274
ISBN 9781628760484. UPC: 746241255457. English.
As the title implies, this music is "in the style of" Handel, using the counterpoint in a way that slowly builds intensity to the dramatic finish. Set in the key of E minor, this piece remains well within the reach of orchestras at the medium-easy level players.
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SKU: CF.CAS10
ISBN 9780825847615. UPC: 798408047610. 8.5 X 11 inches. Key: G major.
With this arrangement, my goal is to maintain the integrity of the original work, while making it accessible to the younger orchestra. An important aspect of the successful performance of this piece is maintaining an energetic tempo. The repeated eighth notes in the accompaniment should be played cleanly and crisply to maintain momentum. There are many places where abrupt changes in dynamics occur. For example, m. 1 begins with a string unison forte, which suddenly drops to piano at m. 11. Accents, staccatos, and other articulations should be carefully observed. To be effective, crescendos should begin at a reasonable volume, so they have somewhere to go dynamically. I hope you and the orchestra enjoy this arrangement.With this arrangement, my goal is to maintain the integrity of the original work, while making it accessible to the younger orchestra. An important aspect of the successful performance of this piece is maintaining an energetic tempo. The repeated eighth notes in the accompaniment should be played cleanly and crisply to maintain momentum. There are many places where abrupt changes in dynamics occur. For example, m. 1 begins with a string unisonA forte, which suddenly drops toA piano at m. 11. Accents, staccatos, and other articulations should be carefully observed. To be effective, crescendos should begin at a reasonable volume, so they have somewhere to go dynamically. I hope you and the orchestra enjoy this arrangement.With this arrangement, my goal is to maintain the integrity of the original work, while making it accessible to the younger orchestra. An important aspect of the successful performance of this piece is maintaining an energetic tempo. The repeated eighth notes in the accompaniment should be played cleanly and crisply to maintain momentum. There are many places where abrupt changes in dynamics occur. For example, m. 1 begins with a string unison forte, which suddenly drops to piano at m. 11. Accents, staccatos, and other articulations should be carefully observed. To be effective, crescendos should begin at a reasonable volume, so they have somewhere to go dynamically. I hope you and the orchestra enjoy this arrangement.With this arrangement, my goal is to maintain the integrity of the original work, while making it accessible to the younger orchestra. An important aspect of the successful performance of this piece is maintaining an energetic tempo. The repeated eighth notes in the accompaniment should be played cleanly and crisply to maintain momentum. There are many places where abrupt changes in dynamics occur. For example, m. 1 begins with a string unison forte, which suddenly drops to piano at m. 11. Accents, staccatos, and other articulations should be carefully observed. To be effective, crescendos should begin at a reasonable volume, so they have somewhere to go dynamically. I hope you and the orchestra enjoy this arrangement.
About Carl Fischer Concert String Orchestra Series
This series of pieces (Grade 3 and higher) is designed for advancing ensembles. The pieces in this series are characterized by:
SKU: CF.CAS44
ISBN 9780825867118. UPC: 798408067113. 8.5 X 11 inches. Key: G minor.
This is a tour-de-force for the advancing string orchestra. Beautiful, dramatic, and flowing, Waterloo Station is very fresh and contemporary. Students will love it for the lush harmonic textures and rhythmic drive that this composer is so noted for.Composed as a characterization of the fast-paced atmosphere of London’s Waterloo Train Station, this fast-slow-fast piece combines technical excitement with heartfelt simplicity.The fast section in G minor consists of two main parts: the intense, emotional A section at m. 21 and the legato, sweeping B section at m. 59. The syncopated tutti figures in the high strings coupled with the fiery cello and bass lines propel the fast sections. The phrase in mm. 1–8 recurs throughout. Making four- to eight-measure exercises of this section below tempo in the violins and viola, focusing on rhythmic clarity, will help to lock in the syncopation. Similarly, the cello and bass should rehearse this slowly as well as mm. 9–16 to gain fluidity and insure a solid foundation.The cellos carry the tune at m. 71, and the ensemble builds from mm. 79–86 to the transition at m. 87. An abrupt change to half tempo here slows the momentum and transitions to a quiet, melancholy tone in m. 91. The middle section (ABA) begins in G minor with a somber quality, highlighted by the Violin I solo. It gradually builds to a beautiful, uplifting setting as it moves to G major in m. 100. Returning back to the hushed G minor tonality, it then speeds up again and transitions back to Tempo I for a brief recapitulation of the fast section. Measure 117 marks the return to vigorous playing, beginning softly and building to a thrilling ride to the end.
SKU: CF.CAS37
ISBN 9780825863660. UPC: 798408063665. 8.5 X 11 inches. Key: C major.
A salute to the famous sailboat race, this rollicking piece in A minor introduces compound time with an opening (and closing) section in 12/8. The fast flowing music of the opening, vividly suggestive of a ship slicing through the waves, returns in a higher key (B minor) after a warmly scored, sweepingly melodic middle section. This is a piece whose sophistication is an excellent showcase for a more advanced performing group.Written in 12/8 in A minor, America’s Cup evokes the intensity and momentum of a wild sea with driving triplets, sweeping melodies, and accented downbeats. The A-material from the opening measure is played aggressively but lightly enough to keep the feeling of forward motion. Strong accents and rhythmically precise playing in the cello and bass provide solid support for the fast moving violin and viola passages. Measure 67 begins the slow, pastoral setting of the B-material. A gentle, lyrical violin motive in A major grows into a high, sweeping melody over sustained harmonies. This provides a brief repose before returning to the fastoriginal tempo and minor key as the recapitulation begins at m. 90. A modulation to B minor (m. 94) lifts the energy of the piece and gives young players the challenge of playing the running lines in another key. Measure 118 builds to the end, keeping the intensity a soft dynamic and growing into the final syncopated tutti unison figure in mm. 122–123.
SKU: CF.FAS43
ISBN 9780825863387. UPC: 798408063382. 8.5 X 11 inches. Key: E minor.
Titled by the students of J. T. Lambert Middle School in East Stroudsburg, PA, which commissioned the original version for band, this brilliant, heavily accented piece emphasizes rhythmic alertness and attention to dynamic contrasts. Bold fanfare writing alternates with lyrical writing of considerable warmth and the spiccato style of playing is introduced.The title for Dance of the Thunderbolts was suggested by students at J. T. Lambert Middle School in East Stroudsburg, Pennsylvania. This piece was originally commissioned for the sixth-grade band at the school in 2003 and has now been transcribed for string orchestra. The students specifically asked for the piece to be “a strong powerful piece with lots of accents and a strong abrupt ending.†As you can see and hear, the piece contains many of these aspects. After the title was suggested I came up with the thunderbolt dance section of the piece first stated at m. 24. Later during the compositional process I decided to frame this theme with a more lyrical theme, but one that still contains the sparkle of the staccato ostinato that is layered together with the elongated theme. Following the thunderbolt dance at m.24 is a short interlude to soften the sound before a return of the theme in fragments traded between different sections and in different tessituras. The lyrical theme returns and is followed by “a strong abrupt ending†as suggested by the students. 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 ClarkLakeland, FL 2007.
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.
SKU: BA.BA11564
ISBN 9790260109148. 31 x 24.3 cm inches. Key: B-flat major. Preface: David R. Beveridge.
The discovery of a lost source to AntonÃn Dvorák's â??Nocturneâ? in B major op. 40 provides new insights into the genesis of the composition and the composer's intended final form of this lyrical little piece for string orchestra.The musical material of what was later to be named â??Nocturneâ? was initially elaborated in the String Quartet in E minor; subsequently it was used in the original version of the String Quintet in G major as its second movement. However Dvorák then extracted it again, expanding and editing it afresh. The final result was the â??Nocturneâ? for string orchestra (two violins, viola, violoncello, double bass). The first edition was published by Bote and Bock in 1883.The authorized second copy of the work that had served as a template for the first printing was discovered by the editor Jonáš Hájek in a privately owned collection. This enabled him to resolve the several ambiguities caused by the existence of multiple versions and to unveil the authentic â??Nocturneâ?.
About Barenreiter Urtext
What can I expect from a Barenreiter Urtext edition?
MUSICOLOGICALLY SOUND - A reliable musical text based on all available sources - A description of the sources - Information on the genesis and history of the work - Valuable notes on performance practice - Includes an introduction with critical commentary explaining source discrepancies and editorial decisions ... AND PRACTICAL - Page-turns, fold-out pages, and cues where you need them - A well-presented layout and a user-friendly format - Excellent print quality - Superior paper and binding
SKU: AP.29738S
UPC: 038081323176. English.
The bright, sunny disposition of Italy is evident in this arrangement of the first movement of Mendelssohn's Symphony No. 4, Italian. Mendelssohn was a master of writing for string orchestra and this arrangement presents the major themes of the first movement in an edited version sure to keep the interest of you intermediate or advanced high school orchestra. (3:45).
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