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: CF.YAS9
ISBN 9780825844867. UPC: 798408044862. 8.5 X 11 inches. Key: A minor.
Firewalk is a piece for young string orchestra designed to teach pizzicato playing to the developing string player. All too often, pizzicato is treated simply as an effect or percussive accent to a passage. With this piece, pizzicato becomes the melody, harmony and rhythm. It calls for the player to use dynamics and phrasing while playing pizzicato. This work is adapted from incidental music I composed for a production of The Birth of Merlin, a play by William Shakespeare. The piece is dedicated to Helen Borgers, who directed this production by the Bard in the Yard Shakespeare Company in Long Beach, CA. The material for Firewalk comes from a section in the play where the characters are dancing a devilish tango with ethereal spirits. The music features jaunty rhythms, dynamic contrasts, and a dramatic climax. Firewalk is a diverse addition to any concert program.Firewalk is a piece for young string orchestra designed to teach pizzicato playing to the developing string player. All too often, pizzicato is treated simply as an effect or percussive accent to a passage. With this piece, pizzicato becomes the melody, harmony and rhythm. It calls for the player to use dynamics and phrasing while playing pizzicato. This work is adapted from incidental music I composed for a production ofA The Birth of Merlin, a play by William Shakespeare. The piece is dedicated to Helen Borgers, who directed this production by the Bard in the Yard Shakespeare Company in Long Beach, CA. The material forA Firewalk comes from a section in the play where the characters are dancing a devilish tango with ethereal spirits. The music features jaunty rhythms, dynamic contrasts, and a dramatic climax.A Firewalk is a diverse addition to any concert program.Firewalk is a piece for young string orchestra designed to teach pizzicato playing to the developing string player. All too often, pizzicato is treated simply as an effect or percussive accent to a passage. With this piece, pizzicato becomes the melody, harmony and rhythm. It calls for the player to use dynamics and phrasing while playing pizzicato. This work is adapted from incidental music I composed for a production of The Birth of Merlin, a play by William Shakespeare. The piece is dedicated to Helen Borgers, who directed this production by the Bard in the Yard Shakespeare Company in Long Beach, CA. The material for Firewalk comes from a section in the play where the characters are dancing a devilish tango with ethereal spirits. The music features jaunty rhythms, dynamic contrasts, and a dramatic climax. Firewalk is a diverse addition to any concert program.Firewalk is a piece for young string orchestra designed to teach pizzicato playing to the developing string player. All too often, pizzicato is treated simply as an effect or percussive accent to a passage. With this piece, pizzicato becomes the melody, harmony and rhythm. It calls for the player to use dynamics and phrasing while playing pizzicato.This work is adapted from incidental music I composed for a production of The Birth of Merlin, a play by William Shakespeare. The piece is dedicated to Helen Borgers, who directed this production by the Bard in the Yard Shakespeare Company in Long Beach, CA. The material for Firewalk comes from a section in the play where the characters are dancing a devilish tango with ethereal spirits. The music features jaunty rhythms, dynamic contrasts, and a dramatic climax. Firewalk is a diverse addition to any concert program.
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
SKU: CF.YAS57
ISBN 9780825866890. UPC: 798408066895. 8.5 X 11 inches. Key: G major.
This is a sweeping new original composition in a subto Scottish style from popular composer Alan Lee Silva. Just another one of the pieces that always seem to flow effortlessly from his talented pen. This is an excellent piece for any contest or festival.This Scottish-flavored, uptempo piece in has a lilting, jubilant-feel throughout. Highland Celebration is built around two rhythmic subdivisions: two groups of three eighth notes per measure and three groups of two eighth notes per measure. Have the ensemble distinguish between the two subdivisions by tapping each one separately. Make an exercise of the rhythm in mm. 1–2 in Violin 1 to facilitate playing the different rhythms precisely: (1 2 3 - 4 5 6) and (1 2 - 3 4 - 5 6). Rehearsing four- to eightmeasure sections under tempo will aid in tightening these rhythms and solidifying pitch.The sections to concentrate on are: mm. 17–24 and mm. 33–40 to make sure that Violins I and II and Cello are playing together; mm. 33–40, to focus on the Violin 1 and Violin 2 unisons and couplings; and mm. 57–62, where the quarter-note subdivisions are emphasized. The piece is book-ended with the introduction material which always begins quietly and builds. The ensemble at m. 79 starts with tutti scalar figures and increases in intensity to the final accented measures at m. 83. Written in AABA form with a double bridge at m. 45, the overall feeling is dance-like and festive.
SKU: FJ.ST6327S
English.
Transform your orchestra into a Latin band with this burnin' jazz samba! Featuring solo violin (electric or acoustic) along with full rhythm section, this chart centers on a blues-like melody with traditional Latin rhythms. A solo section over a single chord lets your students shine in the world of improvisation, or consider bringing in a guest artist. Plenty of fun for both soloist and ensemble!
About FJH String Orchestra
More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up
SKU: CF.CAS24F
ISBN 9780825858253. UPC: 798408058258. 8.5 X 11 inches. Key: D major.
This driving piece by one of Carl Fischer’s most popular composers offers players fun fast fiddlin’ with dynamic contrast and fire. The creative use of syncopation will help to develop your student’s sense of rhythm while they have a good time.
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.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.
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