SKU: HL.14024953
English.
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.
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: HL.4490466
UPC: 073999290868. 9.0x12.0x0.025 inches.
This iconic song from Bernstein's classic stage work remains one of the most popular melodies in American contemporary theater. Stephen Bulla's edition for strings is adapted from the original score, yet features accessibility for younger players. Let your students experience the mastery of this beloved American composer with this first-ever arrangement for string ensemble.
SKU: HL.1190014
ISBN 9781705192542. UPC: 196288131816.
Osvaldo Nicolás Ferraro Gutiérrez (1934-1977), better known as Waldo de los RÃos, was an Argentine composer best remembered for his knack for making pop music out of European classical music. His South American Suite (Suite SudAmericana) is in four movements: 1. Paraguay (Nanduty; Jungle Night; Epic), 2. Argentina (Los Colorados; The Shadow of the Tiger; The Tryst), 3. Peru (Cuzco Ruins; Lima; The Giants), and 4. Uruguay (The Wagon; Gaucho Song; Carnival).
SKU: AP.36-A601299
ISBN 9798888522424. UPC: 676737533847. English.
Morton Gould, equally comfortable in the worlds of both serious and light music, presented his symphonettes (an Americanization of the term sinfonietta, much like kitchenette and dinette) as works of a truly American vernacular, drawing on popular culture as well as classical forms. His American Symphonette No. 2 was the work that first made Gould a name among the American public through radio, with the second movement (Pavanne) a pop orchestra standard to this day. Instrumentation: 2.2.2.2: 4Sax(opt.; AATB; all dCl): 2.3.3.0: Perc(1): Hp(or Pno): Gtr: Str (9-8-7-6-5 in set). The original condensed score is included with this set, but the full score has been extracted from the complete work and also included.
These products are currently being prepared by a new publisher. While many items are ready and will ship on time, some others may see delays of several months.
SKU: AP.36-A601201
ISBN 9798888522431. UPC: 676737534301. English.
Morton Gould (1913-1996), equally comfortable in the worlds of both serious and light music, presented his symphonettes (an Americanization of the term sinfonietta, much like kitchenette and dinette) as works of a truly American vernacular, drawing on popular culture as well as classical forms. His American Symphonette No. 2 was the work that first made Gould a name among the American public through radio, with the second movement (Pavanne) a pop orchestra standard to this day. Instrumentation: 2.2.2.2: 4Sax(opt.; AATB; all dCl): 2.3.3.0: Perc(1): Hp(or Pno): Gtr: Str (9-8-7-6-5 in set). The original condensed score is included with this set, but the full score has been extracted from the complete work and also included.
SKU: AP.36-A601290
UPC: 676737533533. English.
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.