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.BAS5F

ISBN 9780825845093. UPC: 798408045098. 8.5 X 11 inches.

The musical effect of Prarie Lullaby should be graceful and serene, evocative of a peaceful night on the open plains. To that end, players will need to strive for an unlabored rhythmic flow, smooth bowing and a clear, steady tone as close to p as possible.Beginning at m.39, the violin and viola parts are marked pizzicato. If young players are unable to return quickly to argo at m.53, they may make the bow preparation easier by taking a full measure rest at m.52. This option is marked in the parts and score.The divisi notes at m. 69 are provided for ensembles which lack violas. Ensembles with violas may have them play the lower notes while the second violins play the upper notes.Percussion, which is completely optional, should be very subdued. Choose a bell mallet which allows the tones to be heard just above the strings. the woodblock part is intended to imitate the clip-clop sound of a horse's hooves. Two different sizes of woodblocks or temple blocks are needed. Finding two suitable sounds on one woodblock is difficult. Again, the right mallets are very important. The suspended cymbal should be played with brushes if the string ensemble is small. If the suspended cymbal with brushes cannot be heard above a large number of strings, then sticks should be used instead.The percussion part can be performed by one player, provided the instruments and mallets are set up properly and the player has the skill to make the transitions smoothly. Note the optional rest at mm. 53-54.Performance time with the repeat is two and a half minutes.

About Carl Fischer Beginning String Orchestra Series

This series of Grade 1 pieces is designed for first year string groups. The pieces in this series are characterized by:

• Limited parts (often 2nd violin and viola are the same part, cello and bass are same part)
• Limited keys and rhythms - only simple 8th note patterns
• Limited independence of parts
• Playable after limited study time
• First position and natural bowings
• Piano for rehearsal and reinforcement

SKU: BT.PWM4901

Concerto for String Orchestra - the magnum opus of Grayna Bacewicz (1909-1969), the outstanding composer and violinist - was composed in 1948 and at once became one of the most frequently performed works of this Polish artist. This masterpieceof neoclassicism fascinates as much by its invention and virtuosic briliance as its harmonious combination of formal elements of a traditional nature with new tonal ideas. The form of the three-movement Concerto oscillates between that of the baroqueconcerto grosso and the early classical sonata cycle. The neoclassical tendency is evident, above all, in the articulation of the musical structure in keeping with the rigours of periodicity and the manner of developing thematic threads derived fromthem, while the concertato character of particular movements and the generally linear texture indicate baroque connections. The first movement (Allegro) - in the form of an early classical sonata allegro - begins with a subject with energeticfigurations, emblematic for the whole piece and based on a constant, pendulum-like semiquaver movement anchored securely on D. It is precisely because of the nature of this subject that Bacewiczs work has been compared to the Brandenburg Concertosby Jan Sebastian Bach The second movement (Andante), while retaining its concertato charakter, is, at the same time, an example of the composers ability to create emotionally serene lyrical moods, and her sense of cantilena derived from the spiritof romantic song (a motto-subject presented at the beginning by cello solo). In this movement it is both the process of evolution and the instrumental colouring which constitute the constructional agents forming here a self-containedvalue. In thethird movement (Vivo) the composer returns to her favourite type of music, understood as an expression of pure motion in the form of figural motives with infinite transformational possibilities. The spontaneity of the music, the constant mutabilityof the tonal situations, and the sophisticated, acerbic harmonies - as Witold Lutosawski described them - form a colourful mosaic built in the structural skeleton of a sonata rondo. Concerto for String Orchestra is not only proof of thestylizing tendency of the composer but also of an unerring intuition concerning the technical and expressive possibilities inherent in a string instruments ensemble. [Magorzata Gsiorowska, translated by Ewa Cholewka].

SKU: FJ.ST6300S

English.

The ultimate in performance flexibility! Inspired by the music of fusion banjo genius Bela Fleck, this alternative style work can either be performed with a guest soloist or with orchestra alone. An open vamp section lets soloist(s) experiment without the pressure of changing chords. The infectious enthusiasm of electric violinist and composer Cathy Morris shines in this tune that is sure to bring down the house - and then some! *Recorded with Cathy Morris on electric violin.

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