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: HL.4493066
UPC: 196288177722.
Experience the epic world of Skyrim like never before with â??Dragonborn - Skyrim Themeâ? by Jeremy Soule, expertly arranged for string orchestra by Robert Longfield. Immerse your audience in the captivating melodies and soaring harmonies that define this iconic soundtrack. This 6/8 arrangement in B minor brings the magic, majesty, and driving energy of Tamriel to life!
SKU: KJ.SO336F
UPC: 8402704167.
Into the Dragon's Den focuses on playing F-sharps and F-naturals, and helps students become more comfortable with 2-note slurs. The piece centers around E minor, offering the perfect mood for the subject: confronting difficult things and handling fear. As Mr. Brown mentions in his program notes, Like the brave knight [heading into the dragon's den], beginning string students have to venture into the dark unknown to confront F-natural. Approx. time - 2:30 Steps to Successful Literature presents exceptional performance pieces - concert and festival works for beginning to intermediate string orchestras. Each piece is correlated with a specific location in String BasicsTM Books 1 or 2. Literature reinforces musical skills, concepts, and terms introduced in the method. Sometimes, a few new concepts are included and are officially introduced and defined in the score and parts. Each string orchestra work offers extended learning opportunities and briefly taps into one or more elements related to common core state standards.
SKU: CF.FAS21
ISBN 9780825853067. UPC: 798408053062. 8.5 X 11 inches. Key: B minor.
Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece. 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 Clark New York, NY 2003.Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece. 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 Clark New York, NY 2003.Character was composed to introduce young string players to contemporary harmonic techniques while still being within the technical limitations of the developing student. Quartal and quintal harmonies open the composition with a fanfare gesture that ties the piece together. This is followed by an ostinato in the first violins that contains a tricky figuration between G and A that will work the pinky finger on the D-string. Players who are not capable of maneuvering their pinky at this brisk tempo should play the lower part. The main theme is given to the inner voice for a change! After the main theme there is a development section that combines fragments of the fanfare material with fragments of the main theme. A grand pause and then a stronger statement of the main theme then follow this with the first violins up an octave. The piece is then completed with a short coda containing fragments of the ostinato and fanfare material. It feels natural for the tempo to speed up slightly at this point in the piece.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 ClarkNew York, NY 2003.
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