By Scott Joplin. For Piano. (Piano Solo). CD Sheet Music (Version 2.0). PDF file on CD. 850 pages. Published by Subito Music.

Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (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.

By Kathleen Schubert. For Piano. Piano Solo. Sheet. 4 pages. Published by Alfred Publishing.
Level: Early Elementary.

Arranged by Peter Blood, Annie Patterson. Vocal. Size 7.5x10.5 inches. 283 pages. Published by Hal Leonard.

by Fred Sokolow. For 5 string banjo. Jazz and blues, g tuning. Level: Intermediate. Book. Solos. Size 8.75x11.75. 56 pages. Published by Mel Bay Pub., Inc.

(Words and Chords to Nearly 1200 Songs Spiral-Bound). Edited by Annie Patterson and Peter Blood. For Vocal. Vocal. Softcover. 304 pages. Published by Hal Leonard

Edited by David Brody. For violin. Format: fake book. With lead melody, chord names, instructional text and performance notes. Folk, americana and british. 302 pages. 9x12 inches. Published by Oak Publications.

Music Pathways - Repertoire 3B Lynn Freeman Olson, Marvin Blickenstaff See larger cover Your price $7.95 [?6.34] Pre-shipment lead time: 1 to 2 weeks Ready to buy? Quantity: (you can remove it later) Save 10% when you buy 2 or more copies of this title. Average customer rating: Add a review for this title! About Music Pathways - Repertoire 3B Repertoire - 3b. By Lynn Freeman Olson, Marvin Blickenstaff. Arranged by Louise Bianchi; Lynn Freeman Olson; Marvin Blickenstaff. Solo piano. For Piano Solo. Solo part. 32 pages. Published by Carl Fischer

Orchestra Cello, Contrabass, Piano, Viola, Violin 1, Violin 2, Violin 3 - Grade 1

SKU: CF.BAS79

Composed by Larry Clark. Beginning String Orchestra (BAS). Set of Score and Parts. With Standard notation. 8+2+8+5+5+5+3+8 pages. Duration 2:10. Carl Fischer Music #BAS79. Published by Carl Fischer Music (CF.BAS79).

ISBN 9781491151242. UPC: 680160908745. 9 x 12 inches. Key: E minor.

This piece should depict images of kings and castles, knight and horses, dragons and damsels in distress. It is a bold and aggressive piece throughout, but a contrasting lush secondary theme for variety. Typical of why Larry's music is so popular are his signature forceful figures, and strong melodic content that will stimulate students to practice it over and over again.  .
This piece should depict images of kings and castles, knight and horses, dragons and damsels in distress. It should be bold and aggressive throughout, but never with bad tone. There is then contrasted by the lush second theme that is presented first in a softer thin orchestration, but later becomes a change for the whole ensemble to play in a strong, but lush presentation of this theme.One thing that is important to me when writing music for younger students is to offer pieces that challenge all student in the ensemble and give every section an important part of the musical presentation, which naturally should include some melodic material. Every member of the ensemble wants to feel that they are contributing to the collective whole.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 2018.

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

Band Bass Clarinet, Bass Drum, Bassoon, Bells, Clarinet 1, Clarinet 2, Crash Cymbals, Euphonium, Euphonium T.C., Flute, Flute 2, Horn, Mallet Percussion, Oboe, Percussion 1, Percussion 2, Snare Drum, Suspended Cymbal, Timpani, Tom-tom, Trombone and more. - Grade 1.5

SKU: CF.FPS155

Composed by Larry Clark. First Plus Band (FPS). Set of Score and Parts. With Standard notation. 8+2+4+4+2+5+2+2+4+4+4+6+3+2+1+2+3+16+2 pages. Duration 2 minutes, 11 seconds. Carl Fischer Music #FPS155. Published by Carl Fischer Music (CF.FPS155).

ISBN 9781491152157. UPC: 680160909650.

Quest for the Throne evokes images of kings and castles, knights and horses, and dragons in all their glory. It is a bold and aggressive piece throughout, but includes a contrasting, lush secondary theme for variety. In his typical style, Clark has used forceful figures, and strong melodic content to give students music they'll want to practice and play again and again.
This piece should depict images of kings and castles, knight and horses, dragons and damsels in distress. It should be bold and aggressive throughout, but never with bad tone. This is then contrasted by the lush second theme that is presented first in a softer thin orchestration, but later becomes a change for the whole ensemble to play in a strong, but lush presentation of this theme.One thing that is important to me when writing music for younger students is to offer pieces that challenge all students in the ensemble and give every section an important part of the musical presentation, which naturally should include some melodic material. Every member of the ensemble wants to feel that they are contributing to the collective whole.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 2018.

Accordion (keyboard) - Beginning-Intermediate

SKU: MB.97069

Composed by Herman Troppe. Saddle-stitched, Piano Accordion, Style. Archive Edition. Latin American. Book. 24 pages. Mel Bay Publications, Inc #97069. Published by Mel Bay Publications, Inc (MB.97069).

ISBN 9780786635252. UPC: 796279049689. 8.75 x 11.75 inches.

Sixteen solos for keyboard accordion on folk songs from Venezuela, Haiti, Brazil, Chile, Colombia, Costa Rica, the Dominican Republic, Honduras, Panama, Paraguay, and Peru.

Flute and Piano. By Christopher Norton. (Flute). Boosey and Hawkes Chamber Music. Book only. 104 pages. Published by Boosey and Hawkes.