Composed by Scott Joplin (1868-1917). For solo piano. Schirmer's Library, volume 2020. Format: piano solo songbook. With introductory text. Ragtime. 196 pages. 9x12 inches. Published by G. Schirmer, Inc..

For piano four-hands. Duet or Duo; Piano Duet (1 Piano, 4 Hands). Jazz, Rags and Blues for Two. Jazz, Blues and Ragtime. Intermediate. Collection. 24 pages. Published by Alfred Music Publishing

(8 Ragtime Pieces for Piano). By Larry Porter. For Piano. Piano. Softcover. 38 pages. Schott Music #ED21465. Published by Schott Music

For guitar. Transcribed by Ernie Hawkins, Historical notes by William L. Ellis. Guitar: Fingerpicking, Blues, Ragtime. Intermediate-Advanced. Book/CD Set. 108 pages. Published by Mel Bay Publications, Inc

By Benedikt Brydern. For Violin. Duets. Ragtime. Level: Beginning-Intermediate. Book. 36 pages. Published by Mel Bay Publications, Inc.

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.

A Three Volume DVD Collection. Taught by Stefan Grossman. For Guitar (Fingerpicking). Concert/documentary. Grossman-Gtr Workshop. Country. DVD. Size 5.25x7.5. Duration 196 minutes. Published by Grossman's Guitar Workshop. (GW904SDVD) DVD format: Region 1 for use in the USA and Canada.

Arranged by Giovanni De Chiaro. For Guitar (Classical). Solos. Editiones Classicae. Ragtime. Level: Intermediate. Book. Size 8.75x11.75. 288 pages. Published by Mel Bay Publications, Inc.

A Collection of Cakewalks, Rags, Slow Drags, and Foxtrots from the Gilded Age. Fretted. Jazz, Ragtime, Standards. Softcover. Published by Centerstream Publications

Multiple authors. For Guitar (Flatpicking and Fingerpicking). Concert/Documentary. Vestapol. Country. Level: Beginning. DVD. Size 5.25x7.5. Duration 58 minutes. Published by Grossman's Guitar Workshop.

By James Bastien. (Bastien Supplementary Books). Bastien Piano. Pop/Rock/Country. Level: Level 3. Music Book. Size 232. Published by Neil A. Kjos Music Company.

Entertainer and Maple Leaf * 2 in 1 * Easy Piano Solo composed by Scott Joplin (1868-1917). Arranged by Tony Santorella. For easy piano solo. This edition: Paperback. Solo. Ragtime. Sheet Music. Text Language: English. 12 pages. Published by Santorella Publications

The Roots of Bluegrass Guitar. Taught by Eric Thompson. For Guitar (Flatpicking/Plectrum). Method. Grossman-Gtr Workshop. Bluegrass and Country. Level: Intermediate. DVD. Size 5.25x7.5. Duration 73 minutes. Published by Grossman's Guitar Workshop

By James Bastien. (Bastien Supplementary Books). Bastien Piano. Pop/Rock/Country. Level: Level 2. Music Book. Size 232. Published by Neil A. Kjos Music Company.

Arranged by various, ed. Bill Galliford. Instrumental Series; Play-Along. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47345. Published by Alfred Music

Arranged by various, ed. Bill Galliford. Instrumental Series; Play-Along. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47333. Published by Alfred Music

Arranged by various, ed. Bill Galliford. Instrumental Series; Play-Along. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47339. Published by Alfred Music

Arranged by various, ed. Bill Galliford. Play-Along; String Series. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47348. Published by Alfred Music

Arranged by various, ed. Bill Galliford. Instrumental Series; Play-Along. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47342. Published by Alfred Music

Arranged by various, ed. Bill Galliford. Instrumental Series; Play-Along. Instrumental Solos Series. Country; Pop; Radio. Book; CD. 24 pages. Alfred Music #00-47327. Published by Alfred Music