By The Beatles. Bass Recorded Versions Persona. Pop. Softcover. 184 pages. Published by Hal Leonard

By Various. Easy Piano Songbook. Softcover. 288 pages. Music Sales #AM1011461. Published by Music Sales

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.

Easy ABC/Letter Music (Big notes with the note names written on them). Size 9x12 inches. 176 pages. Published by Hal Leonard.

(Book/USB Flash Drive Play-Along Pack). By Various. For C Instruments. Real Book Play-Along. USB Flash Drive. 462 pages. Published by Hal Leonard

(USB Flash Drive Play-Along). By Various. For C Instruments. Real Book Play-Along. USB Flash Drive. Published by Hal Leonard

(Budget Books). By Various. Easy Piano Songbook. Softcover. 304 pages. Published by Hal Leonard

Edited by Alexander Shealy. For recorder. Format: recorder book (solos, duets, trios). With standard notation, chord names, instructional text, fingering charts and lyrics. Instructional and folk. Series: World's Favorite Series, No. 50. 128 pages. 9x12 inches. Published by Ashley Publications.

By Lizzo. By Eric Frederic and Lizzo. Arranged by Jack Holt and Matt Conaway. Contemporary Marching Band. Pop, Rap. Softcover. Published by Hal Leonard

(facsimile score). Composed by David Maslanka. For Saxophone Trio, Wind Ensemble. Full score - large. Published by Carl Fischer

Performed by The Beatles. For voice(s), guitar(s), bass guitar, drum set and keyboard. Format: full score. With vocal melody, lyrics, standard guitar notation, guitar tablature, standard bass notation, bass tablature, chord names and drum notation. Classic rock, pop rock and psychedelic rock. Popular boxed gift set. Includes complete transcriptions of all instrumental and vocal parts. Series: Hal Leonard Transcribed Scores. 1136 pages. 7.25x10.88 inches. Published by Hal Leonard.

Piano, Vocal and Guitar

SKU: BT.MUSAM1001286

By Jenni Wheeler. By Glee Cast. TV-Film-Musical-Show. Book Only. Wise Publications #MUSAM1001286. Published by Wise Publications (BT.MUSAM1001286).

ISBN 9781849386425.

The matching folio for the third Glee album, featuring 20 songs, including those from the deluxe edition, in arrangements for Piano and Voice with Guitar chord boxes.

As with the other albums, a wide cross-section ofmusicalgenres is featured, from the cover of alt. rock hit Gives You Hell by the All-American Rejects, to the heart-wrenching musical classic from Les Miserables, I Dreamed a Dream, and everything in-between,includingtwo Lady Gaga numbers, Poker Face and Bad Romance!

GLEE , de Amerikaanse High School hit, wordt ook uitgezonden op de Nederlandse televisie en is een enorm succes. Vanaf 14 september 2010 is deze serie te zien bij RTL 5 en de kijkcijfers hebben zich na de eerste paar uitzendingen verdubbeld.Glee bevat humor, spanning, cheerleeders, footballspelers en flink wat tienerdrama, maar onderscheidt zich sterk van andere soortgelijke programma's door de bijzondere muziek in de serie. Er worden namelijk nummers vanbekende artiesten gezongen, die in een nieuw hip jasje gestoken zijn. Glee is hierdoor hard op weg om de grootste hype van dit seizoen te worden!Leverbaar:G lee Songbook: Season 1, Volume 1 Glee Songbook: Season 1, Volume 2 GleeSongbook: Season 1, Volume 3

E-flat Edition. Composed by Various. Fake Book. Jazz. Softcover. 504 pages. Published by Hal Leonard (HL.175279).

B-flat Edition. Composed by Various. Fake Book. Softcover. 504 pages. Published by Hal Leonard

(C Edition). By Various. By Various. For C Instruments. Fake Book. Softcover. 464 pages. Published by Hal Leonard

Easy Piano Songbook. By Billie Eilish. Easy Piano Personality. Pop. Softcover. 72 pages. Published by Hal Leonard

Piano/Vocal/Guitar

SKU: HL.380355

By Various. Piano/Vocal/Guitar Songbook. Pop. Softcover. 176 pages. Published by Hal Leonard (HL.380355).

ISBN 9781705152065. UPC: 196288018988. 9.0x12.0x0.414 inches.

Need to bring more good vibes into your day? This collection features 30 feel-good favorites from yesterday and today arranged for piano/vocal/guitar, including: Best Day of My Life (American Authors) • Cover Me in Sunshine (P!nk & Willow Sage Hart) • Don't Stop Me Now (Queen) • Good Day Sunshine (The Beatles) • Good Vibrations (The Beach Boys) • Happy (Pharrell Williams) • Lovely Day (Bill Withers) • Rise Up (Andra Day) • This Is Me (from The Greatest Showman) • Walking on Sunshine (Katrina & the Waves) • What a Wonderful World (Louis Armstrong) • and more.

Songbook for voice and easy piano. Series: Hal Leonard Easy Adult Piano. 96 pages. Published by Hal Leonard.

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.