Format : Score and Parts
SKU: HL.287332
UPC: 888680903671. 5.0x5.0x0.16 inches.
A pivotal moment in the 2018 remake of A Star Is Born, Shallow marks the moment at which Lady Gaga's Ally is thrust into the spotlight and the title of the film is fulfilled. Marked by a beautiful and conversational opening passage with opportunities for soloists, the back half of the arrangement stays true to the original melody with effective harmonies, country rock phrasing and a musical assuredness that juxtaposes phenomenally with the hardship and all-or-nothing rhetoric that the text presents.
SKU: M7.MF-3610
ISBN 9783795716967.
Easy Charts Play-Along 10 is the latest installment of the successful series that allows up-and-coming musicians to play and enjoy hits from the charts. Including Bella Ciao by the French DJ El Profesor, the Oscar-winning song Shallow by Lady Gaga and Bradley Cooper and Shotgun by the British singer George Ezra. All arrangements are available for C, Bb and Eb instruments and can be played by a variety of instruments, such as flute, clarinet, saxophone, and trumpet.
SKU: HL.291634
ISBN 9781540049377. UPC: 888680927844. 9.0x12.0x0.103 inches. Pop Piano Hits Series.
Pop Piano Hits is a series designed for students of all ages! Each book contains five simple and easy-to-read arrangements of today's most popular downloads. Lyrics, fingering and chord symbols are included to help you make the most of each arrangement. Enjoy your favorite songs and artists today! This edition contains: High Hopes (Panic! at the Disco) * No Place like You (Backstreet Boys) * Shallow (Lady Gaga and Bradley Cooper) * Sunflower (Post Malone) * Without Me (Halsey).
SKU: HL.360467
ISBN 9781789361858. UPC: 840126990553. 9.0x12.0x0.205 inches.
Learn to play rock and pop with Rockschool. These specially written arrangements develop the skills and techniques you need to help you achieve your musical goals. Rockschool has commissioned arrangements of titles reflecting popular music's rich heritage in all its forms and have tailored each piece to make it exactly right for the grade. You can also use titles from Rockschool's Classics series as part of the syllabus. The arrangements have been written and performed by top session musicians who have worked with some of the biggest names in rock, metal and pop. The tracks were recorded at Real World's acclaimed recording studios and feature live instruments and first rate performances for an unrivalled level of feel, authenticity and musicianship. Featuring: Everybody Hurts (R.E.M.) • Let Her Go (Passenger) • Other Side of the World (KT Tunstall) • Shallow (Lady Gaga & Bradley Cooper) • (Sittin' on) The Dock of the Bay (Otis Redding) • We Are Never Ever Getting Back Together (Taylor Swift) • and six Rockschool originals. Plus: • Band and artist fact files with recommended listening • In-depth walkthroughs of every track • Easy-access downloadable audio • Example tests and exercises.
SKU: HL.298905
ISBN 9781540059901. UPC: 888680955274. 9.0x12.0x0.556 inches.
This updated second edition features 100 songs from the silver screen in larger-than-usual fake book notation and all in the key of C. Songs include: Born Free • Chariots of Fire • City of Stars (from La La Land) • Endless Love • Footloose • Ghostbusters • Happy (from Despicable Me 2) • I Will Always Love You (from The Bodyguard) • Theme from Jaws • Let It Go (from Frozen) • A Million Dreams (from The Greatest Showman) • My Heart Will Go On (Love Theme from Titanic) • Nine to Five • Over the Rainbow (from The Wizard of Oz) • Shallow (from A Star Is Born) • Singin' in the Rain • Summer Nights (from Grease) • (I've Had) The Time of My Life (from Dirty Dancing) • The Wind Beneath My Wings (from Beaches) • Yellow Submarine • and more.
SKU: HL.322944
ISBN 9781540070111. UPC: 888680977009. 9.0x12.0x0.165 inches.
If you've been taking Glockenspiel lessons for a while, you're probably eager to learn some familiar songs. The First 50 Songs You Should Play on the Bells/Glockenspiel includes a wide variety of favorite songs, from pop hits and movie themes to folk songs and classical melodies, several of which originally featured bells! Songs include: All of Me • All You Need Is Love • Canon in D • Carnival of Venice • Fight Song • The Fool on the Hill • God Bless America® • The Godfather (Love Theme) • Hallelujah • Happy • Hello • I Will Always Love You • Just Give Me a Reason • Let It Go • Pure Imagination • Roar • Rolling in the Deep • Satin Doll • Shake It Off • Shallow • Stand by Me • Stay with Me • This Is Me • Ukranian Bell Carol • What a Wonderful World • and more.
About First 50
You've been taking lessons, you've got a few chords under your belt, and you're ready to buy a songbook. Now what? Hal Leonard has the answers in its First 50 series. The First 50 series steers new players in the right direction. These books contain easy to intermediate arrangements for must-know songs. Each arrangement is simple and streamlined, yet still captures the essence of the tune.
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.