SKU: HL.1438381

ISBN 9798350123692. UPC: 196288204893.

The '60s were a game-changing decade for tunes, kicking off with The Beatles leading the charge from across the pond with the soul-stirring beats of Motown. It was a time when music festivals like Woodstock weren't just about music; they were massive statements of peace, love, and rebellion against the status quo. Travel back in time with this new Super Easy sonbook featuring 46 simple arrangements of this decade's hits to start playing your favorite songs in no time! Each song is arranged with simple right-hand melody, letter names inside each note, basic left-hand chord diagrams, and no page turns. Songs include: Are You Lonesome Tonight? • Bad Moon Rising • Build Me Up, Buttercup • California Dreamin' • Downtown • God Only Knows • Happy Together • I Got You Babe • I Want to Hold Your Hand • I'm a Believer • Light My Fire • Like a Rolling Stone • Mrs. Robinson • On a Clear Day (You Can Seee Forever) • On Broadway • (I Can't Get No) Satisfaction • Somebody to Love • Surfin' U.S.A • Suspicious Minds • Will You Love Me Tomorrow (Will You Still Love Me Tomorrow) • and more!

SKU: CF.FPS156F

ISBN 9781491156377. UPC: 680160914913. 9 x 12 inches.

Personal Note My high school band director, Clarence F. Wroblewski, died on November 24, 2018. In the 1950s, he was a pioneer in the field of public school instrumental music in Baltimore City. He was my mentor and my dear friend. It was his guidance and encouragement that set my young life's course on the path of music. Performance Notes The idea for Ghost Chasers is to have a spooky tune (m. 9, Trumpets) chasing around in simple counterpoint between two sections. (See m. 19). Students will find the independent part playing both challenging and fun. In the contrasting section at m. 30, young students will gain experience in changing their articulation from marcato to legato. Obeying the cues for low brass in this section is recommended, but depending on the instrumentation of the band, directors may disregard the cues if necessary. Directors may also wish to take the opportunity to teach a lesson about major and minor keys and discuss why the tune at m. 9 sounds spooky and the theme at m. 30 sound lighthearted. Overall, the main challenge for this piece is balance. For the chaser idea to be effective the half-measure lag between the two sections playing the same tune must be easily heard. Even more attention to balance must be paid at m. 45, where the spooky theme is added to the chasing theme. If Clarinets can play third-line written D, use it instead of the alternate cued note. If three Timpani are not available, omit the note D.
Personal NoteMy high school band director, Clarence F. Wroblewski, died on November 24, 2018. In the 1950s, he was a pioneer in the field of public school instrumental music in Baltimore City. He was my mentor and my dear friend. It was his guidance and encouragement that set my young life’s course on the path of music.Performance NotesThe idea for Ghost Chasers is to have a spooky tune (m. 9, Trumpets) chasing around in simple counterpoint between two sections. (See m. 19). Students will find the independent part playing both challenging and fun.In the contrasting section at m. 30, young students will gain experience in changing their articulation from marcato to legato. Obeying the cues for low brass in this section is recommended, but depending on the instrumentation of the band, directors may disregard the cues if necessary. Directors may also wish to take the opportunity to teach a lesson about major and minor keys and discuss why the tune at m. 9 sounds spooky and the theme at m. 30 sound lighthearted.Overall, the main challenge for this piece is balance. For the “chaser” idea to be effective the half-measure lag between the two sections playing the same tune must be easily heard. Even more attention to balance must be paid at m. 45, where the “spooky” theme is added to the “chasing” theme.If Clarinets can play third-line written D, use it instead of the alternate cued note. If three Timpani are not available, omit the note D.

SKU: LO.10-5572L

ISBN 9780787773465.

With a Gospel, swing feel, this original a cappella anthem is an upbeat tune with text inspired by Psalm 23. Utilizing choral layering, rhythmic variations, stylistic articulation, and changing dynamics, choirs will love singing it and get your congregation's toes tapping along!

SKU: AP.49658

UPC: 038081567457. English.

Here's a cute, quick (two-minute) rendition of the Michael Bublé hit. Heartfelt lyrics recognize that despite living in crazy times, a special person in your life makes it worthwhile. No solo or vocal percussion required---this contemporary a cappella arrangement covers the tune with the choir and incorporates aspirated chk's as built-in rhythm. Additionally, doom's in the lowest voice part layout a supportive bass line, and a catchy La la refrain stays in the ear long after the final cutoff. Equally effective with large groups or small ensembles.

About Alfred Pop Choral Series

The Alfred Pop Series features outstanding arrangements of songs from the popular music genre. These publications provide exciting, contemporary, and educationally-sound arrangements for singers of all ages, from elementary through high school, to college and adult choirs.

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.