By Richard Matteson, Jr. For Fretted. Tune book. Bluegrass. Level: Beginning. Book. Size 8.75x11.75. 248 pages. Published by Mel Bay Publications, Inc.

By George Gershwin, Ira Gershwin. For Piano/Vocal/Chords. This edition: Piano/Vocal/Chords. Personality Book. Broadway. Book. 260 pages. Published by Alfred Publishing.

(Words and Chords to Nearly 1200 Songs 9x12 Spiral Bound). Edited by Annie Patterson and Peter Blood. For Vocal. Vocal. Softcover. 304 pages. Published by Hal Leonard

(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

The Group Singing Songbook. By Various. Vocal. Size 9.5x12 inches. 281 pages. Published by Hal Leonard.

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

By Howard Goodall. Choir Secular. For with Piano (3-Part Mixed Choir (SAB)). Book; Choral Collection. Faber Edition: Choral Basics. Published by Faber Music

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

SKU: CF.FPS156

Composed by Joseph Compello. Folio. Fps. Set of Score and Parts. 8+2+4+4+2+5+2+2+4+4+4+6+2 +3+2+1+2+3+16 pages. Duration 2 minutes, 50 seconds. Carl Fischer Music #FPS156. Published by Carl Fischer Music (CF.FPS156).

ISBN 9781491156360. UPC: 680160914906. 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.

Composed by Normand Gouin. Parish Choral Series. Catholic Year C Ordinary28; Catholic Year C Ordinary29; Year C Pentecost22;. Faith, Hope/Assurance, Praise/Thanksgiving, Trust/Guidance. Octavo. Published by MorningStar Music Publishers (MN.50-8508).

SATB choir (a cappella)

SKU: LO.10-5572L

Composed by Bryan Sharpe. Choral. Sacred Anthem. Octavo. Lorenz Publishing Company #10/5572L. Published by Lorenz Publishing Company (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!

Arranged by Tim Sharp. Gentry Publications. Octavo. 8 pages. Gentry Publications #JG2520. Published by Gentry Publications

Kantele - beginning Folk, Perfect binding. Method. Book and online audio. 116 pages. Mel Bay Publications, Inc #30857M. Published by Mel Bay Publications, Inc

Violin and Piano

SKU: YM.GTW01100445

Composed by Various. Japanese Traditional Songs; Strings. Score and part. Yamaha Music Media #GTW01100445. Published by Yamaha Music Media (YM.GTW01100445).

ISBN 9784636103052. 8.5 x 12 inches.

Here, you can enjoy the beautiful Japanese classic tunes expressing the changing seasonal sentiments in this book. It features 25 songs, mainly nursery rhymes, children's songs, and shoka songs, and it comes with a karaoke CD of piano accompaniment. Please enjoy these wonderful arrangements, which are perfect for recitals and concerts.

Choir Secular (Women's Choir)

SKU: AP.49658

Composed by Alan Chang, Amy Foster, and Michael Buble. Arranged by Kirby Shaw. Performance Music Ensemble; Single Titles. Alfred Pop Choral Series. Contemporary A Cappella; Pop; Radio; Secular. Choral Octavo. 12 pages. Alfred Music #00-49658. Published by Alfred Music (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.

Choir Secular (SATB choir)

SKU: AP.49657

Composed by Alan Chang, Amy Foster, and Michael Buble. Arranged by Kirby Shaw. Performance Music Ensemble; Single Titles. Alfred Pop Choral Series. Contemporary A Cappella; Pop; Radio; Secular. Choral Octavo. 12 pages. Alfred Music #00-49657. Published by Alfred Music (AP.49657).

UPC: 038081567440. 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.

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.

(Inspiring Ballads and Romantic Standards Sung by Great Female Vocalists). By Various. Piano/Vocal/Guitar Songbook. Softcover. 312 pages. Published by Hal Leonard

Paperback Lyrics. By Various. Paperback Lyrics. Softcover. Size 4.25x6.75 inches. 256 pages. Published by Hal Leonard.

By Bob Dylan. By Bob Dylan. Arranged by Don Giller and Ed Lozano. Music Sales America. Folk, Pop, Rock. Softcover. Composed 2016. 788 pages. Music Sales #AM978923. Published by Music Sale