Composed by Matt Turner. For string orchestra (violin I, violin II, violin I...(+)
Composed by Matt Turner.
For
string orchestra (violin
I,
violin II, violin III
(viola
T.C.), viola, cello,
bass,
drums, piano). Score and
parts. Duration 3
minutes, 02
seconds. Published by
Carl
Fischer
12-String Guitar SKU: HL.287559 By Various. Guitar Collection. Pop, Stand...(+)
12-String Guitar
SKU:
HL.287559
By Various.
Guitar Collection. Pop,
Standards. Softcover.
With guitar tablature.
120 pages. Published by
Hal Leonard (HL.287559).
ISBN 9781540043313.
UPC: 888680904715.
9.0x12.0x0.299
inches.
This
one-of-a-kind collection
presents accessible,
must-know songs from the
Beatles and Bob Dylan to
Dave Matthews Band and
Tom Petty for those who
have been learning
12-string guitar and are
eager to put their new
skills to work. You'll
find a combination of
tab, chords and lyrics
for 50 great songs,
including: California
Dreamin' • Carry On
• Closer to the
Heart • Do You
Believe in Magic •
Free Fallin' • Give
a Little Bit • A
Hard Day's Night •
Hotel California •
Leaving on a Jet Plane
• Life by the Drop
• Like the Way I Do
• Melissa •
Mr. Tambourine Man
• More Than a
Feeling • The One I
Love • Over the
Hills and Far Away
• Solsbury Hill
• Space Oddity
• Still the Same
• Turn! Turn! Turn!
(To Everything There Is a
Season) • The
Waiting • Wish You
Were Here • You
Wear It Well • 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.
(Words and Chords to Nearly 1200 Songs 9x12 Spiral Bound). Edited by Annie Patte...(+)
(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 ...(+)
(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
E-Z Play Today (Easy big-note right-hand-only arrangements for piano, organ, and...(+)
E-Z Play Today (Easy
big-note right-hand-only
arrangements for piano,
organ, and electronic
keyboard). Size 9x12
inches. 152 pages.
Published by Hal Leonard.
E-Z Play Today #13. By Various. E-Z Play Today (Easy big-note right-hand-only ar...(+)
E-Z Play Today #13. By
Various. E-Z Play Today
(Easy big-note
right-hand-only
arrangements for piano,
organ, and electronic
keyboard). Softcover. 96
pages. Published by Hal
Leonard.
E-Z Play Today (Easy big-note right-hand-only arrangements for piano, organ, and...(+)
E-Z Play Today (Easy
big-note right-hand-only
arrangements for piano,
organ, and electronic
keyboard). Size 9x12
inches. 96 pages.
Published by Hal Leonard.
By Various. E-Z Play Today (Easy big-note right-hand-only arrangements for piano...(+)
By Various. E-Z Play
Today (Easy big-note
right-hand-only
arrangements for piano,
organ, and electronic
keyboard). Size 9x12
inches. 368 pages.
Published by Hal Leonard.
For C instrument and voice. Format: fakebook (spiral bound). With chord names, v...(+)
For C instrument and
voice. Format: fakebook
(spiral bound). With
chord names, vocal melody
and lyrics. Jazz. Series:
Hal Leonard Fake Books.
448 pages. 9x12 inches.
Published by Hal Leonard.
Fakebook for Eb instrument and voice. With vocal melody, lyrics and leadsheet no...(+)
Fakebook for Eb
instrument and voice.
With vocal melody, lyrics
and leadsheet notation.
Series: Hal Leonard Fake
Books. 448 pages.
Published by Hal Leonard.
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.
SAB choir, assembly,
keyboard accompaniment,
flute, piccolo, guitar -
Beginning
SKU:
GI.G-8755
Announce
the Good News.
Composed by Rory Cooney.
Advent, OT 3 B, OT 3 C,
OT 5 B, OT 32, OT 33, OT
33 A. Celebration Series.
Sacred. Octavo. With
guitar chord names. 8
pages. GIA Publications
#8755. Published by GIA
Publications (GI.G-8755).
UPC: 785147875505.
English. Text by Rory
Cooney.
The closing
text, “Turn around
and believe in the
gospel,†will
strike a memorable chord
in your congregation when
this joyous piece is
introduced to them.
Flexible instrumentation
options, including a part
for flute or piccolo,
help enliven the already
bright and rhythmic feel
of this piece. Let your
choir announce the good
news to your congregation
and, in turn, your
congregation announce it
to the world! Flute or
Piccolo.
Ligne De Mélodie, Paroles et Accords [Fake Book] - Facile Hal Leonard
For voice and C instrument. Format: fakebook (spiral bound). With vocal melody, ...(+)
For voice and C
instrument. Format:
fakebook (spiral bound).
With vocal melody,
lyrics, piano
accompaniment, chord
names and leadsheet
notation. Hymn. Series:
Hal Leonard Fake Books.
494 pages. 9x12 inches.
Published by Hal Leonard.
