Edited by David Brody. For violin. Format: fake book. With lead melody, chord na...(+)
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.
Edited by Alexander Shealy. For recorder. Format: recorder book (solos, duets, t...(+)
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.
Good As Hell Fanfare [Conducteur et Parties séparées] - Intermédiaire Hal Leonard
By Lizzo. By Eric Frederic and Lizzo. Arranged by Jack Holt and Matt Conaway. ...(+)
By Lizzo. By Eric
Frederic
and Lizzo. Arranged by
Jack
Holt and Matt Conaway.
Contemporary Marching
Band.
Pop, Rap. Softcover.
Published by Hal Leonard
Performed by The Beatles. For voice(s), guitar(s), bass guitar, drum set and key...(+)
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 Ca...(+)
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
Piano/Vocal/Guitar SKU: HL.380355 By Various. Piano/Vocal/Guitar Songbook...(+)
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.
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.