| The Folksong Fake Book - C Edition
Fake Book [Fake Book] Hal Leonard
For voice and C instrument. Format: fakebook. With vocal melody, lyrics and chor...(+)
For voice and C
instrument. Format:
fakebook. With vocal
melody, lyrics and chord
names. Folk. Series: Hal
Leonard Fake Books. 536
pages. 9.6x12 inches.
Published by Hal Leonard.
(10)$34.99 - Voir plus => AcheterDélais: 24 hours - In Stock | | |
| IronHeart Orchestre d'harmonie [Conducteur et Parties séparées] - Débutant Alfred Publishing
Composed by Randall D. Standridge. Concert Band. Concert Band; Part(s); Sc...(+)
Composed by Randall D.
Standridge. Concert Band.
Concert Band; Part(s);
Score. Alfred Debut
Series.
Grade 1.5. 138 pages.
Published by Alfred Music
$48.00 $45.6 (- 5%) Voir plus => AcheterDélais: 1 to 2 weeks | | |
| Red Rock Rag Orchestre à Cordes - Intermédiaire Carl Fischer
Orchestra String Orchestra - Grade 3 SKU: CF.CAS7 Composed by Doris Gazda...(+)
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. $60.00 - Voir plus => AcheterDélais: 1 to 2 weeks | | |
| Iron Mountain Hal Leonard
Score and Parts Concert Band (Score & Parts) - Grade 1 SKU: HL.4008937 (+)
Score and Parts Concert
Band (Score & Parts) -
Grade 1 SKU:
HL.4008937 Concert
Band, Grade 1 4:30 Score
and Parts. Composed
by Gerald Oswald.
Symphonic Dimensions.
Concert, Concert Band.
Softcover. Duration 270
seconds. Hal Leonard
#SDP222-24-02. Published
by Hal Leonard
(HL.4008937). UPC:
196288281641. “Ir
on Mountain” portrays
the legend of the Erzberg
in Austria in an
impressive musical
manner. At the beginning,
the atmosphere of the
cave where the Waterman
resides comes to life
through simulated water
droplets. The Waterman is
pursued and captured by
humans. In his
desperation, he pleads
for freedom and presents
an offer to the people:
gold mines for a year,
silver mines for ten
years, oriron mines
forever. The clear
response from the people
is iron forever. The
composition's finale
emphasizes this choice
with impactful anvil
strikes, and the Erzberg
rises triumphantly to the
forefront of the
narrative. $98.00 - Voir plus => AcheterDélais: 2 to 3 weeks | | |
| Iron Mountain Hal Leonard
Concert Band (Score) - Grade 1 SKU: HL.4008938 Concert Band, Grade 1 4...(+)
Concert Band (Score) -
Grade 1 SKU:
HL.4008938 Concert
Band, Grade 1 4:30
Score. Composed by
Gerald Oswald. Symphonic
Dimensions. Concert,
Concert Band. Softcover.
Duration 270 seconds. Hal
Leonard #SDP222-24-01.
Published by Hal Leonard
(HL.4008938). UPC:
196288281658. “Ir
on Mountain” portrays
the legend of the Erzberg
in Austria in an
impressive musical
manner. At the beginning,
the atmosphere of the
cave where the Waterman
resides comes to life
through simulated water
droplets. The Waterman is
pursued and captured by
humans. In his
desperation, he pleads
for freedom and presents
an offer to the people:
gold mines for a year,
silver mines for ten
years, oriron mines
forever. The clear
response from the people
is iron forever. The
composition's finale
emphasizes this choice
with impactful anvil
strikes, and the Erzberg
rises triumphantly to the
forefront of the
narrative. $21.99 - Voir plus => AcheterDélais: 2 to 3 weeks | | |
| Metropolitan Piano seul Theodore Presser Co.
Chamber Music Piano SKU: PR.110418240 For Piano. Composed by Charl...(+)
Chamber Music Piano
SKU: PR.110418240
For Piano.
Composed by Charles Peck.
Sws. Performance Score.
16 pages. Duration 13
minutes. Theodore Presser
Company #110-41824.
Published by Theodore
Presser Company
(PR.110418240). ISBN
9781491133835. UPC:
680160683338. 9 x 12
inches. This
cosmopolitan 5-movement
suite was inspired by the
multitudinous energy in
every city, where people
from all walks of life
intersect in close
proximity. The resulting
experience breeds
collaboration for the
inspired, ambition for
the eager, danger in the
masses, beauty in the
diversity, coldness in
the operation, power in
the structure, and
everything in between.
The movement titles are:
1. Luminous Canopy, 2.
Urban Glass, 3. Magnetic
Avenue, 4. Iron Organ,
and 5. Midnight City.
METROPOLITAN is also
available for
Orchestra. Metropolita
n was inspired by the
multitude of life
inherent to every city. A
huge variety of people
from all walks of life
comes together, now
united by proximity. The
result is a completely
unique experience that
breeds collaboration for
the inspired, ambition
for the eager, danger in
the masses, beauty in the
diversity, coldness in
the operation, power in
the structure, and
everything in
between.Each movement
explores a different
aspect of this complex
environment. It is the
composer’s hope
that the music may
inform, illuminate, or
resonate with your own
urban
experiences.METROPOLITAN
is also available for
Orchestra. $18.99 - Voir plus => AcheterDélais: 24 hours - In Stock | | |
| Awake the Iron Orchestre d'harmonie [Conducteur] - Débutant Alfred Publishing
By Scott Watson. Concert Band. Concert Band; Score. Alfred Debut Series. Grade 1...(+)
By Scott Watson. Concert
Band. Concert Band;
Score. Alfred Debut
Series. Grade 1.5. 20
pages. Published by
Alfred Music Publishing
(1)$7.00 - Voir plus => AcheterDélais: 1 to 2 weeks | | |
| The New Guitar Big Book of Hits -- British Rock Guitare notes et tablatures Alfred Publishing
(52 Favorites from the U.K. (Guitar TAB)). For Guitar. Book; Guitar Mixed Fo...(+)
(52 Favorites from the
U.K.
(Guitar TAB)). For
Guitar.
Book; Guitar Mixed Folio;
Guitar TAB. The New
Guitar TAB
Big Book. Rock. 272
pages.
Published by Alfred Music
$24.99 - Voir plus => AcheterDélais: 1 to 2 weeks | | |
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