Free range

Waiting to come onstage is one of the most terrifying experiences one can have. Knowing that in around three or so minutes you will be called onstage to be judged and viewed by an awaiting crowd of your peers strikes you to the core and puts the familiar pang of pressure and anxiety straight into your stomach. Which takes us to the beginning of our story; enter, me, in a blonde shoulder length wig. I am dressed in a flowing white shirt, laced with frills and puffed sleeves. Atop my shirt lays my

lake was formed was due to the collapse of a volcano ,known as Mount Mazama. Its max depth is 1.949ft. Oregon consists of 6 different areas. The coast, Klamath mountains , Willamette lowlands,Cascade Mountains, Columbia Plateau , and the basin and range region. The Pacific shoreline of Oregon is bordered by narrow coastal plains of sandy beaches, luxuriant

The concert was a joint concert with choir and band. The genres choir sang were church music and lullabies and band played various genres including pop, classical, and holiday music. Some songs choir sang was “The Word Was God” and “Riversong.” Band played songs such as “Phantom of the Opera,” Beethoven symphony No. 5. The instrument choir used was their voices and a piano. Band used a variety of instruments such as trumpets, trombones, tubas, French horns, clarinets, flutes, saxophones, piccolos

Of Mice & Men Alternate Ending George aimed the gun and steadied it, and he brought the muzzle of the gun close to the back of Lennies head. The hand shook violently, but his face set and his hand steadied, Georges heart was pounding, Lennie was still looking across the river trying to picture his rabbits as he was told to do. George suddenly jerked his hand away as Lennie spoke. "Don stop now George, tell, tell about the rabbits and the fatta the lan" But George

primarily granodiorite and quartz are all over the Cascade Range, forming the Grotto/Index (~25m.y.) and Snoqualmie (~18m.y.) Batholiths of common rock types. More recent Swauk sedimentary structures are seen as overlap from the nearby Blewitt (formerly Swauk) Pass region, likely formed as result of the last ice age1,2,5. These sedimentary layers fade out deeper into the mountains, as the igneous intrusions become more predominant within the range. White and black-grained diorite is common and clearly

Shrimp survival rate (%) is correlated with the crop duration in 2012 (p = 0.0006, r = 0.75) and in 2013 (p = 0.0031, r = 0.71). Shrimp yield (kg/ha/crop) was correlated with the crop duration in 2012 (p = 0.0028, r = 0.68) and in 2013 (p = 0.0016, r = 0.74). The crop duration is negatively correlated with average culture period water temperature, while it is positively correlated with CV of hourly water temperature, and with the count of hours fall in the following temperature zones: out of best

Referring to Fig. 1(ii), consider in region II, the reference voltage vector is following the arc x1x2 at a particular modulation index m. The position of the reference voltage vector is shown in Table 1. It shows that, depending on modulation index value, the duration of stay within subsector 1 and subsector 2 changes. Similarly, consider in region III, the reference voltage vector is following the arc y1y2 at aparticular modulation index. The position of the reference voltage vector is shown in

Mount Saint Helens is a volcano located in southwestern Washington. It is 8,363 feet tall. Geologists say that Mount St. (Saint) Helens is a stratovolcano, also known as a composite volcano. Stratovolcano is a volcano that is built upward because of layers of hardened volcanic ash, lava, and other volcanic debris. These kinds of volcanoes are distinguished by their steep sides. They often erupt extremely explosively, putting people and properties nearby at risk. The present-day name, Mount Saint

how they were formed and when they last had an eruption. Let’s begin with Mount St. Helens which is located in the pacific northwest of the United States. To be more specific it is located in Washington State and is a part of the Cascade mountain range that spans from California to Canada. It is a composite volcano, which has steep sides that are formed by alternating layers of lava

the Mass. For the sake of this discussion, we will focus on the Credo. In this paper, I will examine the works of Joseph Haydn and Giovanni Palestrina and compare certain elements such as the length, instrumentation, rhythm, articulation, dynamics, range, language, melody, and harmony. The analysis will be taken from Haydn’s “Nelson Mass” (1798) and Palestrina’s “Missa Papae Marcelli”. First, let us determine the differences in length between the two Credos. In Haydn’s work, the piece extends for