Napa Valley Research Paper

The winery industry can be categorized into red and white wine segments. The red wine segment, measured by tonnage of varietals crushed, has grown at a compounded annual rate of 4.7% for 10 years from 1989 to 1998, and a year over year growth rate of 8.2% from 1998 to 1999. Judging by the strong growth rate experienced in the red wine segment, it is reasonable to conclude that the red wine segment is in the growth phase of the life cycle model. In addition, production of red wine varietals which are relatively unknown such as syrah and sangiovese nearly doubled in a year from 1998 to 1999. The white wine segment, however, is at the mature phase of its life cycle as the segment shrunk slightly by 0.42% from 1998 to 1999. Overall, the industry is still at the growth stage lead by growth in the red wine segment.

With our observation of the Shawangunk formation, we see a sedimentary rock formation containing a range of grain size. Such sizes range from pebbles (3cm-5cm), fine-grain sand, and medium-grain sand. There is some grading towards the bottom left of the outcrop known as a reverse grading with some small cross beds present (Figure 2). The grading occurs towards a slight part of the outcrop where we see the grading beginning as fine grain sediments and working up to coarser grain. With moderate sorting we see variations of degree of sorting per bed. As the degree of sorting varies as does the sphericity. The sediment bedding is well seen ranging in sizes of +/--20 cm to 40 cm. This outcrop has thick beds as one can see the basic units with cracks in between each (Figure 3). With mostly tabular beds consisting of sub-angular, and sub-rounded sediments, this outcrop also consists of some ventricular beds (Figure 4). When looking at figure 4, we have a small space of a ventricular bed present. This is because the bed comes in, pinches thicker bedding,

Ms. Quintana CEO of Northern Napa Valley Winery Inc. was considering conducting business with Trans Continental stores to sell excess grapes from the 2008 harvest. Prior to making a decision Quintana must determine how much of the harvest should be retained for the production of Northern Napa’s own red table wine. Quintana realized that the quantity of red table wine produced is closely associated to the sales.

Sonoma County, California (CA) is located in the central part of the state just northwest of the San Francisco/Oakland area. With a population of around 485,000 (81% white), the residents work mainly in the agricultural industry. Sonoma County, California (CA) is the world famous home of the state's popular wine industry that includes the Napa Valley. Many of the county's current issues related to drug abuse and addiction could be attributed to its proximity to the high crime areas of Oakland to the south.

The west coast of North America has been tectonically and volcanically active for billions of years. The Sierra Nevada Mountains in eastern California were born of volcanoes, and magma has been erupting in the Long Valley to the east of the mountains for over three million years (Bailey, et. al., 1989). However, the climactic eruption of the region occurred relatively recently in the region's geologic history. About 760,000 years ago, a huge explosion of magma warped the Eastern Sierra into the landscape that exists today. The eruption depleted a massive magma chamber below the earth's surface so that the ceiling of the chamber imploded, forming what is now known as

The Variety of grapes planted in Grand Valley vary widely and the yield percentage is relatively low. The styles in wine vary from dry white and red with ice wine as well. Ice wine is a sweet and concentrated wine made from grapes that freeze on the vine. There are many different varietals of wine used in the Grand Valley which include red wines, white wines, and rose wines. White wines consist of merlot, Shiraz, and Cabernet Franc and rose wines consist of Rose’. The TTB, which is the Alcohol and Tobacco tax and trade Bureau, imposes many different requirements on an Ava such as evidence of the name of the proposed AVA is locally or nationally known as referring to the area, historical or current evidence that the boundaries are legitimate, evidence that growing conditions such as

San Joaquin Valley, which encompasses approximately 10,000 square miles, is bounded to the east by the Sierra Nevada Range, to the west by the Coast Ranges, to the south by the Tehachapi Mountains, and to the north by the Sacramento San Joaquin River Delta. The Sierra Nevada Range comprises igneous and metamorphic rocks of pre-Tertiary age, and the granitic rocks of the Sierra Nevada comprise the basement complex beneath the Great Valley. Overlying the basement complex are up to approximately 30,000 feet of Late Cenozoic sedimentary deposits, which are thickest in the central and northern portions of the San Joaquin Valley. The sedimentary units

Most alluvial fan deposits occur near the margins of the depositional basin because they occur in low areas at the base of the Temblor formation or Sierra Nevada’s. The marine deposits, beach

Geographically, Saanich Peninsula is located on the southern end of Vancouver Island, north of the city of Victoria. It has arable land with the mildest climate in Canada. The annual precipitation varies from 635 millimeters in Victoria (city) and increases by 45% in the northern part of the Peninsula, particularly at the airport and nearby areas (Victoria, n.d.). Saanich Peninsula is situated in the south eastern part of the Nanaimo lowland and Vancouver Island ranges. Its eastern side is bordered by Cordova Channel and the western side by Saanich Inlet. The Peninsula is mainly underlain by fractured and faulted volcanic and igneous rocks (i.e., lithosphere). (Huntley et al., n.d; Agriculture and Agri-Food Canada, 1998b). The Peninsula has soils of different texture exposed in sea-cliff and wave-cut platform including sands and gravels; mud, rock; humic; gravely, sandy loam; silt, clay loam; and gravely, loamy sand. Some typical local soils and soil types in the Peninsula are Metchosin, Brigantine, Shawnigan, Langford, Saanichton, Qualicum, Shawnigan etc. (Huntley et al., n.d; Agriculture and Agri-Food

From here the whole valley could be seen and it was easily observed where the glaciers cut into the valley. The second site was a field across from the street from the mudboil. This site was underneath where the slide happened. It used to be farm land, but since the slide the soil has not been able to support anything but invasive species. Additionally, there are now standing pools of salt water in the field that were not there before. Walking through the field the high sulfur content can easily be smelled, which is a result of the slide. The valley face now has a steep grade that was left there after the loss of soil from the slide. The third site was the Onondaga Creek. The creek is extremely turbid due to a high amount of sediment carried by the water. This sediment is lacustrine material, mostly clay, and gets deposited further downstream. The fourth site was a view of the alluvial fan. This is a cone shaped fan that spreads out water and debris. It gives an idea of where the water and soil were forced to go during the slide. The final site was the mudboil and its connection to the Onondaga Creek. Walking into the mudboil there are recessional rings, which are evidence of material slipping and causing an increase in pressure. There is some moving water, but it is from a lateral source. The mudboil itself is formed by a vertical poll of water. The ground in the mudboil looks solid but is actually soft and unsupportive. If there was a need to release pressure there would have been a small eruption of water in the mudboil. The water coming out would contain sediments and drains towards the

Before all the news about the impossible real estate market, Silicon Valley and the drought, California was known for something a little sweeter: wine. With the drought bringing less water to fields, vintners are thrilled to say that wine grape quality has never been better. In fact, the 2014 wine grape harvest produced one of the best vintages this decade, according to the Wine Institute.

The supply of grapes, apples, bulk wine and grape juice concentrate for Vincor’s wine products comes from a combination of sources. Privately owned vineyards (Canada, U.S., Australia) provide somewhere between 35% to 57% of the raw products needed to

Wine industry is defined as a sector of the food industry producing grape wines, champagne, cognac, and fruit-berry wines. Competitors of E&J Gallo Winery include Constellation, Jackson Family Wines, and Treasures Wine Estate. Their biggest competitor is Constellation, the parent company of Canandaigua, a New-York based winery and producer of Richard’s Wild Irish Rose; they have produced 4.6 billion in 2007 sales including beer and spirits. Alternative products for wine are other alcoholic beverages including vodka, tequila and gin. Wine is not just targeted to one class or group of individuals, they target to anyone over 21 years of age whether that is the low-income, middle-class, or high-class. In recent

Napa County is best known for its world renown wineries. The wine industry is the central economic driver in Napa and Sonoma counties. It boasts itself as the world’s fourth largest wine producer. Napa and Sonoma County’s farming industry employs thousands of farm laborers, sales reps, and sommeliers. Additionally, the wine industry thrives on tourism and exportation of goods. This requires thousands of support industries such as shipping companies, hospitals, and hotels. “In 2015, the wine business employed about 325,000 people statewide and generated more than $57 billion in economic activity, including $7.2 billion in tourist-related income” (Hodgins, 2017 p.1).

As the river flows, it cuts rocks which it carries them down its course and grinds them as it moves farther to forms sediments. When the river enters a relatively flat ground, it slows down resulting in sedimentation. This process is common in the plains where the river spreads over a wider area to form a U-shaped valley. Due to the