Over packing is a very big problem to a lot of travelers. This is so because it poses a lot of additional burdens and problems to the individual. With these problems, he or she won't exactly be able to entirely enjoy the entire trip that aims to enjoy the exploration of the sights, tastes and cultures of several places. Thus, the foremost question before really traveling, “How to pack when traveling?”
When considering how to pack when traveling one is bound to also consider what to pack when traveling. The most important mindset where one starts when packing is traveling light. The major benefits for bringing as little as possible are multi-faceted. For one, one will feel more secure with the little that he or she has to look out for. In matters of finances, the lighter you pack, the less you are to spend on a lot of things connected to baggage cost. Also, one will be able to move more freely with the little that one brings. With all of the aforementioned things in place, one need not worry too much about the baggage anymore.
How to pack when traveling should consider security. When one brings easily identifiable baggage with its contents because it isn't too much, then there will be a decrease in the incidents of theft, loss and damage.
A second consideration should be economy. This is so because one greatly reduces all sorts of costs when one travels lightly. For one, you will not be charged anymore for those who will be carrying your bags around. Furthermore additional freight charges are also avoided. When transportation is considered, one doesn't have to take the more expensive kinds contrasted to the public utility vehicles. With all of that, one generally saves a lot.
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It is not always about money – you may have sufficient funds to afford either but one of them would suit you more. And it is not always about your general style or preferences as ‘travel style’ is totally different. Many positive people may turn to be ‘unbearable’ fellows while traveling only because they have chosen the wrong style.
You can go for group tours if you agree with some or most of the statements below:
- You are single and do not have a travel buddy: Join group tours for more fun, less cost and of course to make new friends.
- You are not alone but still enjoy knowing people from all over the world; where else will you have this chance?
- You are female(s) traveling to less developed countries – stick to group tours if possible. Groups can offer more safety and comfort.
- You seek for maximum efficiency: Group tours have pre-scheduled itineraries to maximize your sightseeing. No matter how long your wife/husband would prefer to stay at a shop or your photo addict friend would like to take extra shots; the tour has to end when the guide blows the whistle.
- Although money is not everything, it is something: In some countries such as Turkey, Greece or Morocco private tours cost almost double or even triple prices when compared to the group tours. For small families or friend groups (2-3 traveler) it’ll be more cost effective to join escorted group tours.
If you are not sure about your travel style yet, here are the reasons why people prefer private tours despite the higher costs:
- You want to have full control on where to go, how to go, when to relax, when to shop etc. No matter how much more it cots, take a private tour.
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The truth is that no one knows for sure though there are some pretty good guesses. The chances are that a number of processes combined to create the views that you see in todays Grand Canyon. The most powerful force to have an impact on the Grand Canyon is erosion, primarily by water (and ice) and second by wind. Other forces that contributed to the Canyon's formation are the course of the Colorado River itself, vulcanism, continental drift and slight variations in the earths orbit which in turn causes variations in seasons and climate.
Water seems to have had the most impact basically because our planet has lots of it and it is always on the move. Many people cannot understand how water can have such a profound impact considering that the Canyon is basically located in a desert. This is one of the biggest reasons that water has such a big impact here. Because the soil in the Grand Canyon is baked by the sun it tends to become very hard and cannot absorb water when the rains to come. When it does rain the water tends to come down in torrents which only adds to the problem. The plants that grow in the Grand Canyon tend to have very shallow root systems so that they can grab as much water as possible on those rare occasions when it does rain. Unfortunately these root systems do nothing to deter erosion by holding the soil in place. Now you've got lots of water, no place for it to go, but down to the Colorado River, and nothing holding the soil and rock in place. The result is frequently a flash flood roaring down a side canyon that can move boulders the size of automobiles, buses and even small houses. If automobiles, buses and small houses are in the way then it will take them too. Luckily no one builds houses in the Grand Canyon so that's not a problem but there are a few autos, vans and buses sitting at the bottom of the Colorado. This mass that moves down a side canyon during a flash flood is more like a fast flowing concrete than water and it can be very dangerous. You should always be well informed of weather conditions when you are hiking through side canyons in the Grand Canyon.
After erosion by liquid water the next most powerful force is probably its solid form, ice. In the colder months, especially on the north rim, water seeps into cracks between the rocks. These cracks can be caused by seismic activity, or by the constant soaking and drying of the rocks. When the water freezes it expands and pushes the rocks apart and widens the cracks. Eventually rocks near the rim are pushed off the edge and fall into the side canyons. These rocks sometimes hit other rocks and are stopped but on occasion one fall by a large rock will cause a cascading effect and create a rock fall that will alter the landscape drastically in the side canyon. Debris from rock falls piles up at the bottom of the side canyons and is then carried down to the Colorado River the next time there is a flash flood. Rock falls frequently take out sections of trail in the Grand Canyon requiring the Park Service to close these trails until they can be repaired.
Once the ice had pushed the rocks off the edge and the water in the flash floods has carried them down to the river, then the Colorado itself takes over. The erosive action of the Colorado has been severely constrained by the building of the Glen Canyon Dam, which ended the annual spring floods, but there is still a lot of water flowing relatively quickly through a very narrow gorge. Before building the dam the Colorado River had spring floods that would exceed a flow rate of 100,000 CFS. All of that snow melting in the Colorado Rockies came pouring down through the Grand Canyon in May and June, every year, like clock-work. These spring floods were considerably larger than todays "trickle" of 8,000-10,000 CFS at low water and even the 20,000 CFS peak flow rates.
The Colorado's spring floods used to carry away all of the debris that
was deposited in the main channel by the flash floods, but todays
mediocre flow rates have a tough time doing the job. It still gets done
to some extent, it just takes a lot longer. In the process of moving
the rocks and sediment down the river to the Pacific Ocean the bed of
the river is scoured by all of this fast moving debris which slowly
eats away at the banks and bed of the river. This causes the river to
widen and cut down deeper into the lower rock layers. Another cause for
the slowing of the erosive force of the Colorado River
is the fact that it is now trying to cut through harder granites and
schists found at the bottom of the Canyon instead of the softer
limestones, sandstones and shales near the top. This rock takes a lot
longer to erode and a slower moving river means it takes even longer.
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Very retro stainless steel toothpick dispenser. Authentic 50's diner design.
Route 66 Place
Introduction:
The
History of Modern Northern Arizona and Route 66 are inseparable. Route 66 is
but one of several modern and historic transportation route that cross Northern
Arizona. Historically, explorers like Beale traveled the 35th parallel route, and in more modern times
Route 66 shared the route with Southern Union Gas, and the Burlington Northern
Santa Fe Railroad. The communities of the northland have been affected by these
influences but much of their growth and prosperity has been shaped by their
relationship with Route 66 and the various forms it has taken across time.
Early Roads:
Route 66 was created out of earlier, locally developed roads. In this regard then, Route 66 has roots in an earlier period of transportation. Initially, there was not a tremendous need for highways in the West after the initial wave of railroad building. The railroads performed an effective job of transporting goods and passengers across Northern Arizona. The communities served by the railroad (initially the Atlantic and Pacific, later the Santa Fe) were all small, and easily navigated on foot, or by horse. It really was not until the advent of the bicycle and later, the automobile, that there was a nationwide call for serviceable streets and highways. Road building also sprang from the Progressive Era as a way of linking the rapidly changing urban landscape with the isolated rural regions of the U.S.
As such, there were local roads which followed earlier established trails connecting one town to the next across Northern Arizona. These roads were the first roads established as official, receiving whatever care the State Engineer's Office could spare. Road building and maintenance was modeled after the railroad example with dedicated crews and equipment for specific sections of highways. For the most part, these crews did their best to keep roads smooth by grading them with drags, and providing minimal filling and cutting to reduce only the worst grades and dips.
Establishment and Building of Route 66:
Early federal highway building was based upon a number of programs which led to the creation of true inter-state highways. First, the government threw its weight behind establishing and improving so-called Postal roads, that is, roads upon which mail was to be carried. It also provided funding for states to establish roads they felt were important. These had mixed results. One initial problem was that because local highway engineers were not thinking in terms of a national system, and thus many strange little roads which benefited few were created. On the positive side, rural and urban America became linked through the Post roads initiative, decreasing the distance between the two populations. The big change came when highway builders did consider the results of linking local roads to create national highways, rather than simply building roads to connect local towns. The funds for these programs were small given the task at hand. Early roads had to be as short as possible, yet avoid fills or cuts, and bridges and tunnels as much as possible. These constraints helped to make the roads one with the environment, rather than today's highways which tend to dominate the environments through which they pass. Given these issues, Route 66 was laid out as a Northeast-Southwest highway which primarily overlaid existing roads. In Northern Arizona then, Route 66 overlay the Holbrook-Winslow highway, the Winslow-Flagstaff highway, the Flagstaff-Williams highway, and so on. There were some notable stories therein. The road from Williams to Ash Fork was a constant source of problems for road builders because of the combination of grade, water, soil and weather. Likewise the realignment of the railroad in Western Arizona caused 66 to change course a number of times.
Road building in the Northland presented a fairly overwhelming challenge given the variety of geology and terrain through which Route 66 passed. The road could not be called a "12 month" road until paving was completed in 1937.
Evolution of Route 66:
Route 66 evolved over the years in such a way that we can clearly see 4 distinct versions of the road. The first is the road as it was established in 1926. This road was simply the official designation of 66 over the existing roads of the day. With only tiny exceptions, this road was unpaved. Almost immediately following, we see the beginning of the "improvement" phase where the road was widened to federal and state specifications, and some changes were made to alter the course of 66 away from steep grades, or deep canyons. This period was followed by the paving of 66. Inclusive with paving came another round of realignment. Locally we can see examples of such realignment at Padre Canyon, Parks, the Ash Fork grade, and in other select spots across Northern Arizona. Paving was completed by late 1937. Another array of local realignment occurred after World War II. where the concrete road appeared. local examples include the Walnut Canyon-Flagstaff alignment in 1947, and the Yucca cut-off west of Kingman which bypassed Oatman in 1952. Parks and Bellmont display all three versions. Finally is the establishment of I-40. In much of Eastern Arizona, I-40 overlays 66 almost completely with a few exceptions between Holbrook and Winslow and between Winslow and Flagstaff. On the West side the new alignment I-40 cut, laid the foundation for preserving one of the longest stretches of 66, from just West of Ash Fork, to the Colorado River.
Effects of Route 66 on Northland Cities and Towns:
Generally, Northland towns were following
the lead set by other Rocky Mountain communities across the West where tourists
became a viable part of each localities economy, and each town worked on ways
to best exploit that resource. To that end, we can see an Eastward growth for
each town to grab tourists and motorists as they hit town with one sort of
business or opportunity. The main streets of Northern Arizona's towns were
lined with tourist/traveller-oriented enterprises; restaurants, drive-ins,
curio shops, gas stations, and motels all formed the commercial sections of the
town's main drag. The most extreme example of this community building along
Route 66 might be Gallup, New Mexico, which has a main street nearly 14
miles long, yet most of the town is less than several blocks deep.
Route 66 traveling near the railroad tracks of the Santa Fe,
often helped reinforce the separations established by the railroad so that the
areas of town on the north side of the highway were often quite different from
those on the south side.
Current Route 66:
The last piece
of active Route 66 at Williams, Arizona was decommissioned in 1986. This event
heralded a period of reflection regarding the role of Route 66 on local and
national history. Across the states through which Route 66 ran, historical
associations sprang up to grapple with the issues surrounding preservation of
something as unwieldy as a highway, and its attendant architecture. There was a
rush of book publishing. Some works were combinations of "coffee table"
and popular culture works like Michael Wallis' Route 66: The Mother Road,
some were personal as in the case of Tom Teague's Searching for 66, or
Quinta Scott's Route 66: The Highway and Its People. Many more simply
attempted to capture the "scrap-book" flavor of travel of the earlier
part of this century. Many of these publications hinted at the importance of
Route 66 (and the potential future for Route 66 studies), but all for the most
part failed to identify just what it is about Route 66 that make such study
worthwhile, and there was little agreement about what time period or version of
the road's past was to be the appropriate subject of such study or
preservation.
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The Beginning Although
entrepreneurs Cyrus Avery of Tulsa, Oklahoma, and John Woodruff of
Springfield, Missouri deserve most of the credit for promoting the idea
of an interregional link between Chicago and Los Angeles, their
lobbying efforts were not realized until their dreams merged with the
national program of highway and road development. While
legislation for public highways first appeared in 1916, with revisions
in 1921, it was not until Congress enacted an even more comprehensive
version of the act in 1925 that the government executed its plan for
national highway construction. Officially,
the numerical designation 66 was assigned to the Chicago-to-Los Angeles
route in the summer of 1926. With that designation came its
acknowledgment as one of the nation's principal east-west arteries. From
the outset, public road planners intended U.S. 66 to connect the main
streets of rural and urban communities along its course for the most
practical of reasons: most small towns had no prior access to a major
national thoroughfare. The Formative Years Route
66 was a highway spawned by the demands of a rapidly changing America.
Contrasted with the Lincoln, the Dixie, and other highways of its day,
route 66 did not follow a traditionally linear course. Its diagonal
course linked hundreds of predominantly rural communities in Illinois,
Missouri, and Kansas to Chicago; thus enabling farmers to transport
grain and produce for redistribution. The diagonal configuration of
Route 66 was particularly significant to the trucking industry, which
by 1930 had come to rival the railroad for preeminence in the American
shipping industry. The abbreviated route between Chicago and the
Pacific coast traversed essentially flat prairie lands and enjoyed a
more temperate climate than northern highways, which made it especially
appealing to truckers. I
n his famous social commentary, The Grapes of Wrath, John Steinbeck
proclaimed U. S. Highway 66 the "Mother Road." Steinbeck's classic 1939
novel, combined with the 1940 film recreation of the epic odyssey,
served to immortalize Route 66 in the American consciousness. An
estimated 210,000 people migrated to California to escape the despair
of the Dust Bowl. Certainly in the minds of those who endured that
particularly painful experience, and in the view of generations of
children to whom they recounted their story, Route 66 symbolized the
"road to opportunity." From
1933 to 1938 thousands of unemployed male youths from virtually every
state were put to work as laborers on road gangs to pave the final
stretches of the road. As a result of this monumental effort, the
Chicago-to-Los Angeles highway was reported as "continuously paved" in
1938. Completion
of this all-weather capability on the eve of World War II was
particularly significant to the nation's war effort. The experience of
a young Army captain, Dwight D. Eisenhower, who found his command
bogged down in spring mud near Ft. Riley, Kansas, while on a
coast-to-coast maneuver, left an indelible impression. The War
Department needed improved highways for rapid mobilization during
wartime and to promote national defense during peacetime. At the outset
of American involvement in World War II, the War Department singled out
the West as ideal for military training bases in part because of its
geographic isolation and especially because it offered consistently dry
weather for air and field maneuvers. Route
66 helped to facilitate the single greatest wartime manpower
mobilization in the history of the nation. Between 1941 and 1945 the
government invested approximately $70 billion in capital projects
throughout California, a large portion of which were in the Los
Angeles-San Diego area. This enormous capital outlay served to
underwrite entirely new industries that created thousands of civilian
jobs.The Depression Years and the War
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