How to overcome Jetlag

Written by Sarah Moore


Continued from page 1

While traveling, drink plenty of water. Stay away from alcohol, fizzy drinks and coffee. These drinks only exacerbate jetlag causing dehydration, tiredness and headaches. Drink plenty of water. Chamomile tea is very calming. Eat Lightly. The last thing your body needs it to digest a large meal. Exercise - “Economy Class Syndrome” is caused from inactivity or sitting inrepparttar same position for an extended time. Whenrepparttar 142702 time permits, get up and walk aroundrepparttar 142703 aircraft.

Specific exercises and stretching techniques can be accessed through:

http://www.airnz.co.nz/resources/inflight_exercises.pdf

Try and get some sleep. Sleeping onboard will not only help to passrepparttar 142704 time, but can help you feel refreshed upon arrival. A travel neck pillow will assist in your sleeping, providing excellent head support. Avoid sleeping pills at all costs.

When you arrive, getting a quick nap will seem very attractive indeed – but resist this temptation. Go to bed at your normal bedtime (based on local time). This will force your body to adjust to any new time zones far quicker.

Article by Travel J - Traveler's Resources & Information - http://www.travelj.com

Sarah Moore has been in the travel and tourism industry for over 20 years and is currently working with one of the worlds largest coach networks. Sarah is also the webmaster of TravelJ - A Traveler's Resources & Information Network - http://www.travelj.com


Yosemite National Park

Written by Gregg Strand


Continued from page 1

The geology of Yosemite is characterized by granitic rocks and remnants of older rock. About 10 million years ago,repparttar Sierra Nevada was uplifted and then tilted to form its relatively gentle western slopes andrepparttar 142627 more dramatic eastern slopes. The uplift increasedrepparttar 142628 steepness of stream and river beds, resulting in formation of deep, narrow canyons. About 1 million years ago, snow and ice accumulated, forming glaciers atrepparttar 142629 higher alpine meadows that moved downrepparttar 142630 river valleys. Ice thickness in Yosemite Valley may have reached 4,000 feet duringrepparttar 142631 early glacial episode. The downslope movement ofrepparttar 142632 ice masses cut and sculptedrepparttar 142633 U-shaped valley that attracts so many visitors to its scenic vistas today.

(This information was obtained fromrepparttar 142634 National Park Service and is inrepparttar 142635 public domain.)

Find last-minute national parks discount hotel and lodging availability. Save time by searching several locations at once. Also, access to cheap airline tickets and car rental information. http://www.national-parks-hotels-lodging.com


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