SIERRA NEVADA TRANSFERS
We provide high-quality private transfers from Faro airport to Sierra Nevada at the best price on the market, up to 3 passengers 757€ and up to 8 passengers 871€ (Final Price Per Vehicle). All of our transfers are private and with fixed prices. (All taxes included and motorway tolls). We provide baby seats and child seats at no extra cost (if requested on booking).
ALGARVE GOLF TRANSFERS
Portugal is known as the best golf destination in Europe. We provide private transfers between your accommodation and all golf courses in Algarve.
Whatever your group size, we will have a vehicle for you – from private transfers for individuals or small groups to coaches transfers for large groups. If you need to request quotation Click Here
FARO AIRPORT TRANSFERS
Transfers from Faro Airport to Sierra Nevada You will be received by a professional driver with years of experience on private transfers and dedicated to providing the best service based on his experience and knowledge of the Algarve. He will be waiting for you at the arrivals hall with a sign with your name on it, and he will take you directly to your destination.
The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies primarily in Nevada. The Sierra Nevada is part of the American Cordillera, an almost continuous chain of mountain ranges that forms the western "backbone" of the Americas.
The Sierra runs 400 miles (640 km) north-south and is approximately 70 miles (110 km) across east-west. Notable Sierra features include General Sherman, the largest tree in the world by volume; Lake Tahoe, the largest alpine lake in North America; Mount Whitney at 14,505 ft (4,421 m), the highest point in the contiguous United States; and Yosemite Valley sculpted by glaciers from one-hundred-million-year-old granite, containing high waterfalls. The Sierra is home to three national parks, twenty wilderness areas, and two national monuments. These areas include Yosemite, Sequoia, and Kings Canyon National Parks; and Devils Postpile National Monument.
More than one hundred million years ago during the Nevadan orogeny, granite formed deep underground. The range started to uplift four million years ago, and erosion by glaciers exposed the granite and formed the light-colored mountains and cliffs that make up the range. The uplift caused a wide range of elevations and climates in the Sierra Nevada, which are reflected by the presence of five life zones (areas with similar plant and animal communities). Uplift continues due to faulting caused by tectonic forces, creating spectacular fault block escarpments along the eastern edge of the southern Sierra.