For much of the world, the Algarve is synonymous with Portugal, yet the Portuguese will tell you the exact opposite: the region has little in common with the rest of the country. The southern stretch of coast is more reminiscent of a North African landscape than a European one. It has no cosmopolitan cities, like Lisbon and Porto, which are farther north. Most of Portugal is known for quaint towns, medieval castles, and grand palaces. The Algarve is more recognizable for impenetrable blocks of tourist apartments, hotels, and meticulously manicured golf courses. And beaches. Think Algarve and the mind pictures long, glorious stretches of golden sands, secluded coves framed by odd ochre-colored rock formations, and deep green waters. With about 160 km (100 miles) of coastline, Portugal's southern province is one of Europe's premier beach destinations. The occasionally chilly ocean is the Atlantic, but the Algarve has a sultry Mediterranean feel. Its consistent climate is the best in Portugal, and one of the kindest in the world: more than 250 days of sunshine a yearmore than almost any other international resort area. The moderating effect of the Gulf Stream produces a fresh springtime breeze throughout winter, and in late January and February, white almond blossoms blanket the fields. In summer the heat is intense but rarely unbearable, and regardless, beautiful beaches and innumerable pools are always just a dive away. Magnificent year-round weather has made the Algarve a huge destination for sporting vacations. Superb golf facilities aboundseveral with tees dramatically clinging to cliffs and fairways just skirting the edge of the oceanand horseback riding, tennis, big-game fishing, sailing, and windsurfing are immensely popular. Sports, beaches and hospitable weathernot to mention easily organized package vacationsare surely the reasons the Algarve receives as many visitors as the rest of Portugal in its entirety. But it's not just international tourists that descend on the Algarve; many Portuguese from Lisbon and elsewhere in the north have holiday homes and spend their summer vacations here. The coast is neatly divided into the rugged Barlavento to the west and the flat beauty of Sotavento to the east. West is where you'll find the famous orange cliffs and surreal eroded rock stacks.

Question: "Which part of Portugal is not known for quaint cities?"

Response: "Portuguese"

A: no

Michigan will lose $2 million in federal funding and $600,000 in state funding to provide legal aid to the poor in 2003, according to Deierdre L. Weir, executive director of the Legal Aid and Defender Association, Inc., the state's largest provider of legal services to the poor. Current federal funds of nearly $10.7 million from the Legal Services Corporation (LSC) will drop to $8.7 million for next year, according to Weir. She said that the reductions reflect a decline in the number of persons in the state who are living in poverty, according to the U.S. Census Bureau's 2000 census. LSC uses census data to determine funding across the nation, and according to the census, the state's poverty population fell from an estimated 1.2 million in 1990 to an estimated 968,000 in 2000. The state's legal aid agencies are also bracing for yet another cut in 2003 of some $600,000 of state funding. A portion of filing fees paid by litigants in the state's circuit courts, and a portion of interest on lawyers trust accounts (IOLTA) are earmarked for Michigan legal aid programs. These funds are expected to drop from currently $7.5 million in 2002 to $6.9 million when the Michigan State Bar Foundation makes distributions next year. Most of the decrease is attributed to the past year's low interest rates. "The irony of these funding cuts is that while there may be fewer poor people in Michigan today, the demand for service will not change because the poverty population remains so large and the legal aid funding so little that local providers will never able to serve all who need our service," said Weir. "It's as if the poor will be victimized twice-once for being poor and again as victims of these funding cuts." The U.S. Census Bureau, in spite of its best efforts, cannot locate every poor person living in a census tract, therefore the poor are also undercounted, added Weir. The brunt of these cuts will be felt most in Wayne County where according to the census some 333,000 poor people live, the largest concentration of poverty in the state. LAD will lose more than $870,000 for legal aid in Wayne County, nearly half of the state's total loss, said Weir. While difficult to measure, the loss of funds will mean that several thousand of Michigan's poor in need of legal service will not receive it, or they will receive significantly limited service. Cutbacks will include service in such civil legal matters as landlord-tenant, bankruptcy, consumer, child custody, predatory lending, mortgage foreclosure, utility shutoffs, social security, wills, and probate. "Local providers will have to work harder and smarter and use more technology instead of staff to provide as much service as we can with fewer dollars," said Weir. "We will be providing more selfhelp training to clients enabling them to navigate the legal system on their own in routine matters, more assistance on the telephone, and less direct representation by attorneys in specific, high impact matters. Currently, Michigan has 13 legal aid agencies covering the state's 83 counties.

Question: "How did the Michigan's poverty population change in 2003 and how did it affect the federal funding?"

Response: "It decreased and reduced funding"

A: yes

Water flowing over Earths surface or underground causes erosion and deposition. Water flowing over a steeper slope moves faster and causes more erosion. How water transports particles depends on their size. When water slows down, it starts depositing sediment. This process starts with the largest particles first. Runoff erodes the land after a heavy rain. It picks up sediment. Runoff carries most of the sediment to bodies of water. Mountain streams erode narrow, V-shaped valleys and waterfalls. Erosion and deposition by slow-flowing rivers create broad floodplains and meanders. Deposition by streams and rivers may form alluvial fans and deltas. Floodwaters may deposit natural levees. Erosion and deposition by groundwater can form caves and sinkholes. Stalactites and stalagmites are mineral deposits. They build up in caves as water continues to drip.

Question: "What body of water carries the particles?"

Response: "Floodwaters"

A:
no