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Some one-eighth of Saskatchewan’s surface area is covered by water, including Lake Wollaston and large portions of Lake Athabasca and Reindeer Lake. Water flowing through the province’s rivers drains variously to the Atlantic and Arctic oceans and to the Gulf of Mexico. Most of Saskatchewan’s waters flow from west to east, its great rivers (which provided the first transportation routes) rising in the Rocky Mountains and emptying ultimately into Hudson Bay. The northwestern portion of the Precambrian Shield, however, drains into Lake Athabasca and then to the Beaufort Sea via the Mackenzie River. The extreme southwestern portion of Saskatchewan, including the Frenchman River, is part of the Missouri River drainage basin that empties into the Gulf of Mexico.

Saskatchewan’s soils can be broadly divided between the forest soils of northern regions and the grassland (prairie) soils of the south. The former tend to be thin and acidic, light in colour, and infertile. Poorly drained peat and mineral soils are also common in northern Saskatchewan. Grassland soils vary in colour from very dark (almost black) in the more humid central zones to dark brown over much of the southern prairie and lighter brown in the drier southwest regions. Climate is a major determinant of soil type. The black and dark brown soils are the most fertile and support the majority of agricultural production.

After you install this hotfix, Group Policy is applied synchronously during the next logon if a drive that is marked "no reconnect" is mapped. Therefore, it may take longer than expected to log on to the client computer.For more information about Group Policy, visit the following Microsoft TechNet website:

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The global version of this hotfix installs files that have the attributes that are listed in the following tables. The dates and the times for these files are listed in Coordinated Universal Time (UTC). The dates and the times for these files on your local computer are displayed in your local time together with your current daylight saving time (DST) bias. Additionally, the dates and the times may change when you perform certain operations on the files.

This issue occurs because of an error in GPP that causes it to ignore the non-persistent flag during the drive-mapping process.

Continental glaciation greatly influenced Saskatchewan’s landscape, scouring and molding the northern shield to produce a landscape of rocky outcrops, lakes, and rivers. Glacial deposits on the shield tend to be thin and discontinuous. The southern plains are covered with a veneer of sediments laid down by ice sheets and their subsequent meltwaters. The most important agricultural regions occur in areas of finer-grained sediment, while rolling hills of hummocky moraine and other coarser-grained sediments are primarily used for ranching. Cut into the plains are many spectacular river valleys, including those of the North and South Saskatchewan rivers and the Qu’Appelle River. Many of these river valleys were carved by meltwaters during the retreat of the ice sheets.

A supported hotfix is available from Microsoft. However, this hotfix is intended to correct only the problem that is described in this article. Apply this hotfix only to systems that are experiencing the problem described in this article. This hotfix might receive additional testing. Therefore, if you are not severely affected by this problem, we recommend that you wait for the next software update that contains this hotfix.If the hotfix is available for download, there is a "Hotfix download available" section at the top of this Knowledge Base article. If this section does not appear, contact Microsoft Customer Service and Support to obtain the hotfix. Note If additional issues occur or if any troubleshooting is required, you might have to create a separate service request. The usual support costs will apply to additional support questions and issues that do not qualify for this specific hotfix. For a complete list of Microsoft Customer Service and Support telephone numbers or to create a separate service request, visit the following Microsoft Web site:

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http://support.microsoft.com/contactus/?ws=supportNote The "Hotfix download available" form displays the languages for which the hotfix is available. If you do not see your language, it is because a hotfix is not available for that language.

Saskatchewan, province of Canada, one of the Prairie Provinces. It is one of only two Canadian provinces without a saltwater coast, and it is the only province whose boundaries are all wholly artificial (i.e., not formed by natural features). It lies between the 49th and 60th parallels of latitude, it is bounded on the west by longitude 110° west of Greenwich, and its eastern limit, with minor adjustments, is longitude 102° W. Its southern half is largely an extension of the Great Plains of central North America, rarely rising 2,000 feet (610 metres) above sea level. It measures 760 miles (1,223 km) from south to north, tapering from a width of 393 miles (632 km), where it abuts Montana and North Dakota in the United States, to 277 miles (446 km), where it meets the Northwest Territories. Saskatchewan is Canada’s fifth largest province in area and sixth in population. Saskatchewan’s landscape makes its inhabitants conscious of the sky, and the changing patterns of light and shadow on clouds, which commonly offer magnificent sunrises and sunsets, are as much a part of the scenery as any contour of the earth. Economically, the province has always been heavily dependent on the exportation of its agricultural and mineral products and is thus peculiarly sensitive to fluctuations in world markets beyond its own or even Canada’s control. Area 251,367 square miles (651,036 square km). Pop. (2021) 1,132,505; (2023 est.) 1,218,976.

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For more information about how to obtain a Windows 7 or Windows Server 2008 R2 service pack, click the following article number to view the article in the Microsoft Knowledge Base:

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Assume that you use Group Policy Preferences (GPP) to manage the mapping of drives in a network environment. Additionally, you set the non-persistent flag when you map a drive on a client computer that is running Windows 7 or Windows Server 2008 R2. However, when the client computer is not connected to the network, the mapped drive is displayed unexpectedly as a disconnected drive in Windows Explorer. Note This issue does not occur if you use the following command to configure the non-persistent flag or the persistent flag:

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The files that apply to a specific product, milestone (RTM, SPn), and service branch (LDR, GDR) can be identified by examining the file version numbers as shown in the following table:

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General information about Group PolicyFor more information about software update terminology, click the following article number to view the article in the Microsoft Knowledge Base:

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The MANIFEST files (.manifest) and the MUM files (.mum) that are installed for each environment are listed separately in the "Additional file information for Windows Server 2008 R2 and for Windows 7" section. MUM and MANIFEST files, and the associated security catalog (.cat) files, are extremely important to maintain the state of the updated components. The security catalog files, for which the attributes are not listed, are signed with a Microsoft digital signature.

Climate is a major limiting factor for agriculture, restricting it to the area south of 55° N latitude. Even within this zone, there are as few as 80 to 100 frost-free days annually. Temperature variations are extreme; January temperatures have fallen below the mid −60s F (about −53 °C) in settled parts, and in July temperatures of more than 100 °F (about 41 °C) have been recorded. The normal mean daily reading for the arable regions ranges from −5 to 10 °F (about −21 to −12 °C) in January and from the mid-50s to the mid-60s F (about 13 to 18 °C) in July. In other words, Saskatchewan has a variable climate with cold winters and warm to hot summers. Because the province lies in the continental interior, precipitation is low, averaging from about 10 to 20 inches (about 250 to 510 mm) each year. Most winter precipitation falls as snow, which ranges from about 30 inches (about 750 mm) in the southwest to more than 60 inches (about 1,500 mm) in the north-central area. Drought years are not uncommon.

The most important division of the land in Saskatchewan is between the northern one-third of the province, which is part of the Canadian Shield, and the plains, which cover the southern two-thirds. The Canadian Shield is an area of mostly igneous and metamorphic rocks of Precambrian age (about 540 million to 4 billion years old); hence, it is often referred to as the Precambrian Shield. The plains comprise a wedge-shaped succession of sedimentary rocks, the oldest of which abut the shield margin while the youngest occur in the Cypress Hills in the southwestern portion of the province. The highest elevations in Saskatchewan are also found in the Cypress Hills, peaking at 4,567 feet (1,392 metres) above sea level. These hills—the only part of Saskatchewan that escaped glaciation—contain unique plant and animal life. The lowest point in the province, 699 feet (213 metres), is in the extreme northwest.