From KILKISBI@wattsind.com Mon Apr 7 16:04:48 2003 From: KILKISBI@wattsind.com (Kilkis, Birol I.) Date: Mon, 7 Apr 2003 11:04:48 -0400 Subject: [LON-CAPA-cvs] MIME coded data Message-ID: <750A7AC5DCCAD4119FF800306E00646302E970EE@and998nts.wattsind.com> This message is in MIME format. Since your mail reader does not understand this format, some or all of this message may not be legible. ------_=_NextPart_001_01C2FD17.080CD8D0 Content-Type: text/plain; charset="iso-8859-1" Dear Matthew,Is there a way to get the following data without MIME encoding? is a MIME encoded message --matthew1026420578 Content-Type: text/plain matthew Thu Jul 11 16:49:38 2002 EDT Added files: /loncom/thesaurus rawkey.txt Log: BIG list of metadata keywords. --matthew1026420578 Content-Type: text/plain Content-Disposition: attachment; filename="matthew-20020711164938.txt" Index: loncom/thesaurus/rawkey.txt +++ loncom/thesaurus/rawkey.txt board,diver,diving,torque Sincerely yours, Prof. Dr. Birol I.. Kilkis ------_=_NextPart_001_01C2FD17.080CD8D0 Content-Type: text/html; charset="iso-8859-1" Content-Transfer-Encoding: quoted-printable MIME coded data

Dear Matthew,Is there a way to get the = following data without MIME encoding?

is a MIME encoded message = --matthew1026420578 Content-Type: text/plain matthew Thu Jul 11 = 16:49:38 2002 EDT Added files: /loncom/thesaurus rawkey.txt Log: BIG = list of metadata keywords. --matthew1026420578 Content-Type: text/plain = Content-Disposition: attachment; = filename=3D"matthew-20020711164938.txt" Index: = loncom/thesaurus/rawkey.txt +++ loncom/thesaurus/rawkey.txt = board,diver,diving,torque

Sincerely yours,

Prof. Dr. Birol I.. Kilkis

------_=_NextPart_001_01C2FD17.080CD8D0-- From lon-capa-cvs@mail.lon-capa.org Mon Apr 7 18:37:09 2003 From: lon-capa-cvs@mail.lon-capa.org (www) Date: Mon, 07 Apr 2003 17:37:09 -0000 Subject: [LON-CAPA-cvs] cvs: modules /gerd/blackboard 0004.jpg 0005.gif 0006.gif 0007.jpg 0008.gif 0009.gif 0010.gif 0011.gif 0013.gif 0014.md 0015.pool 0017.md 0018.course Blackboard.md Comments IMS.md export_Translationpool for /gerd/blackboard/META-INF MANIFEST.IMS Message-ID: This is a MIME encoded message --www1049737029 Content-Type: text/plain www Mon Apr 7 13:37:09 2003 EDT Added files: /modules/gerd/blackboard 0004.jpg 0005.gif 0006.gif 0007.jpg 0008.gif 0009.gif 0010.gif 0011.gif 0013.gif 0014.md 0015.pool 0017.md 0018.course Blackboard.md export_Translationpool IMS.md /modules/gerd/blackboard/META-INF MANIFEST.IMS Modified files: /modules/gerd/blackboard Comments for Log: BlackBoard Sample Course Export Data --www1049737029 Content-Type: text/plain Content-Disposition: attachment; filename="www-20030407133709.txt" Index: modules/gerd/blackboard/0014.md +++ modules/gerd/blackboard/0014.md Translation pool A pool containing questions of all types for use in exploring translation of Courseinfo pools to other systems Index: modules/gerd/blackboard/0015.pool +++ modules/gerd/blackboard/0015.pool Translation pool A pool containing questions of all types for use in exploring translation of Courseinfo pools to other systems Describe the most recent glacial episode in the last Great Ice Age, and explain briefly how it affected the American midwest. The most recent glacial in the last Great Ice Age reached its peak about 20,000 years ago. The Laurentide ice sheet covered much of Canada and the American midwest as far south as Illinois and Ohio. The Cordilleran ice sheet in the western US covered western Canada and the northwestern US. In addition in North America there were smaller ice bodies, called ice caps in the Rocky Mountains, and the Sierra Nevada. Elsewhere ice caps existed in the Andes in South America and in the Himalayas in Asia. Sea level was about 150 meters lower than today and broad expanses of the continental; shelves were exposed along the eastern continental margin of the US. Pollen data indicate that spruce trees, which prefer cooler climates grew in what is now Alabama and Georgia during the last glacial maximum, and migrated northwards to Canada during the present interglacial. The most recent glacial ended about 14,000 years ago when our present interglacial began. Although the period 14,000 years to the present has been a period of general warming there have been occasional reversals to colder conditions. The younger Dryas cold period that occurred about 10,000 years ago is thought to have been the result of a temporary change in ocean circulation caused by the large volumes of fresh water arriving in the North Atlantic from melting of the retreating Laurentide ice sheet. Even more recently, the Little Ice age was a period of colder temperatures in northern Europe between the 15th and 19th centuries, split into two segments by a warm period in the 17th century. The Laurentide ice sheet covered Michigan during the last glacial maximum. The present surface coverage of drift which blankets the lower peninsular owes its origins to the last glacial period. Retreat of the ice left behind a number of depositional landforms. There are abundant kettle lakes, eskers and moraines. Terminal moraines were formed after the glacial maximum when the ice had retreated from its maximum extent south of Michigan. Retreat was punctuated by minor readvances, and the large number of terminal moraines allow reconstruction of the direction of ice flow in Michigan during this time. The Great Lakes themselves were the product of deepening of pre-existing valleys by glacial action. The lakes only achieved their present configuration relatively recently. Water levels and the locations of shorelines changed considerably during the period following ice retreat. Locations of outflows from the lakes changed as the elevation of the land was modified by a process known as isostatic rebound. Whenever the lithosphere is loaded with a large load, such as a big ice sheet, it is depressed. When the load is removed the lithosphere slowly rebounds to its former position. Depression and rebound are possible because beneath the lithosphere is the weaker asthenosphere which can flow. In the same way that a heavily laden boat sits lower in the water, so ice-covered lithosphere sinks and asthenosphere flows out from underneath it to accommodate the sinking. The asthenosphere flows back underneath it when the load is removed. The effects of the last glacial are still evident from changes in elevation across the northern hemisphere. Areas previously loaded with ice such as the Canadian shield (Ontario, Quebec, Manitoba) and Scandinavia are now rising. Areas to the south (e.g., Holland) which previously were uplifted by the displaced aesthenosphere flowing into them are now sinking as the asthenosphere returns northwards. Michigan is now no longer rising, and neither is it sinking. Areas to the south are sinking somewhat and the Canadian shield is rising somewhat (at a maximum rate of 1 cm/yr.). The number of officially recognised Great Lakes is ... 5 Five five FIVE There are 5 Great Lakes: Lake Superior Lake Ontario Lake Michigan Lake Erie Lake Huron The total number of Great lakes is 5. 5 Five five FIVE Which of the following are considered to be Great Lakes? Lake Michigan Lake Huron Lake Superior Lake Champlain Lake Cuyahoga Lake Baikal There are 5 Great Lakes: Michigan, Huron, Superior, Ontario and Erie Although Lake Champlain and Lake Cuyahoga are in the northeastern US they are not considered "Great Lakes". Lake Baikal is in Siberia. Each of the following states has shoreline on only one of the Great Lakes. Match the state to the lake. Minnesota Illinois Indiana Pennsylvania Ohio Lake Ontario Lake Michigan Lake Superior Lake Erie Lake Huron Lake Superior borders: Minnesota, Wisconsin, Michigan and Ontario Lake Michigan borders: Wisconsin, Illinois, Indiana and Michigan Lake Huron borders: Michigan and Ontario Lake Erie borders: Ohio, Michigan, Pennsylvnia, New York and Ontario Lake Ontario borders: New York, Ontario Your answers will be chosen from: Lake Michigan (Illinois & Indiana); Lake Superior (Minnesota), and Lake Erie (Pennsylvania and Ohio). The deepest of the Great Lakes is ... Lake Michigan Lake Huron Lake Superior Lake Eries Lake Superior is the deepest of the Great Lakes. Maximum depths are as follows: Superior: 406.3 m Michigan: 281.3 m Ontario: 244.45 Huron: 228.6 m Erie: 64 m The deepest of the Great Lakes is: Lake Superior. Average depths are: Superior: 146.3 m Ontario: 86.26 m Michigan: 85.04 m Huron: 59.44 m Erie: 19.9 m List the following states in order from highest to lowest by the number of Great Lakes on which they have shoreline. Wisconsin Indiana Vermont Michigan Michigan has shoreline on 4 lakes (Superior, Michigan, Huron and Erie) Wisconsin has shoreline on 2 Great Lakes (Superior and Michigan) Indiana has shoreline on 1 Great Lake (Michigan) Vermont does not have shoreline on any of the Great Lakes (although it does have shoreline on Lake Champlain). The correct order is: Michigan Wisconsin Indiana Vermont The Great Lakes were formed as a result of deepening of existing depressions due to glacial action during the last ice age. FALSE TRUE Although the Great Lakes did not reach their current configuration and drainage patterns until about 4000 years ago, the depressions now occupied by the lakes were formed by deepening of existing valleys during movement of the Laurentide ice sheet during the last Ice Age which ended about 10,000 years ago. The Great Lakes were indeed formed during the last ice age. There were a number of precursor lakes during the retreat of the Laurentide ice sheet (e.g., Lake Chicago and Lake Algonquin), but the work of deepening existing valleys to create the depressions that noew hold the Great Lakes occurred as a result of movement of the Laurentide ice sheet. Index: modules/gerd/blackboard/0017.md +++ modules/gerd/blackboard/0017.md Testing Blackboard v. 4.11 Testing only Education Online Teaching and Learning Index: modules/gerd/blackboard/0018.course +++ modules/gerd/blackboard/0018.course