2021 Google is a formal valley located in catchement©area of Hovinbekken stream in Oslo, ©
3
0
0
Fulltekst
(2) Part of the farm also became brick factory connected to the Hovinbekken stream.. 250m. valle hovin. The ice industry became very prosperous, therefore 2 more dams were built in the trace of the natural depression.They even connected another stream with these new dams.. When Farmer realised the presence of wetland, where sometimes is water and sometimes not, they cultivated the terrain depression and built the channel in order to create constant water flow and bring more water into the pond, which was started to use for ice harvesting during the winter months.. The first map is from 1792 and shows Sondre Hovind farm, one of 7 parts of Hovin Farm. The farm is located on the hill, surrounded by meander of Hovinbekken stream. Into the main stream was connected the moist area with natural terrain depression, which created a pond.. 1792. 1911. 1937. Together with building new highway in 1980s all original topography was confused. Hovinbekken stream was pipped and 2 streams were separated, now the Hovin valley is feed only by small stream and its own micro catechemnt. From the moist wet area full of dams only on is remain - Hovindammen. Football fields were added agains the natural topography, that is the reason why they are often wet and muddy and grass had to be replaced by artificial grass.. The growing city and new development meant great changes and earth movement for the Hovin Valley. The farm became part of the city.. 1950. 2021. 2030. hovinbekken chatchement area ice harvesting. hovinbekken piping. river opening projects. hovinbyen strategic plan Hovin Valley is neighbouring with the new development of area called Hovinbyen, where is expecting to create 30,000 - 40,000 new homes, with 60,000 - 80,000 new residents, in addition to the 40,000 that live here today.. Bedrock and soil conditions determinate the usage of whole area since the very beginning. On the top, where mountains are located the bedrock is volcanic origin, where the steep topography ends, the undivided piece of rock starts. On the the top is soil from sea and fjord deposits. The piping the stream in 1950s and growing city brot significant change. the place became industrial area. those 2 streams were connected much Northern than the original trace used to be so that Hovin Valley became disconnected from its main water source and now its fuel only with its own micro catchment.. Ground conditions affected also the way how the Hovinbekken stream flowed. The stream collects its water from lakes and marshland from the Nordmarka region of Grefsen and Årvollmarka. It was running from the forest until it met quite flat land and started to meandering. On the soft, fertile land people established first farms.. bedrock Undivided cambosiluric rocks in areas covered by Quaternary deposits and heavily degraded. soil Sea and fjord deposition. Weathering material. Through the time from the his whole catchment area became economical project. On suitable sites ice dams were built because the slow flow of Hovinbekken was perfect for ice harvesting. And channels were built to distribute water between agricultural fields. 500m. page size: 841 x 594 mm. radka komrsová moist, mist and the in-between. scale: see scale bars.
(3) In the large context of Hovinbyen Valle Hovin is going to play crucial role in the community life therefore was important to connect it well with its surroundings. Due to disturbance of natural terrain, flowing towards the fjord by highway the connection with norther part of neighborhood is limited, nevertheless it is possible to connect the valley by a cycle path in the route of a piped stream. The main connection with the surroundings takes place vertically, where the valley forms a connection between the two housing estates and at the same time provides a sufficient path network between the sports fields, the arena and the sports halls. The plan also shows the catchment area of the proposed design, located in future development area as a condition which is needed to be taken consideration in planing. Further downstream, the plan envisages the opening of a stream and connection to the ongoing construction of a residential housing estate with an open stream.. t. legend Green areas. Piped stream Long distance connection / Cyclo paths. Water shead of Valle Hovin Well connected areas. page size: 841 x 594 mm. radka komrsová moist, mist and the in-between. Walkable connection New development. scale 1:5000.
(4)
RELATERTE DOKUMENTER
The combined effect of these measures may well be a decline in jihadi activity in the short run, i.e., in the next two to five years. There are already signs that this is
The Norwegian Defence Research Establishment (FFI) has for decades been doing hydrographical surveillance in prioritized areas. In connection with this work, FFI has also
1) Analysis of the Mid-Sound Stations: Table 4.1 gives the computed PSD of time series C1, E1 and H1 at three different frequencies. The PSD of the z-component at 0.001 Hz is
The novel figure-of-8 cable cerclage enhanced fixation stability and reduced re- displacement of the posteromedial-buttress in cephalomedullary nailing of subtrochanteric
The main overlap area between cod and capelin coincided with the main distribution area of capelin in all years (Fig 8A, S3 Appendix). The mean overlap was higher between mature cod
Although, particularly early in the 1920s, the cleanliness of the Cana- dian milk supply was uneven, public health professionals, the dairy indus- try, and the Federal Department
From May to July 2004, photographer Camilla Damgård was engaged in pictorially documenting smoking behaviour both before and after the new law came into effect on June 1, 2004..
The scene containing media is referenced in the main BIFS scene (the layout scene) as a stream of type SceneDescription stream and encapsulated in a new Object Descriptor (for
