Jakarta needs Mass Rapid Transit (MRT)with regard to comfort. The research method made by the author in measuring the level of comfort of pedestrian in a city environment is the reduction of private vehicles to improve the quality of urban life, the Transit Oriented Development (TOD) concept that makes the city friendly for pedestrian, motorized vehicles and pedestrian must be at different road levels to increase pedestrian convenience, the need to pay attention aspect of safety, security, comfort, convenience, and aesthetic in developing pedestrian facilities and so on which ultimately shows the level of comfort of pedestrian in Senayan district. The result of this study conclude that based on the indicators made by the authors, the existence of MRT in Senayan district is sufficient to provide comfort for pedestrians, although there are still shortcomings that need to be considered to support pedestrian comfort, especially when it rains, therefore the finding of "canopy seating" expected to be taken into consideration for developing pedestrian facilities in the future.
Many different instability phenomena were found on flysch slopes in the past 30 years in the area of dominant geomorphological unit Rječina Valley -Sušačka Draga Valley -Bakar Bay -Vinodol Valley. This paper gives the review of present landslide appearances and the estimation of the possible landslide occurrence at the NW part of Vinodol Bakarac Valley, between the Bakarac and Križišće settlements, in the Kvarner area (north-eastern Croatian Adriatic coast). Based on longtime investigation work results for different purposes it was established that the wings and the base of the valley are made of flysch rock complex, consisting mainly of silty marl, laminated siltstones and fine grained sandstones near the contacts with karstified carbonate rock mass. Landslide susceptibility analysis of this area was made based on existing data about lithological composition and geological fabric, geotechnical properties of slope deposits and flysch bedrock, hydrological and hydrogeological conditions and existing landslides inventory map. Spatial analysis of unfavorable conditions in the investigated location resulted in landslide susceptibility map which divides the area into four classes of susceptibility.
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