Sapporo city map pdf

The currencies handled also vary depending on the bank or post office, so it is best to inquire beforehand or check it with the staff at the counter. However, they do not deal in the exchange of coins. At banks, post offices and convenience stores, etc. You can withdraw money from ATMs using foreign-issued cash cards and credit cards. They can also be used on Saturdays, Sundays and national holidays, and though bank and post office ATMs are only available from until or , convenience store ATMs can be used 24 hours a day excluding late-night maintenance periods.

The property is situated 1. Government Office and 2. The property is 2. At the hotel, all rooms include a desk, a flat-screen TV, a private bathroom, bed linen and towels. All guest rooms will provide guests with a microwave. Well set in the Sapporo City Centre district, this hotel is set 2. The hotel features family rooms. At the hotel, every room comes with a desk, a flat-screen TV, a private bathroom, bed linen and towels.

Hotel Sapporo Suites offers certain rooms with city views, and each room comes with a kettle. All units at the accommodation are equipped with a seating area. Randor Residential Hotel Sapporo Suites offers a hot tub. Popular points of interest near the hotel include Former Hokkaid? Hotel Potmum Sapporo Budget-friendly. Set in Sapporo, 1. Among the facilities at this property are a hour front desk and room service, along with free WiFi throughout the property. The hotel will provide guests with air-conditioned rooms offering a desk, a kettle, a fridge, a safety deposit box, a flat-screen TV and a private bathroom with a shower.

Some rooms come with a kitchenette with a microwave. At Hotel Potmum Sapporo all rooms are equipped with bed linen and towels. Guests at the accommodation can enjoy an American breakfast. Sapporo TV Tower is 1. The nearest airport is New Chitose Airport, 44 km from the hotel. Tokyu Stay Sapporo Odori Mid-range. Government Office, located an 8-minute walk from the property. At the hotel, all rooms are equipped with a desk, a flat-screen TV and a private bathroom.

All rooms come with a kettle, while certain rooms are equipped with a kitchenette with a microwave. All guest rooms will provide guests with a fridge. A buffet breakfast is served daily at the property. Staff at reception can lend a hand around the clock with advice on the area. The nearest airport is New Chitose Airport, 40 km from the accommodation. Randor Residence Susukino Suites Budget-friendly.

The accommodation features a hot tub. Each unit comes with a fully equipped kitchen with a microwave, a seating area with a sofa, a flat-screen TV, a washing machine, and a private bathroom with bath and a hairdryer. There is also a fridge, stovetop and a kettle. Guests can refresh in the hot tub and request relaxing massages for an extra cost.

The houses shown in Fig. Most of the residents continued to live at the inclined houses just after the earthquake, but many residents moved without being able to withstand the inclination of houses after around 1 month. The red portion in Fig. Many houses suffered inclination by liquefaction. The inclination of the house shown in Fig. The residents of this house moved soon after the earthquake.

The surrounding ground of the house shown in Fig. The inclined houses shown in Fig. The right house was with the largest inclination in the Utsukushigaoka. The utility pole shown in this photo has settled about 1. Therefore we did a field survey of inclined houses by using a digital angle meter in Utsukushigaoka. Utsukushigaoka, Kiyota ward, Sapporo city was selected as a target area in this research because the inclination of houses caused a serious health problems of the residents and the liquefaction also occurred in the past earthquake.

The field survey was conducted on September 19th and 20th, about 2 weeks after the earthquake. Figure 5 shows inclination of the outer wall of the houses in Utsukushigaoka 1 jo and 3 jo. The inclination is shown in color-coded of every 0.

Vector synthesis was performed in two orthogonal directions and the direction of inclination with larger inclination is indicated by an arrow in this figure. If the maximum inclination and the synthesized inclination are less than 0. The location of largest subsidece of road is also indicated by red cross in this figure. It is found that the houses that were greatly inclined were adjacent and that such houses are inclined in the same direction according to Fig. The houses were also inclined in the direction of the largest subsided road.

The houses in the vicinity of the subsided road, houses A to C are listed in Table 2. These houses with large inclination are located near the park Utsukushigaoka Sumire Park where many sand volcanoes appeared by liquefaction. The houses B and C were greatly inclined in the direction of the subsided road. The inclined houses located along the main street are listed in Table 3. Houses D and E were inclined in the north direction, Houses F and G were inclined to the west direction.

The houses where the inclination were great in Utsukushigaoka 3 jo are listed in Table 4. The inclination of the outer wall of the house J was 2. The second largest inclination house H was inclined 2. Houses H and J were inclined to the southeast direction, and house I was inclined in the southwest direction.

The houses J and I were inclined to the front road. These results revealed that most of the large inclined houses inclined to the same direction. The number of houses in each inclination angle is shown in Fig. Health problems may occurred at the houses with an inclination of 0. Survey of inclination of houses was conducted again 1 month after the earthquake. Inclination of houses increased more than 1.

There were two aftershocks that exceeded JMA seismic intensity 5 between our first and second field survey, and there were houses with large inclinations due to this aftershock. It was difficult for the residents to live there and most of decided to move. Hokkaido has frequently suffered damages induced by liquefaction, such as in the Tokachi-oki, the Kushiro-oki, the Tokachi-oki earthquakes.

The enormous liquefaction damage caused by the Tokachi-oki earthquake in Sapporo city. The liquefaction in the Hokkaido Iburi-tobu earthquake is compared with that in the Tokachi-oki earthquake here. Figure 7 shows areas of ground deformation and inclination of houses in the Tokachi-oki earthquake according to reconnaissance report of the Japanese Geotechnical Society The Japanese Geotechnical Society The surveyed area and the houses with an inclination of 0.

This figure reveals that liquefaction-induced damages in both earthquakes occurred in the vicinity of the former river, and the damage area in the Hokkaido Iburi-tobu earthquake is considered to be more extensive than that in the Tokachi-oki earthquake.

Inclination of houses in the Tokachi-oki earthquake and the Hokkaido Iburi-tobu earthquake The Japanese Geotechnical Society Figure 8 shows an old topographical map of Kiyota ward, Sapporo city in Geographical Survey Institute According to this map, Utsukushigaoka was valley.

Figure 9 is superimposed the past terrain on Fig. According to this figure, the houses built in the former valley were inclined. It can be seen that houses A , B and C with large inclination and largely settled road were located at the former valley. Houses D and E were inclined in the direction of north and houses F and G in the west direction.

These areas were formerly flood or valley plain. Houses H , I and J are also located at the former valley.

It is clear that the direction of inclination of the houses coincides with the direction of former valley or flood plain. The surveyed areas of this study was originally recessed areas that erodes mountains, plateaus and terrace, then the area was reclaimed for residential houses in Houses D to F and G were located at the former flood and valley plains, houses A to C and H to J were located at the former bottom of valley plains.

It was revealed that the inclination damage of houses due to liquefaction is greatly affected by the old topography. The groundwater is very shallow and it is considered that the ground is a high possibility of liquefaction.