Walking Grades and Fitness
Grading is a somewhat difficult topic as much depends on the individuals own perception of his or her abilities. The following is intended as a general guide to our grading system. The levels of difficulty are divided into categories B/C/D. Although the trekking is not at great altitude, it occasionally traverses rough terrain and involves some long days and steep climbs.
Grade B walks (Moderate): are for those of any fitness level who are able to traverse moderately hilly terrain. Walking is limited to day excursions from a central location to which you will be transported. These day hikes are normally no more than 6 hours in duration and all walking may be done with no backpack or with a light day pack.
Grade C walks (Strenuous): are for the more serious hill walker and a higher level of physical fitness is required. However, no special physical preparations should be needed. Walking days are normally 6-8 hrs and may involve up to 900m of ascent and descent. You should be prepared for several consecutive days of walking, sometimes at higher altitudes, so stamina is important. However, occasionally rest days in the course of the trek will be included.
Grade D walks (Tough): require that you are very fit and previous trekking experience is strongly recommended. Grade D includes long walks with steep uphill and downhill gradients. There will be some hiking at high altitudes (up to 4000m) and corresponding cold weather conditions. These treks will also involve several long days (up to 8-9 hours) of trekking continuously without a rest day.
#805. Geologists and Volcanologist tour of Kamchatka.
Based on the tour by the Geologists' Association of London, UK; these notes are adapted from their guidebook by Dr.Tony Waltham.
SEASON: July 15th - September 15th
Departure 2017: please check our similar tour #101
Group size - up to 16 pax.
See more pictures of this trip.
The northwesterly movement of the Pacific plate has created the Kamchatka volcanic province. This is one of the world's finest example of large scale subduction of an oceanic plate at a very active convergent boundary. The result is a chain of very large andesitic stratovolcanoes. In typical plate boundary style, the volcanic zone includes some more explosive, caldera-forming diacritic volcanic centers, and also basaltic centers that are producing more mildly explosive cinder cones and shield volcanoes. Continued northwestern movement, at a rate of about 80mm per year, of the Pacific Ocean plate causes its subduction beneath Kamchatka. A long history of plate convergence has created parallel volcanic mountain belts that now form the core of the Kamchatka peninsula.
The eastern mountain range is the youngest and contains all the active volcanoes except Ichinsky, which is now only fumarolic. Many of the major eruption deposits have been dated by potassium-argon and radiocarbon methods. Most of the calderas date from about 30,000 to 40,000 years ago, and most of the present cones on the stratovolcanoes have formed entirely in the last 20,000 years. Kamchatka's line of volcanoes continues southwards along the Pacific margin, through the Kuril Islands and into Japan. Clockwise around the Pacific rim, the volcanoes continue in the Aleutian Islands into Alaska. The gap between Kamchatka and the Aleutians is marked by the shear zone along the Bering Fault, a passive transform plate boundary with no subduction and therefore no volcanoes. It meets the Kamchatka coast just north of Shiveluch, and there are therefore no volcanoes further north.
Day 1. Arrive at Petropavlovsk airport. The new road for 24 km into Petropavlovsk is across the farmland on the alluvial flats of the Avacha River.
The Petropavlovsk Hotel is just off the main road in the outskirt of the city. A short evening walk around can provide some first glimpses of Russian life on the streets.
Day 2. Breakfast in hotel. Pack most of your accoutrements in your main case, and leave it in the pile in the reception area. Wear boots and warm outdoor gear. Pack in a small bag one set of spare clothes, extra sweater, overnight kit etc. and torch - the minimum for one night away between two days of walking; have your sleeping bag in there too, or have it separate; and ensure that you can identify your own bag and sleeping bag; have anorak, camera, film etc. with you; no food is needed. Leave hotel by 6WD bus.
Head out of Petropavlovsk for 18 km along the road towards Yelisovo city. Turn off right onto a track, past a small village, and on through birch woods. The route disintegrates into not much of a track up an almost dry river bed. The channel is active annually in melt-water and storm floods; it is also sporadically modified by lathers during activity on the volcanoes ahead. Red and black rounded blocks are andesitic and basaltic lava and tephra, some with feldspar phenocrysts; banks expose dissected debris flows and some lenses of finer airfall ash. The route climbs away from the channel, to continues up sloping tundra with alder and willow. The track ends at sprawling group of cabins, 25 km from the main road; Avacha volcano is up ahead to the right, and Koryaksky is ahead to the left. Lunch is in one of the cabins.
In the afternoon take a gentle walk up the valley to Camel Mountain, a distinctively humped ridge amid a group of small hills on the saddle between Avacha and Koryaksky. The hills are mainly eroded remains of old cinder cones, with some shoulders and summits of welded spatter. They are mainly basaltic, with some loose blocks of lighter andesite; nodular inclusions of dunite (almost pure mosaics of green olivine) are collectable. Snow fields drape some of the slopes. Return to camp, for dinner, and an early night in the tents.
Day 3. Breakfast. Pack your overnight bag and sleeping bag, and roll up your camp-mat, and put them all in the baggage truck before setting out for the day's walk. Have anorak, extra sweater and woolly hat on, or in a day bag. Food is not needed. A water bottle is useful for your own drinking supply.
The volcano walk is on a single trail, where members can walk as far as they wish and then return down the same trail. People can walk at their own pace, but should avoid walking alone; in case of accidents as trivial as a sprained ankle, it is essential to be in groups of at least three. The camp is at an altitude of about 950 m, and Avacha's summit is at 2741 m. The climb to the rim of the summit crater involves a climb of nearly 1800 m. An easier option is to aim to reach the shoulder on the old crater rim, which offers a lovely stretch of scenic walking, and requires a climb of about 1100 m.
The Avacha trail crosses the stream near camp and then heads up pyroclastic slopes, where stream sections expose stratified lapilli tuffs; these become steadily steeper. There are increasingly good views back to the splendid andesite cone of Koryaksky; this rises to 3456 m and is scored by deep gullies, but its current activity is limited to a few small fumaroles.
The steep part of the trail ends where it turns onto a gently rising shoulder, which provides the delightful walk on an easier gradient. The shoulder is the rim of the early crater, formed when the main mass of the old summit slipped in a gigantic landslide down towards the coast, followed immediately by a massive lateral blast and eruption. The old has been nearly filled and obliterated by the growth of the new summit cone. It is surfaced with loose cinders which lie over partially welded pyroclastic flows; some sections of channel are filled with lava with rubbly tops to individual flows.
On the ancient crater rim, there is an old vulcanologist'. The newer summit cone rises above, and its northern slope overlaps and buries the old caldera rim, so that the easy shoulder does not continue round. Andesites on the ridge and above have 4 mm augite and 2 mm feldspar phenocrysts. There are views south to the andesite cone of Viluchinsky and beyond to the complex peaks of Mutnovsky and the rounded shield volcano of Gorely; to the north lie the old degraded cones of the Zhupanovsky volcanoes.
The trail to Avacha's summit starts up some snow fields, but then winds up the steep cinder cone. Its surface is mainly loose, red, oxidized tephra, with areas of airfall ashes, and there are some exposures of the underlying welded pyroclastics.
The summit crater yawned hundreds of meters deep until 1991, when it was filled with andesite lava. The black lava now forms a gentle dome - it is the fresh top of a classic plug dome. Steam rises through its fissured surface, and there are even more fumaroles and solfataras round its edge, at the contact with the crater walls of red pyroclastics. Walk round the rim to the left; giant crescent flow ribs mark the lava's surface where it moved sluggishly east and flowed over the lowest point on the old crater rim. It flowed for a kilometer down the volcano flank, but was so viscous that it came to rest on an angle of nearly 45°. Climbing over the blocky andesite is not easy, but a little scrambling reaches some active vents lined with sulphur crystals. The rim to the right overlooks slopes of sulphur deposits, but soon reaches the lava overflow. There are fine views of Koryaksky and all points beyond.
The descent of the summit cone is on a straight steep down-trail alongside the zigzag up-trail; it requires an element of bold scree running, with considerable care where areas of welded tephra tend to promote spectacular somersaults. Return to the camp before 5pm. After some modest refreshments, the bus heads back down to Petropavlovsk. A late dinner in the Petropavlovsk, soon after we return.
Day 4. Breakfast in hotel. Leave your things in your room, as we return in the evening. Wear boots and outdoor gear. Have rain gear and a spare sweater in a day bag; no food is needed; keep clutter to a minimum as it will only be a pain in the helicopters. Leave in our own conventional bus, for the 45 minutes drive to the heliport, at Yelisovo, close to the main airport.
The helicopter flight to the Valley of Geysers takes about 75 minutes, on either of two routes. The all-weather eastern route heads round the southern and eastern flanks of Avacha, flying at heights of just a few hundred meters above ground if that is necessary to keep below any thick cloud cover. It continues north up a broad valley to the east of the Zhupanovsky volcano; the low flying gives splendid views of the taiga landscape, and this valley is home to many brown bears, who may be easily seen from above. Over a low col, the flight approaches the coast, where a few hunters' cabins lie among the trees; Karymsky and the two Semlyachik volcanoes lie inland to the left. The flight then turns inland up the valley just before the Kikhpinych volcano, and turns into the lush green tributary which is the Valley of Geysers.
The western route heads round the western side of the smaller cones of Arik and Aag, which continue the line of volcanoes northwest from Koryaksky. It then heads across the interior tundra, keeping west of Zhupanovsky, on its way to Karymsky If the eruptions are still in Strombolian style, one should be seen on the flight past. The active cone is 700 m high, and stands inside an old caldera; the even older Dvor caldera is truncated as the higher bowl to the north. Just to the south, Karymsky Lake lies in the Academia Nauk caldera, which erupts less frequently. Northwards, the flight goes over Maly Semlyachik volcano with its spectacular crater lake of green water. Past the inactive Bolshoi Semlyachik, the route veers slightly right for the Valley of Geysers.
The Valley of Geysers
The cluster of geysers, fumaroles and hot springs in this valley were only discovered in 1941. They lie above the marginal fractures of the oldest Uzon caldera. The hot water that emerges is largely recirculated rainfall, mixed with some juvenile water from magma. The magmatic heat source is probably the roots of the Uzon volcano, where ground temperatures reach 250°C at about 500 m depth beneath the caldera floor; alternatively, the Kikhpinych volcano may be the heat source. The Geysernaya River has cut its valley into bedded andesitic tuffs that were deposited in a lake in the first Uzon caldera; the southeastern valley slope is the heavily eroded caldera wall, broken into older volcanic. Some dacite lavas and intrusions occur in the tuffs, and all the exposed rocks have been altered hydrothermally. Some slopes have been gullied to leave earth pillars. There are extensive deposits of opaline siliceous geyserite, some built into large banks and terraces below the main vents. The valley's geysers include a few with large but brief periodic eruptions, and many more which produce hot water spouts frequently or almost continuously.
The helicopters land in front of the timber lodge that is the access point for all visitors to the trails into The Valley of Geysers (Dolina Geyserov), within the Kronotsky Nature Reserve. Walkabouts in the valley are not allowed, so we will stay in a group.
The boardwalk leads to the lip of the valley for a fine overall view. The upper slopes of the valley expose cliffs of pumaceous tuffs, some eroded into earth pillars. The valley floor has a lush green plant cover, except where active banks of geyserite have not yet been colonized.
A branch to the left ends at the Bolshoi (Big) and Maly (Small) Geysers. An eruption of Bolshoi, on the left, throws water about 10 m high amid clouds of steam, for about 10 minutes; it erupts on a cycle of about 75 minute. Maly Geyser throws water out at 45° for about 8 m, in eruptions lasting 5 minutes on a 35 minute cycle.
The main path descends to a bridge over the Geysernaya River a little further upstream. The river reaches a temperature of 26°C with its geothermal input in the summer; winter snow-melt reduces it to about 16°C. Water from the springs and geysers varies from 35°C to 100°C. Just upstream of the bridge, the Schell (Crack) Geyser erupts briefly every 35 minutes; it was heavily eroded during a typhoon flood in 1981. The Fountain Platform is a great bank of geyserite producing copious quantities of steam from numerous vents; it is claimed as the world's greatest concentration of geysers and fumaroles. On the platform. Malachite Grotto is a nearly permanent spouter erupting from a geyserite cone; the Fountain and New Fountain are connected so that they switch their water spouts every few minutes but combine to provide almost continuous activity.
The boardwalk ends before another old bridge. Velikan (Giant) Geyser is on the far bank, inside the bend of the river; it erupts with a cascade of water to heights of about 25 m, but only for about a minute, before sending steam jets to far greater heights for another few minutes; its cycle is around 8 hours. A trail on the terrace above the valley floor provides views down onto the Fountain Platform, and also passes various hot pools, blue with suspended clay, and boiling mud pots, red with iron oxides. Lunch is scheduled at the Valley of Geysers lodge.
The Uzon Caldera
The Uzon depression is bordered to the north and west by steep caldera walls that have survived into the modern landscape. These are essentially features of the second in the series of three caldera collapses; the third (minor) collapse merely deepened the depression west of the helipad that is now largely marsh ground and lake remnants on a floor of lacustrine sediments. The highest ground is formed by the basaltic cone of Uzon volcano, which stands above the western rim of the caldera.
Immediately west of the helipad, Bannoe Lake has a steam vent beneath it; this erupted in 1989, but is now quiet. The lake is about 30m deep, and its bottom 7m are a pool of liquid sulphur at a temperature of 140oC; large blocks of glassy black sulphur have been extracted by volcanologists. It appears that the sulphur vent is similar to the black smokers of ocean floors.
Further west, trails wind across the marsh ground on the caldera floor to a variety of hot springs, boiling lakes and mud pots in the dacitic tuffs and lake sediments. Various of the hot springs have associated sulphur, opal, pyrite and mercury deposits. Most of the colouring at the spring sites is due to temperature-sensitive algae.
Towards the east, a trail leads through alder bushes up the Belaya dome; this is formed of slab-jointed dacite porphyry that varies from dark lava and tuff to glassy obsidian and light pumice. Some is hydrothermally altered, with kaolinite, opal, alunite and sulphur. Adjacent to Belaya, there are two small acid lakes with pH of 2. Further north. Lake Dalneye is nearly 1 km across, in a splendid maar crater fringed by a tuff ring of very scoriaceous basalt; it was produced by the modest steam explosions of a phreatic eruption from a vent beneath the lakes and marshes of the caldera floor.
Return by helicopter to Yelisovo, and by bus to the Petropavlovsk Hotel. Dinner in hotel.
Day 5. Breakfast in hotel. Pack most of your gear in your main case, and leave it in the reception area. Wear boots and warm outdoor gear. Pack in a small bag one set of spare clothes, an extra sweater, overnight kit and torch, and perhaps another change of clothes - the minimum for two nights away between three days of walking; have your sleeping bag in the bag or separate; and ensure that you can identify your own bag and sleeping bag; have anorak, camera, film etc. with you; no food is needed.
Head out of Petropavlovsk on the old road towards Yelisovo. Turn off left across the alluvial flatlands at the mouth of the Avacha River valley. The Paratunka Valley is a geothermal zone with a series of hot springs along its floor. Boreholes have proved groundwater at 80 °C in the porous volcanic rocks at depths of 80-100m. The heat source is magma at depth in the fracture zone along the line of the East Kamchatka Volcanic Belt. Buried pipelines take hot water to greenhouses and a fish farm.
The tarred road lies along the west side of the flat valley floor. Near the end of the farmed land, a dirt road begins; this provides access to the Mutnovsky area for new developments in the form of a geothermal power station and a tourist hotel (both under construction) and also various gold ore deposits (still in the mine prospect stage). The pylons and power lines are the environmental cost of the geothermal resources out in the volcanic wilderness. From the road there are views east to the splendid but inactive cone of Viluchinsky volcano, and north along the glaciated trough of the Paratunka Valley. The road climbs a gently sloping ridge in a lovely environment of open mountain tundra. We stop at a viewpoint on the broad plateau east of Gorely; the shield volcano of Gorely lies to the west, beyond the rim of its modest caldera wall; the ice-clad ramparts of the Mutnovsky volcano lie further away to the south; the Viluchinsky cone rises to the northeast. The onward route depends on which campsite is used, and this depends on snow conditions left by the summer melt after the previous winter; it cannot therefore be known in advance.
Osvystannaya Valley is reached by turning right onto a track that makes a steep and rough descent into the Gorely caldera. The track continues south across a basin floor of wind-blown silt sand and ash, and descends into the valley of the Osvystannaya River with Gorely is on the right. The campsite is in a beautiful and remote wilderness, with the steep andesitic slopes of Mutnovsky rising to the south and the gentler basaltic slopes of Gorely to the north. A short walk to the south reaches the rim of the canyon that drains out of Mutnovsky; it contains some fine waterfalls cut into the volcanic rocks, but its floor is choked with snow many meters deep. Dinner is at camp, then an early night in the tents.
Optional visit: Dachnye Hot Springs lie ahead along the main track. The new geothermal power station and the Mutnovsky gold deposit (with 28 tons of gold reserves in a hydrothermal system of large quartz veins amid a sulphide-bearing stockwork) both lie to the east in the valleys draining to the coast. The maintained track virtually ends at the construction site for some of the power station works and a new tourist hotel, and the campsite is in the valley just below. Two streams converge at the campsite; one is cold for drinking, and the other is warm for washing. A path up the true-left bank of the warm stream is steep, wet and slippery in places; it leads to the source of the hot water in the steam cloud of the old volcanic vent of Aktivny. Just 200 m across, this contains a host of hot springs, small geysers, fumaroles and boiling mud pools. They all lie in hydrothermally altered pumice tuffs and ignimbrites. A walk up the cold stream reveals exposures of welded ignimbrites containing blocks up to 150 mm across that were components of the pyroclastic. All around the site there are rusty pipes projecting from the ground and spouting large or small flows of steam. These were all exploratory bore holes drilled to assess the geothermal resources. Some are recent, but others are 20 years old; treat them with respect as they have been known to explode. Most production bore holes for the new power station are 4 km away to the east. Dinner is at camp, then an early night in the tents.
Day 6. Breakfast. Have an anorak, extra sweater and woolly hat on, or in a day bag. Food is not needed. A water bottle is useful for your own drinking supply. Leave everything else in your tent.
The volcano walk is on a single trail there and back, and everyone should walk into the caldera. Wandering off alone is seriously discouraged, as snow bridges, ice falls and unstable ground on geothermal crusts all provide hazardous environments.
From the Osvystannye campsite, the walk is nearly 7 km, with a rise of less than 600 m, into the main caldera. A gentle stroll soon starts to climb steadily on the bedded pyroclastics of the Mutnovsky slopes beside a stream which emerges from the caldera exit gorge ahead.
From the Dachnye campsite, the walk is longer but with less to climb. A 6WD bus goes as far as possible on a track below the two hills of Skalisty and Dvugorby , which are volcanoes more than 20,000 years old of pale rhyolite lavas and pyroclastics. Beyond the track, a foot-trail climbs past more old bore holes spouting steam, to the pass between Mutnovsky and Dvugorby, from where Asacha (left), Opala and Gorely (right) are seen ahead. The route then makes a long traverse of the hillside, on a mix of rough tundra, blocky andesite lava and banks of airfall ash and pumice reworked by the wind; it crosses three broad snow-fields, before a final rise to the mouth of the caldera exit gorge.
The two routes meet above a short descent into the gorge. Above the steep wall to the south, the steam plume can be seen rising above the active crater of the volcano. Seen away to the east, there are cinder cones and tuff rings over flank vents on the Gorely slopes.
The Mutnovsky 3 caldera
The walk up the gorge is largely on banks of hard snow and firn ice, that has accumulated in winter avalanches off the gorge walls. Much of the surface is covered in wind-blown ash, and some of it is melted into little astrugi pinnacles; the caldera drainage flows in snow caves on the rock surface, and is sometimes seen or heard deep in crevasses or collapse areas. The gorge walls are cut in coarse rhyolitic pyroclastic flows laced with thin dark dykes.
The caldera's eastern glacier lies ahead where it melts out on a steep rock slope, aided by a series of fumaroles; steam from these has created ice tunnels that emerge in the glacier snout.
Climb the slopes of volcanic tephra and glacial till on the right, and descend slightly to the snout of the western glacier, which is also advancing over fumaroles. A way between the ice and the caldera wall passes beside various geothermal vents; these include fumaroles, mud pools and solfataras, and their style may change within hours as melt-water from the adjacent glacier seeps into the ground and is boiled at very shallow depth. A lake is sometimes dammed up behind the glacier; at other times it drains through the ice, leaving a flat bed of reworked ash pitted by solfataras and boiling mud-pools. Streams emerge from the snow and ice fields, and flow back under the glacier toe.
Picnic lunch is taken at some spot away from the fumaroles that are active at the time of the visit The caldera floor is at an altitude of about 1540 m, which is still 800 m below the ice-capped summit of the Mutnovsky volcano.
The walk continues up the western snow-fields below the caldera wall cut in thinly bedded pyroclastic flows that are probably old surge deposits. The glacier on the left has its source in the stage 4 caldera, which has coalesced with the main caldera that is largely of stage 3.
A steep scramble aided by rope handlines leads up coarse welded pyroclastics to a knife-edge ridge between the caldera and the active crater. The steam plume from the active crater rises far above, but when the wind blows it around, the vigorous fumaroles and solfataras that are its source can be seen on the crater floor. The crater is about 350 m across, and its walls drop nearly vertically for over 100 m to its flat floor of scree and inwashed ash.
Return to the campsite back along the outward route. Dinner at camp.
Day 7. Breakfast. Pack your overnight bag and sleeping bag, and roll up your camp-mat, and put them all in the vehicle before setting out for the day's walk. Have an anorak, extra sweater and woolly hat on, or in a day bag. Food is not needed. A water bottle is useful for your own drinking supply.
Again the volcano walk is on a single trail there and back, where members can walk as far as they wish and then return down the same trail. Avoid walking alone; in case of accidents as trivial as a sprained ankle, it is best to be in groups of at least three.
From either campsite, the 6WD bus head north to the track round the edge of the large lake that lies in the unfilled eastern crescent of the Gorely caldera. From the lake flats, the walk up the volcano is about 5 km, climbing steadily to gain 750 m in height. The walk up the huge shield volcano is over a mixture of rough grassy tundra with very low dwarf willow and bare stripes of basaltic a lava. Some lava flow structures are recognizable, and there are also patches of volcanic ash redistributed by the wind.
Aim up the slope for the saddle between the two low summits which are the raised rims of separate craters. Higher up, long gently graded snow-fields provide the easiest route up (and certainly the best way to come back down). The southwest crater, to the left, is dead and rather featureless.
Head through the saddle and then round to the right, along the far rim of the main crater complex. The first large crater contains a cold lake about 100 m below; its surface has ice floes from a small glacier on its internal slope. The walls of all the craters expose profiles through thick sequences of lava flows with a limited component of interbedded pyroclastics. Continue beyond it to a broad shelf that extends inside the very large old central crater. Picnic lunch on the shelf. Just ahead, there is a sudden, unguarded, vertical descent into the active crater. Over 100 m down, a hot acidic lake has active fumaroles and solfataras around its margin and beneath the surface. The recent eruptions of Gorely have been largely steam events produced when these vents heat up and therefore increase their output.
Return back along the outward route to the bus by the lake. The bus head back out of the Gorely caldera, and then return to a hotel in the Paratunka Valley. Rest and swim in pool with thermal hot water.
Day 8. Breakfast in hotel. Leave in a conventional bus, for the journey back to Petropavlovsk. Bring all your baggage with you.
Boat excursion in Avacha Bay.
A boat trip out into the bay is a very relaxing way of gaining an alternative view of the splendid setting of Petropavlovsk and its dramatic volcanoes. Departing from a pier near the center of town, the expanse of the hilly city soon falls into perspective. Further toward the middle of the bay, both Koryaksky and Avacha volcanoes come into view behind the city. When Avacha erupted in 1991, people living in Petropavlovsk could watch the red stream of lava coming down the slope towards the city, while hot ashes were shooting into the skies above the summit crater.
Avacha Bay is geographically as perfect a bay as a city could hope for. It is large and deep, with a narrow opening which keeps out foul weather and ice. The harbour is open to shipping year round, and is also well protected from the dreaded tsunami waves that are created by earthquakes around the Pacific Ocean margins. The boat heads toward the mouth of the bay, allowing views of the Northwest side of Petropavlovsk and the many boats that make their home in these ports. Near the mouth of the bay, the Three Brothers are tall finger-like sea stacks, whose rock faces rise vertically out of the water . The cliffs around the bay house many colonies of seabirds in their natural habitats, and puffins are commonly seen among many other types of seabird.
Return to the Petropavlovsk Hotel for lunch.
The Institute is on the old main road out of Petropavlovsk. A visit includes a short video and presentation by one of the volcanologists to outline the volcanic features of the Kamchatka peninsula. Emphasis is on the huge eruption of Tolbachik in 1975/6, which was predicted after precursor earthquakes, and which brought instant volcanic fame to Kamchatka. There is opportunity to see the small museum, with its spectacular photographs of most of the volcanoes. Specimens are labeled in Russian, so provide a fun identification challenge; don't miss the huge mass of black sulphur (looking like dull basalt glass) that came from Bannoe Lake at Uzon.
Return to the Petropavlovsk Hotel some time in the afternoon, and take your own walk in Petropavlovsk . Dinner is in the hotel.
Day 9. Breakfast. Take a morning walk in the neighborhood or take a bus into town.
The city of 240,000 people is spread along the shores of Avacha Bay wherever buildings can fit between the wooded hills. To see a little of the Russian urban lifestyle, the two obvious alternatives are a walk in the suburbs near the hotel, and a bus ride into the town centre or beyond. There is even time for both.
This involves a gentle stroll to reach various shops, markets and local sights. The main Silhouette crossroads has a bookshop and a money exchange on one corner. Continue along the main road to an open-air market on the left and a large department store on the right, which together give some idea of normal shopping in Russia. Look out for the blocks of flats just beyond. These are old and could have collapsed in an earthquake. They now have large ribs of reinforced concrete up their sides, with steel ties providing tension across their roofs, to prevent oscillating shear whereby the walls fail and the stronger floor decks pancake, to the serious detriment of the occupants. These are now intended to be safe in any local earthquake; all the newer blocks were built to better codes.
Head southwest to reach some older suburbs with typical timber houses; in their midst, the Church of St. Peter and St. Paul (like Petropavl...) has classically beautiful Russian Orthodox gold onion-shaped spires; it is less than 30 minutes walk from the hotel; the area offers views of Avacha Bay.
Bus to town
The centre of town is worth a visit; take a bus, as it's too far to walk both ways. Bus shelters are concrete with a big red A on the roof and a crowd in front. It is easiest to use the big white Daewoo or green buses; numbers 1, 21 and 22 go into town, and there's one every few minutes. Buy a ticket from the conductress on the bus; any distance is the same fare.
The modern city centre is on the parallel one-way roads south of Lenin's statue. The art shop has some good material, popular with visitors (and accepts US dollar notes); it is up the stairs through an obscure door in the back (go round to the left) of the bank at 36 Sovetskaya Street. The Regional Museum, at 20 Leninskaya Street has some excellent displays, and is well worth a visit. For a scenic bus ride, stay on a number 21 bus to its terminus, way down the bay past multiple suburbs, small bays and harbours. Lunch is in the Petropavlovsk Hotel. Afterwards, leave by bus to the airport. Depart from Kamchatka.
Cost EUR 2690 per person.
- Full board
- Twin bedded accommodation in hotel in PKC and Paratunka, in VauDe tents.
- 6-hour marine boat excursion
- English-speaking rep at the arrival and departure in PKC airport
- Transfers by coach and 4WD/6WD bus
- City tour and museums fees
- Guide, interpreter and cook services
- Visa invitation and visa registration
Questions? Interested in booking a trip? See here for answers to frequently asked questions and here for more Kamchatka pictures, click here for booking details or ask your questions here.