Noarootsi parish (Estonian: Noarootsi vald, Swedish: Nuckö
kommun) was a rural municipality in Lääne County, western Estonia
between 1991 and 2017. It covered an area of 296 km2 (114 sq mi)
and had a population of 910.
The administrative center of the
Noarootsi parish was the village of Pyurksi (Birkas in Swedish). It
is located 10 km north of the capital of Lääne County, Haapsalu.
Noarootsi was historically the only parish on the Estonian
mainland where most of the locals spoke Swedish. In 1934, the parish
had 4,388 inhabitants, of whom 2,697 (64%) were Estonian Swedes.
Noarootsi Church
Noarootsi St. Catherine's Church; also
Noarootsi Church is a church belonging to the Estonian Evangelical
Lutheran Church in the village of Hosbi in the Western Nigula
parish. The church is used by the Catholic Church of St. Catherine
of Noaroots in the EELC. The church probably existed as early as the
13-14 centuries. century, but the first church teachers and church
activities in Noarootsi are mentioned in a letter in the 16th
century, when the Noarootsky parish center of St. Catherine
Noarootsi is mentioned as the center.
The Noarootsi Church
suffered greatly during the Livonian War. It was restored in the
17th century and the bell tower dates back to that time. In the 18th
century, a funeral chapel was built as an exceptional addition to
the foot of the tower. The church had three chapels, built in the
17th century as the congregation grew stronger - Sutlepa Chapel,
Rooslepa Chapel and Osmussaare Chapel.
The chair was made by
Elert Thiele in 1656. Other attractions include the altar plateau of
the baptism (1528), the figurative Baroque epitaph of Ungru on the
eastern choir wall (1630, Joachim Winter, sculptor working in
Haapsalu) and a wooden balcony, probably from the 17th century,
carved with an ax.
In the churchyard surrounding the church,
there are interesting old ring crosses and tombs of the landowners
Noarootsi. There is also a monument to the Noarootsi War of
Independence, erected in 1935, destroyed under Soviet rule and
rebuilt in 1990.
Rooslep Chapel
Rooslepa Chapel is a
chapel in Rooslepa village in Läänemaa, Läänemaa. Rooslepa cemetery
is located next to the chapel. The stone chapel was completed in
1834 and collapsed after World War II. Before the construction of
the stone chapel, there was a 17th century wooden chapel, which was
moved to the Sutlepa cemetery and in 1970 to the Estonian Open Air
Museum. In 1997, money was raised for the restoration of the chapel,
and the restored chapel was consecrated in 2007. Regular services
are held once a month, mainly on the 4th Sunday of the month,
starting at 16:00. For more information, please call 5218467.
Sutlep Chapel
Sutlep Chapel is a 17th century coastal
Swedish chapel that has been in the Estonian Open Air Museum since
1970. The chapel was re-consecrated in 1989 and currently serves as
an auxiliary church for the community of St. John in Tallinn. In
1996, a bell tower was built near the main gate of the Sutlepa
cemetery, where the chapel used to be.
Sutlepa Chapel is one
of the oldest wooden buildings in Estonia. The chapel was built in
the Noarootsi parish in Sutlepa village as an auxiliary church for
the parish church. The date of construction is not precisely
determined, but archival records mention the chapel as early as
1627. However, the date "1699" carved above the church door probably
marks the time of the building's construction, which has survived to
this day.
It is known that in 1825 there were eight services
in the chapel, and there may have been baptisms, weddings and
funerals as well. The services were conducted in Estonian and
Swedish.
In the 1830s, the chapel was rebuilt (according to
various sources, in 1834 or 1837 on the doorstep) - the chapel was
dismantled and rebuilt using logs from the nearby Rooslep chapel.
Interior
The interior of the building, which reflects the
first half of the 19th century, is skillfully combined with elements
of the Baroque style. In 1837, the village master Johannes Klingberg
created a pulpit that imitates the work of Tobias Heinz (1589-1635),
a master of the Tallinn Baroque period. The objects also date from
the altar table and grate (1810) and the octagonal base of the
baptistery (1802). The image of Christ hanging over the altar was
transferred to the chapel by the landowner K. von Taube in 1831.
There is a fundraising box next to the door where donation can be
placed inside and outside the building. The close proximity to the
sea is reminiscent of the pewter wreaths hanging on the walls in
memory of the people who stayed there.
The chapel
accommodated about 150 people and traditionally sat on the right and
the women on the left. On both sides of the altar, there are also
so-called German benches, where wealthier and more respectable
families sat.
Osmussaare chapel
In 2014, the chapel, together with the
Osmussaare cemetery, was declared a cultural monument. The first
wooden chapel was probably built in the 16th century in the former
harbor. Since the surface of Osmussaar rises by about 3 mm per year,
the chapel is today located one and a half kilometers north of the
harbor. On September 3, 1766, a limestone chapel was inaugurated,
built on the same site. A statue of Martin Luther reading the Bible,
which was destroyed by a British ship near Osmussaar in 1852, was
erected at the gate of the Cable Fence.
Seven families lived
on a wooden board on the wall of a chapel on the island, who were
forced to leave the island on June 12, 1940 to make way for the Red
Army. The wooden board has now been replaced with a metal plate.
During the Second World War, the chapel was badly damaged.
Therefore, only the facade with the chapel tower has survived. In
1994, the former Osmar built a new bell tower near the chapel.
Prehistory and Early Settlement (Before the 13th Century)
Archaeological evidence for prehistoric human activity in Noarootsi
itself is limited or unclear. The area appears to have been sparsely or
entirely unpopulated during the ancient historic period, unlike many
other Estonian coastal zones with Stone Age or Bronze Age traces.
General Estonian coastal settlement patterns (e.g., Kunda culture from
~8500 BC onward) do not strongly apply here; instead, the region’s
development ties more closely to later maritime and land-use changes.
Swedish settlers arrived in the second half of the 13th century, likely
from Swedish-speaking areas of Finland (then part of the Kingdom of
Sweden) or mainland Sweden, drawn by fishing, seafaring, and
Church-owned lands. They brought privileges known as Svensk Rätt
(“Swedish rights”), granting personal freedom, freedom of movement, and
lower taxes—distinguishing them from Estonian serfs.
The first
written mentions of Swedes in the broader region appear in 1294 (in
Haapsalu town laws). Noarootsi itself is first documented as “Nuckö” in
1391. Osmussaar (Odensholm), part of the parish, was mentioned as early
as 1250. Swedish place names (e.g., villages like Dirslätt/Aulepa,
Roslep/Rooslepa) and the Vormsi-Noarootsi-Riguldi dialect (an Eastern
Swedish variety) attest to this early presence.
Medieval Period
and Livonian Era (13th–16th Centuries)
Swedes settled on Church lands
in coastal western Estonia, including Noarootsi. St. Catherine’s Church
(Noarootsi kirik) was likely built in the late 13th or early 14th
century on what was then an island; it is one of Estonia’s oldest rural
stone churches and was first mentioned in writing around 1500. Chapels
were later added in Sutlepa, Rooslepa, and Osmussaar.
During the
Livonian War (late 16th century), Russian troops plundered the area in
1575, damaging the church and devastating settlements. Swedish influence
grew as the region came under Swedish control from the 1580s (part of
Swedish Estonia, 1561–1710/1721). This era accelerated cultural and
economic life: manors were established (e.g., in Paslepa/Pasklep and
Pürksi/Birkas), but this also began restricting coastal Swedes’
traditional rights and sparked long-term peasant-landlord conflicts.
Swedish Dominion and Early Modern Period (17th–Early 18th Century)
Under Swedish rule, education and Lutheran church life flourished. In
1650, pastor Isaacus Mariaestadius Hasselblatt (or Hasselblad) founded
one of northern Estonia’s first peasant schools in Noarootsi/Pürksi,
teaching in Swedish—though it was short-lived. Students often learned
reading at home or in Sunday schools. Manors proliferated, and the area
gained chapels and improved infrastructure.
The Great Northern War
(1700–1721) and a devastating plague epidemic (1710–1711) killed about
two-thirds of the population, emptying many villages. This marked the
beginning of “Estonianization,” as Estonians from the mainland
repopulated the area. Noarootsi fell under Russian control after 1710.
Russian Empire Era (18th–Early 20th Centuries): Struggles and
National Awakening
Conflicts with German-speaking manor lords
intensified. Coastal Swedes, though never full serfs, faced ambiguous
status after Estonia’s 1816 serf emancipation (which did not fully apply
to them). Agrarian reforms in 1856 finally granted local self-government
and compulsory schooling, improving conditions.
The mid-to-late 19th
century brought intellectual revival. In 1873, Swedish missionary Thure
Emanuel Thorén established a teachers’ seminary at Paslepa manor
(1873–1887), training Swedish-speaking educators and laying groundwork
for nationalism. Noarootsi became a hub: the first choral society (1898
in Paslepa), lending library (1902), Swedish calendar/almanac (1903),
and Swedish Educational Society (1909 in Vööla manor). Temperance
societies and folk high schools emerged. Pürksi manor housed an
agricultural school and later a folk high school.
By the early 20th
century, Noarootsi was the intellectual center of Estonian Swedes.
Economic life revolved around fishing, seafaring, agriculture, and (in
Riguldi/Rickul) shipbuilding.
Independent Estonia (1918–1940):
Cultural Flourishing
In the Republic of Estonia, minorities gained
rights, including cultural autonomy (1925 law). The 1934 census recorded
4,388 residents in Noarootsi Parish, with 2,697 (64%) Estonian
Swedes—the only mainland parish with a Swedish majority. Pürksi Folk
High School (1920–1943) served as a cultural beacon. Trade boomed:
potatoes, apples, and ships (e.g., from Riguldi) went to Sweden and
Finland. Relations with Sweden and Finland strengthened.
World
War II, Soviet Occupation, and Decline (1939–1991)
Soviet military
bases arrived in 1939, turning the area into a restricted border zone
(with checkpoints even for locals). Most Estonian Swedes (nearly 8,000
total across Estonia) evacuated to Sweden in 1943–1944 ahead of full
Soviet re-occupation. Those remaining faced deportations,
collectivization into kolkhozes, and military restrictions. Villages
depopulated dramatically; many historic farms and structures
deteriorated. The area was repopulated partly by war refugees from
northeastern Estonia and Ingria. Contacts with Sweden were severed until
the late 1980s.
Population plummeted from pre-war levels; by the late
Soviet period, Swedish identity was minimal.
Post-Soviet Revival
and Contemporary Era (1991–Present)
Estonia’s restored independence
in 1991 ended the border zone. The first Noarootsi homestead/folk days
were held in 1988 (pre-independence). Swedish-language instruction
resumed (1989), and Noarootsi Gymnasium opened in Pürksi in 1990 with
Swedish immersion. Noarootsi Parish operated as a municipality
(1991–2017) before merging into Lääne-Nigula Parish. By 2005, the
population was ~900–910, with only ~50 identifying as Swedish (down from
thousands). Some descendants have returned, reclaiming land or
developing tourism.
Today, Noarootsi preserves its heritage through
the Museum of the Coastal Swedes (Aiboland), restored churches (e.g.,
St. Catherine’s, Rooslepa Chapel), manors, traditional red-painted
farms, and bilingual signage. It is a quiet tourist destination
emphasizing Swedish-Estonian history, nature (beaches, forests), and
craft (e.g., local breweries naming beers after old villages). The
overall Estonian Swedish population in Estonia remains small
(~800–1,000), but cultural memory endures via festivals, the Rannarootsi
Museum in Haapsalu, and ties to Sweden.
Noarootsi (Estonian: Noarootsi; Swedish: Nuckö) is a coastal
peninsula and former rural municipality in Lääne County, western
Estonia, located about 10 km north of the county seat Haapsalu. Its
central coordinates are approximately 59°00′N 23°31′E.
The former
Noarootsi Parish covered roughly 296 km² and included 23 villages (e.g.,
Pürksi as the administrative center, Dirhami, Einbi, Osmussaare,
Paslepa, Rooslepa, Saare, and Sutlepa) plus offshore features like
Osmussaar Island.
Geographically, Noarootsi forms part of the
West-Estonian Lowland and is renowned for its dynamic post-glacial
coastal landscape shaped by ongoing isostatic rebound (land uplift). It
exemplifies Estonia’s northwestern coastal zone, blending sandy beaches,
dunes, pine forests, marshes, shallow lagoons, and wetlands within the
larger Haapsalu-Noarootsi Wetland Complex.
Geological Formation
and Land Uplift
Noarootsi’s most distinctive feature is its
relatively recent emergence from the sea. Until the mid-19th century,
the peninsula consisted of a group of small islands (shown as “Nackoon”
on a 1705 map). Post-glacial isostatic rebound—caused by the melting of
the Fennoscandian Ice Sheet ~11,000 years ago—lifted the land,
connecting these islands to the mainland.
This uplift continues today
at one of the fastest rates on the Estonian mainland (typically 2–3 mm
per year, with local variations). Since post-glacial terrestrialization
began ~9,300 years ago, the land has risen over 90 meters in total in
the region. This process drives ongoing landscape evolution: shallow
bays turn into lagoons, then lakes, and eventually bogs or dry land
through sediment accretion and reed encroachment.
The bedrock is
primarily Ordovician limestone, overlain by Quaternary clay, marine
sediments, and glacial deposits. Soils are humus-rich but stony mineral
types (Leptosols, Regosols, Cambisols, and Gleysols), supporting diverse
wetland and forest vegetation.
Topography and Landforms
Noarootsi is low-lying and flat, with elevations ranging from sea level
to about 10 m above sea level. The terrain features:
Sandy
beaches and dunes: Iconic “singing sands” (where quartz grains produce a
squeaking sound underfoot) line kilometres of coastline. These are
backed by pine forests and dune systems.
Coastal meadows, reefs, and
mudflats: Extensive shallow coastal areas include sandflats, shingle
ridges, and rocky shores.
Inland features: Small shallow lakes
(remnant lagoons), marshes between dunes, and patches of bog or fen.
The peninsula’s western edge faces the Baltic Sea (Väinameri
sub-basin), while inland bays (remnants of a former strait) create a
mosaic of protected wetlands. Offshore, Osmussaar Island (about 5 km ×
1.5 km) rises with a Baltic Klint cliff, alvar grasslands, and unique
gneiss-breccia boulders from a ~540-million-year-old meteorite impact.
Climate
Noarootsi has a maritime-influenced humid continental
climate (Dfb classification). Winters are relatively mild for the
latitude (January mean ~−3°C), while summers are cool (July mean ~16°C).
Annual precipitation averages around 650 mm, with the wettest months in
late summer/autumn (e.g., October ~97 mm) and more even distribution
than inland Estonia. Wind-driven water-level fluctuations (up to 1.5–2
m) dominate over tides, and storms can cause significant coastal
changes. The moderating Baltic Sea effect keeps temperatures less
extreme than Estonia’s interior.
Hydrology and Wetlands
The
area is part of the Haapsalu-Noarootsi Wetland Complex (~27,450 ha), a
Ramsar-important site with priority EU habitats. Key elements include:
Shallow brackish lagoons (347 ha, depths 0.5–1 m, salinity 0.5–30 g/L).
Extensive reedbeds (Phragmites australis and Cladium mariscus) up to 1
km wide.
Coastal meadows, intertidal flats, and alkaline fens.
Limited water exchange with the open sea, combined with river inflow
and wind, leads to nutrient trapping and high productivity. Ongoing
uplift accelerates terrestrialization, turning marine habitats into
freshwater systems.
Vegetation and Ecosystems
Vegetation
reflects the coastal gradient:
Pine-dominated forests on dunes and
higher ground, rich in mushrooms and berries.
Coastal meadows with
halophytes (e.g., Juncus gerardii, sea-blite) maintained by grazing or
mowing.
Alvar grasslands on Osmussaar (calcareous, thin-soiled,
supporting orchids and rare herbs).
Reedbeds and fens in wetlands,
with transition mires and bogs.
The area supports exceptional
biodiversity: 225 bird species (key stopover for migratory waterfowl,
waders, and eagles), amphibians, fish, and mammals (e.g., otter). It is
one of Estonia’s premier birdwatching sites, with tens of thousands of
birds during migration.